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<journal-meta>
<journal-id journal-id-type="publisher-id">Front. Environ. Sci.</journal-id>
<journal-title>Frontiers in Environmental Science</journal-title>
<abbrev-journal-title abbrev-type="pubmed">Front. Environ. Sci.</abbrev-journal-title>
<issn pub-type="epub">2296-665X</issn>
<publisher>
<publisher-name>Frontiers Media S.A.</publisher-name>
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<article-id pub-id-type="publisher-id">1373287</article-id>
<article-id pub-id-type="doi">10.3389/fenvs.2024.1373287</article-id>
<article-categories>
<subj-group subj-group-type="heading">
<subject>Environmental Science</subject>
<subj-group>
<subject>Review</subject>
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</article-categories>
<title-group>
<article-title>Biochar application for sustainable soil erosion control: a review of current research and future perspectives</article-title>
<alt-title alt-title-type="left-running-head">Sharma</alt-title>
<alt-title alt-title-type="right-running-head">
<ext-link ext-link-type="uri" xlink:href="https://doi.org/10.3389/fenvs.2024.1373287">10.3389/fenvs.2024.1373287</ext-link>
</alt-title>
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<contrib-group>
<contrib contrib-type="author" corresp="yes">
<name>
<surname>Sharma</surname>
<given-names>Prabhakar</given-names>
</name>
<xref ref-type="corresp" rid="c001">&#x2a;</xref>
<uri xlink:href="https://loop.frontiersin.org/people/381769/overview"/>
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<aff>
<institution>Department of Agricultural Engineering and Technology</institution>, <institution>School of Engineering and Technology</institution>, <institution>Nagaland University</institution>, <addr-line>Dimapur</addr-line>, <addr-line>Nagaland</addr-line>, <country>India</country>
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<author-notes>
<fn fn-type="edited-by">
<p>
<bold>Edited by:</bold> <ext-link ext-link-type="uri" xlink:href="https://loop.frontiersin.org/people/101844/overview">S&#xf6;ren Thiele-Bruhn</ext-link>, University of Trier, Germany</p>
</fn>
<fn fn-type="edited-by">
<p>
<bold>Reviewed by:</bold> <ext-link ext-link-type="uri" xlink:href="https://loop.frontiersin.org/people/2643269/overview">Mark Kibblewhite</ext-link>, Cranfield University, United Kingdom</p>
<p>
<ext-link ext-link-type="uri" xlink:href="https://loop.frontiersin.org/people/2654832/overview">Anastasiah Ngigi</ext-link>, Multimedia University of Kenya, Kenya</p>
</fn>
<corresp id="c001">&#x2a;Correspondence: Prabhakar Sharma, <email>prabhakar.sharma@gmail.com</email>
</corresp>
</author-notes>
<pub-date pub-type="epub">
<day>27</day>
<month>03</month>
<year>2024</year>
</pub-date>
<pub-date pub-type="collection">
<year>2024</year>
</pub-date>
<volume>12</volume>
<elocation-id>1373287</elocation-id>
<history>
<date date-type="received">
<day>19</day>
<month>01</month>
<year>2024</year>
</date>
<date date-type="accepted">
<day>15</day>
<month>03</month>
<year>2024</year>
</date>
</history>
<permissions>
<copyright-statement>Copyright &#xa9; 2024 Sharma.</copyright-statement>
<copyright-year>2024</copyright-year>
<copyright-holder>Sharma</copyright-holder>
<license xlink:href="http://creativecommons.org/licenses/by/4.0/">
<p>This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.</p>
</license>
</permissions>
<abstract>
<p>Soil erosion is a pressing environmental issue with significant agricultural productivity and ecosystem stability implications. In recent years, biochar, a carbon-rich product of biomass pyrolysis, has emerged as a promising soil amendment tool for erosion control due to its ability to improve soil quality and stability. This review paper aims to comprehensively analyze the effectiveness of biochar role in mitigation of soil erosion and sustainable land management practices. By examining a wide range of research studies, this paper elucidates the impact of biochar on key soil erosion parameters as it directly affects the soil structure, water-holding capacity, and nutrient retention. The paper discusses how biochar interacts with soil particles and aggregates to enhance their stability and resistance to erosive forces. It also assesses the influence of biochar properties, such as feedstock type, pyrolysis temperature, and application rate, on its erosion control efficacy. Furthermore, this review explores the role of biochar in promoting plant growth and root development, thereby reinforcing the vegetation cover and further reducing erosion susceptibility. Finally, an outline of potential challenges and opportunities for the widespread adoption of biochar-based erosion control strategies in different agricultural and environmental contexts is presented. Overall, this review provides valuable insights into the multifacet role of biochar in sustainable soil management and offers recommendations for future research directions on direct and indirect application on soil erosion control.</p>
</abstract>
<kwd-group>
<kwd>biochar</kwd>
<kwd>soil erosion</kwd>
<kwd>erosion control mechanisms</kwd>
<kwd>soil amendment</kwd>
<kwd>soil quality</kwd>
</kwd-group>
<custom-meta-wrap>
<custom-meta>
<meta-name>section-at-acceptance</meta-name>
<meta-value>Soil Processes</meta-value>
</custom-meta>
</custom-meta-wrap>
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</front>
<body>
<sec id="s1">
<title>1 Introduction</title>
<p>Soil erosion is a significant environmental issue affecting various parts of the world. It is the process by which topsoil is removed or displaced by natural forces, such as wind or water flow. This is exacerbated by human activities like deforestation, overgrazing, and improper agricultural practices (<xref ref-type="bibr" rid="B7">Bhattacharyya et al., 2015</xref>). The global annual soil loss due to erosion is significant, suggesting approximately 24&#xa0;billion tons of fertile topsoil loss yearly (<xref ref-type="bibr" rid="B1">Abdel Rahman, 2023</xref>). Soil erosion, caused by water, wind, and human activities, severely threatens agricultural productivity, food security, and environmental sustainability. Soil erosion can have various detrimental impacts, including reduced agricultural productivity, water pollution, sedimentation in rivers and lakes, and destruction of natural habitats (<xref ref-type="bibr" rid="B32">Issaka and Ashraf, 2017</xref>).</p>
<p>Globally, several regions face extreme soil erosion problems. For example, extensive soil erosion is a critical issue in China, primarily due to deforestation, overgrazing, and intensive farming practices (<xref ref-type="bibr" rid="B67">Wang et al., 2021</xref>). It led to sedimentation in rivers, reduced agricultural productivity, and increased desertification. Many African regions, particularly sub-Saharan Africa, experience significant soil erosion. Deforestation, overcultivation, and poor land management further contribute to the problem (<xref ref-type="bibr" rid="B1">Abdel Rahman, 2023</xref>). This has severe consequences for agricultural productivity and food security in the region. Countries like Indonesia and the Philippines struggle with soil erosion due to deforestation, unsustainable farming practices, and the expansion of palm oil plantations (<xref ref-type="bibr" rid="B56">Ramdani and Lounela, 2020</xref>), which led to the loss of fertile soil, reduced biodiversity, and increased sedimentation in water bodies. Soil erosion is also a concern in the United States, particularly in the Midwest and Great Plains regions, where intensive agriculture developed degradation of soil quality and increased sedimentation in waterways (<xref ref-type="bibr" rid="B13">Chen et al., 2022</xref>). In South American countries like Brazil and Argentina, deforestation, unsustainable agricultural practices, and land degradation contribute to significant soil erosion issues by impacting local ecosystems and global climate patterns (<xref ref-type="bibr" rid="B61">Santiba&#xf1;ez and Santiba&#xf1;ez, 2007</xref>).</p>
<p>In India, soil erosion is a pressing issue, particularly in regions with intensive agricultural activities, deforestation, and improper land management practices. Factors such as overgrazing, monsoon rains, and the unsustainable use of land contribute to the problem. They impact the agricultural productivity and fertile topsoil, results into sedimentation in rivers and increases vulnerability to natural disasters like floods and landslides in India (<xref ref-type="bibr" rid="B7">Bhattacharyya et al., 2015</xref>). Initiatives such as implementation of watershed management practices, afforestation programs, and sustainable agricultural techniques are being undertaken to mitigate soil erosion and conserve the country&#x2019;s vital natural resources.</p>
<p>Soil erosion contributes to the loss of essential nutrients and topsoil. As the fertile top layer is gradually washed or blown away, the soil&#x2019;s ability to support plant growth diminishes, which impacts crop yields and overall agricultural sustainability. The loss of nutrients crucial for plant growth (such as nitrogen, phosphorus, and potassium) further exacerbates the problem, necessitating the increased use of fertilizers, which have environmental and economic implications (<xref ref-type="bibr" rid="B50">Nathan et al., 2022</xref>; <xref ref-type="bibr" rid="B81">Zhu et al., 2022</xref>; <xref ref-type="bibr" rid="B34">Jiao et al., 2023</xref>). Moreover, erosion-induced sedimentation in water bodies can disrupt aquatic ecosystems and water quality by causing eutrophication and additional environmental challenges (<xref ref-type="bibr" rid="B67">Wang et al., 2021</xref>). To combat this, implementing measures such as conservation tillage, agroforestry, and cover cropping is crucial in preserving the nutrient-rich topsoil and sustaining agricultural productivity in the long term (<xref ref-type="bibr" rid="B20">Fahad et al., 2022</xref>).</p>
<p>So far, several effective practices have been implemented globally to control soil erosion. These practices included the use of conservation tillage, which involves minimizing soil disturbance during planting and establishing buffer zones near water bodies to trap sediment and reduce nutrient runoff (<xref ref-type="bibr" rid="B70">Wen et al., 2023</xref>). Additionally, adopting agroforestry techniques, such as planting trees in combination with crops, helped stabilize the soil and mitigate erosion (<xref ref-type="bibr" rid="B20">Fahad et al., 2022</xref>). Terracing and contour farming continued to be widely employed on hilly terrain to reduce water runoff and prevent soil loss (<xref ref-type="bibr" rid="B17">Deng et al., 2021</xref>). Furthermore, promoting cover cropping and crop rotation strategies contributed to maintaining soil structure and fertility, thereby minimizing erosion risks (<xref ref-type="bibr" rid="B38">Koudahe et al., 2022</xref>; <xref ref-type="bibr" rid="B62">Scavo et al., 2022</xref>). The emphasis on maintaining soil structure and microbial diversity also contributes to improved water retention and reduced susceptibility to erosion. In addition, the organic farming plays a pivotal role in promoting sustainable agricultural practices and effectively controlling soil erosion (<xref ref-type="bibr" rid="B22">Gamage et al., 2023</xref>). Organic farming enhances the capacity to withstand the negative impacts of climate change by fostering resilience within the agroecosystem. It establishes robust and environment friendly farming systems that demonstrate resilience to temperature variations and drought while indirectly prevents soil erosion. The organic farming also advocates for sustainable and eco-friendly management, embraces conservation practices, and supports restoration activities. At the same time, the organic farming practices reduce the risk of water pollution from chemical runoffs, fostering a healthier environment. However, the inorganic fertilizers increased soil erosion and degradation while providing essential nutrients for plant growth (<xref ref-type="bibr" rid="B64">Tripathi et al., 2020</xref>). The reliance on these fertilizers often leads to a reduction in microbial habitat and biodiversity within the soil. The integration of all these measures, along with sustainable land management approaches, played a critical role in combating soil erosion and preserving agricultural productivity.</p>
<p>India has been actively implementing various measures as well to combat soil erosion. These include promoting sustainable agricultural practices like conservation tillage and crop rotation and constructing check dams and contour trenches for water conservation (<xref ref-type="bibr" rid="B7">Bhattacharyya et al., 2015</xref>). Afforestation programs and watershed management projects have also been crucial in controlling soil erosion and preserving soil fertility (<xref ref-type="bibr" rid="B46">Liu et al., 2020</xref>). Educational campaigns to raise awareness about effective soil conservation techniques among farmers and local communities may produce adequate results (<xref ref-type="bibr" rid="B49">Mango et al., 2017</xref>).</p>
<p>Biochar, a carbon-rich product of biomass pyrolysis, has shown promise as an effective tool for controlling soil erosion (<xref ref-type="bibr" rid="B69">Wani et al., 2023</xref>). Its porous structure and high surface area enhance soil porosity and water retention by reducing runoff and soil loss during heavy rainfall (<xref ref-type="bibr" rid="B36">Kameyama et al., 2012</xref>). Biochar-amended soils have improved stability, reduced susceptibility to erosion, and enhanced nutrient retention capacity (<xref ref-type="bibr" rid="B50">Nathan et al., 2022</xref>; <xref ref-type="bibr" rid="B66">Vahidi et al., 2022</xref>). Furthermore, incorporating biochar into soil has been found to promote microbial activity by fostering a healthier soil ecosystem that further contributes to erosion control (<xref ref-type="bibr" rid="B16">Das et al., 2021</xref>; <xref ref-type="bibr" rid="B33">Jia et al., 2024</xref>). Biochar application exerts generally positive impacts on different forms of soil erosion, including wind, water, and cultivation erosion. In the context of wind erosion, biochar enhances soil moisture and structure by promoting aggregation and reducing susceptibility to wind-driven soil loss to some extent (<xref ref-type="bibr" rid="B63">Silva et al., 2015</xref>). The water erosion is mitigated through biochar application with the improvement in water retention capacity, reduction in surface runoff, as well as enhancement in soil stability (<xref ref-type="bibr" rid="B24">Gholamahmadi et al., 2023</xref>). This effectively prevents the soil particles from being transported by water to great extent. In the event of soil disturbance during agricultural practices, biochar&#x2019;s role in enhancing soil structure and stability also contributes to reduced erosion. Although the specific mechanisms differ for different scenarios, the overarching effect of biochar is a consistent for soil resilience across various erosion types and making it a versatile and effective solution for sustainable land management. Although biochar use for soil erosion control appears promising, further research is necessary to fully understand its long-term effectiveness, optimal application rates, and potential environmental impacts. Nonetheless, biochar holds potential as a sustainable solution for mitigating soil erosion and improving overall soil health.</p>
<p>Besides its effectiveness in reducing soil erosion, biochar offers significant advantages in soil nutrient management. With its high surface area and porosity, biochar exhibits a remarkable ability to retain essential plant nutrients, preventing their leaching and making them available to plants over an extended period (<xref ref-type="bibr" rid="B21">Feng et al., 2022</xref>; <xref ref-type="bibr" rid="B50">Nathan et al., 2022</xref>). Furthermore, its application contributes to improved soil structure, increased water retention, and enhanced microbial habitat, <italic>i.e</italic>., fostering nutrient cycling and promoting overall soil health (<xref ref-type="bibr" rid="B36">Kameyama et al., 2012</xref>). Its role in mitigation of greenhouse gas emissions by sequestering carbon further highlights its potential as a sustainable solution for agricultural sustainability and environmental conservation (<xref ref-type="bibr" rid="B2">Abhishek et al., 2022</xref>).</p>
<p>While biochar offers numerous benefits in soil nutrient management, its application must be carefully managed, considering factors such as feedstock type, production process, and soil characteristics. Its widespread adoption requires further research to determine optimal application rates, the long-term effects on soil health, and potential environmental impacts (<xref ref-type="bibr" rid="B49">Mango et al., 2017</xref>). Despite these considerations, biochar shows promise as a sustainable tool for improving soil fertility, enhancing crop productivity, and contributing to climate change mitigation efforts (<xref ref-type="bibr" rid="B2">Abhishek et al., 2022</xref>; <xref ref-type="bibr" rid="B78">Zhang et al., 2022a</xref>).</p>
<p>Current understanding suggests that biochar can effectively mitigate soil erosion by enhancing soil stability, reducing surface runoff, and improving water infiltration (<xref ref-type="bibr" rid="B36">Kameyama et al., 2012</xref>; <xref ref-type="bibr" rid="B71">Xia et al., 2022</xref>). However, challenges remain, including the need to establish optimal application rates, as excessive biochar application might alter soil properties and impact plant growth (<xref ref-type="bibr" rid="B24">Gholamahmadi et al., 2023</xref>). Additionally, the influence of biochar on specific soil types, climates, and crop varieties requires further investigation for a comprehensive understanding of its effectiveness in diverse agricultural settings. Studies are underway to assess the long-term impacts of biochar application on soil fertility, microbial activity, and ecosystem dynamics. Exploring the synergistic effects of biochar in combination with other soil conservation practices is also a critical area of research, aiming to develop integrated and sustainable approaches for effective soil erosion control in various agricultural landscapes.</p>
<p>Addressing the global soil erosion problem requires a combination of sustainable land management practices, afforestation, soil conservation measures, and responsible agricultural techniques. This review paper encompasses a comprehensive analysis of the current research on using biochar for soil erosion control, emphasizing its effectiveness, mechanisms, and potential applications. It also addresses the challenges and opportunities of adopting biochar-based strategies in sustainable land management.</p>
</sec>
<sec id="s2">
<title>2 Biochar impact on soil erosion parameters</title>
<p>Biochar has shown considerable potential in positively influencing various soil erosion parameters (<xref ref-type="fig" rid="F1">Figure 1</xref>). Its application significantly reduces soil loss by enhancing soil stability, improving aggregate strength, and promoting the formation of stable soil aggregates (<xref ref-type="bibr" rid="B78">Zhang et al., 2022a</xref>; <xref ref-type="bibr" rid="B55">Qiu et al., 2023</xref>). The porous structure of biochar aids in increasing water infiltration and reducing surface runoff, thereby minimizing the impact of water on soil erosion (<xref ref-type="bibr" rid="B35">Jien and Wang, 2013</xref>). Additionally, biochar-amended soils exhibit improved water-holding capacity, which is likely reducing soil erosion vulnerability during heavy rainfall events (<xref ref-type="bibr" rid="B36">Kameyama et al., 2012</xref>). Its ability to enhance soil organic matter content and stimulate microbial activity contributes to developing a more resilient soil structure that likely mitigates erosion risks. Moreover, the long-term stability of biochar in the soil ensures a sustained impact on erosion control, which is making it a valuable tool in promoting sustainable land management practices and preserving soil integrity (<xref ref-type="bibr" rid="B16">Das et al., 2021</xref>; <xref ref-type="bibr" rid="B30">Hou, 2021</xref>). The current research explores the mechanisms underlying biochar&#x2019;s influence on soil erosion parameters and optimizes its application for effective erosion control in various environmental settings.</p>
<fig id="F1" position="float">
<label>FIGURE 1</label>
<caption>
<p>Biochar impact on soil erosion parameters.</p>
</caption>
<graphic xlink:href="fenvs-12-1373287-g001.tif"/>
</fig>
<sec id="s2-1">
<title>2.1 Impact on soil structure/texture</title>
<p>This is evident that biochar significantly impacts the soil structure. Its introduction to the soil enhances soil aggregation by creating a more stable and porous soil matrix. By improving aggregation, biochar develops the formation of stable soil aggregates with better soil porosity, water infiltration, and retention (<xref ref-type="bibr" rid="B78">Zhang et al., 2022a</xref>). The porous nature of biochar allows for increased water and nutrient-holding capacity, which is promoting a favorable environment for root growth and microbial activity. The biochar improves soil structure by reducing soil compaction, particularly in clayey soils, thus enhances the root penetration and nutrient uptake (<xref ref-type="bibr" rid="B10">Blanco-Canqui, 2021</xref>). The long-term stability of biochar in the soil contributes to sustained improvements in soil structure, which is crucial for sustainable agricultural practices and ecosystem health (<xref ref-type="bibr" rid="B36">Kameyama et al., 2012</xref>). The influence of soil texture on soil-biochar interactions plays a crucial role in determining the effectiveness of biochar applications. Studies have shown that soil texture affects the adsorption capacity, porosity, and nutrient retention of biochar. In sandy soils, biochar often improves water retention and nutrient availability due to its high surface area and porosity, thus enhances the overall soil fertility. Conversely, in clayey soils, biochar alleviates compaction issue, improve drainage, and enhance the soil structure. Further research should be conducted to understand the intricate mechanisms of biochar-soil interactions and to optimize its application for improving soil structure and long-term agricultural sustainability.</p>
</sec>
<sec id="s2-2">
<title>2.2 Impact on water holding capacity of soil</title>
<p>Biochar can have a significant impact on the water-holding capacity of soil. Its porous structure and high surface area enable it to hold water effectively, thus enhancing the soil&#x2019;s ability to retain moisture (<xref ref-type="bibr" rid="B36">Kameyama et al., 2012</xref>). When incorporated into the soil, biochar acts as a sponge by absorbing excess water during high precipitation and releasing it slowly during dry periods, which maintains optimal soil moisture level for plant growth. This characteristic is particularly beneficial in arid and semi-arid regions with limited water availability. The improved water-holding capacity provided by biochar also contributes to drought resistance, reduces the need for irrigation, and promotes the survival and growth of crops, which ultimately enhances the agricultural productivity and sustainability (<xref ref-type="bibr" rid="B36">Kameyama et al., 2012</xref>). At the same time, the impact of biochar on water retention fluctuates depending on biochar type, application rate, soil type, and environmental conditions, which emphasizes the importance of these factors while utilizing biochar for water management in agricultural systems (as highlighted in <xref ref-type="sec" rid="s4">Section 4</xref>). The influence of biochar on soil water retention for sustainable water resource management and climate-resilient agriculture need to be investigated further.</p>
</sec>
<sec id="s2-3">
<title>2.3 Impact of nutrient retention</title>
<p>Biochar has a substantial impact on the retention of nutrients in the soil. Its high surface area and porous structure provide an ideal environment for nutrient adsorption and retention, which prevents leaching and making essential nutrients available to plants over an extended period. By effectively trapping nutrients such as nitrogen, phosphorus, potassium, and various micronutrients, biochar helps to reduce nutrient and pollution release into water bodies by promoting environmental sustainability (<xref ref-type="bibr" rid="B75">Yang et al., 2017a</xref>; <xref ref-type="bibr" rid="B76">2017b</xref>; <xref ref-type="bibr" rid="B73">2019a</xref>; <xref ref-type="bibr" rid="B21">Feng et al., 2022</xref>; <xref ref-type="bibr" rid="B50">Nathan et al., 2022</xref>). Furthermore, biochar in the soil enhances the cation exchange capacity and facilitates the retention and exchange of positively charged ions, which are crucial for plant growth (<xref ref-type="bibr" rid="B19">Domingues et al., 2020</xref>). This improved nutrient retention capacity increased the nutrient-use efficiency in agricultural systems and minimized the need for additional fertilizers <italic>i.e.,</italic> reduced the risk of nutrient loss (<xref ref-type="bibr" rid="B78">Zhang et al., 2022a</xref>). The specific effects of biochar on nutrient retention can also vary depending on factors such as biochar feedstock, production process, application rate, and soil type, which emphasizes the importance of tailored approaches for optimization of nutrient management in diverse agricultural settings. The intricates mechanisms underlying the interaction between biochar and soil nutrients for sustainable farming practices to maximize nutrient retention and minimize environmental impacts should be a topic of future research.</p>
</sec>
</sec>
<sec id="s3">
<title>3 Biochar interaction mechanisms</title>
<p>The interaction between biochar and soil involves complex and multifaceted mechanisms that influence various soil properties and processes (<xref ref-type="fig" rid="F2">Figure 2</xref>). One key mechanism is the physical structure of biochar, which contributes to improved soil porosity, water retention, and aeration, <italic>i.e</italic>., promoting favorable conditions for plant growth and microbial activity (<xref ref-type="bibr" rid="B18">Ding et al., 2016</xref>; <xref ref-type="bibr" rid="B6">Alkharabsheh et al., 2021</xref>; <xref ref-type="bibr" rid="B44">Liu et al., 2024</xref>). The high surface area and porosity of biochar also facilitate the adsorption and retention of nutrients, organic compounds, and contaminants, which is enhancing soil fertility and reducing the leaching of essential nutrients. Additionally, the chemical properties of biochar, such as its pH and surface charge, influences the soil acidity, nutrient availability, and cation exchange capacity by further impacting soil health and plant nutrition (<xref ref-type="bibr" rid="B19">Domingues et al., 2020</xref>). Moreover, the biological interactions between biochar and soil microbiota are crucial in nutrient cycling, organic matter decomposition, and stable soil aggregates, which contributes towards long-term soil fertility and structure development (<xref ref-type="bibr" rid="B78">Zhang et al., 2022a</xref>). These intricate mechanisms are essential for optimizing biochar application in diverse agricultural systems for sustainable soil management practices and mitigation of environmental challenges associated with soil degradation and nutrient loss. The complexities of biochar-soil interactions for development of effective and tailored strategies are being explores for maximizing the benefits of biochar in enhancing soil quality and agricultural productivity.</p>
<fig id="F2" position="float">
<label>FIGURE 2</label>
<caption>
<p>Multifaceted mechanisms affecting soil properties and processes due to the interaction between biochar and soil.</p>
</caption>
<graphic xlink:href="fenvs-12-1373287-g002.tif"/>
</fig>
<sec id="s3-1">
<title>3.1 Interaction with soil particles</title>
<p>The introduction of biochar into soil initiates intricate interactions with soil particles, which influences various physical and chemical properties. Biochar&#x2019;s porous structure and high surface area enable it to interact with soil particles physically by enhancing the soil aggregation and stability. The biochar forms stable soil aggregates, improves soil porosity, water infiltration, and water-holding capacity, thereby creates a more favorable environment for plant growth (<xref ref-type="bibr" rid="B19">Domingues et al., 2020</xref>). Chemically, biochar interacts with soil particles through its surface functional groups, which is affecting the soil pH, nutrient availability, and cation exchange capacity. These interactions also improve the soil fertility, enhance the nutrient retention, and reduce the nutrient leaching, <italic>i.e</italic>., ultimately benefiting plant health and productivity (<xref ref-type="bibr" rid="B18">Ding et al., 2016</xref>). These intricate relations between biochar and soil particles are crucial for optimizing its application to improve soil quality, promote sustainable agriculture, and mitigate environmental degradation. For the future research, the application of biochar would be a valuable tool for soil enhancement and sustainable land management.</p>
</sec>
<sec id="s3-2">
<title>3.2 Aggregate formation in the field due to biochar</title>
<p>Biochar has demonstrated a significant potential in promoting aggregate formation in soil (<xref ref-type="bibr" rid="B31">Hua et al., 2014</xref>). Biochar stabilizes soil aggregates through its physical and chemical properties, leading to improved soil structure and stability. The porous nature of biochar allows for the creation of microhabitats that facilitate the colonization of beneficial soil microorganisms, which ultimately promoting the soil aggregation. Additionally, biochar serves as a binding agent, helping to cement the soil particles together and enhancing the stable macroaggregate formation (<xref ref-type="bibr" rid="B9">Blanco-Canqui, 2017</xref>; <xref ref-type="bibr" rid="B74">Yang et al., 2019b</xref>). This enhanced aggregation contributes to better soil porosity, water infiltration, and root penetration, ultimately fostering a more conducive environment for the plant growth (<xref ref-type="bibr" rid="B19">Domingues et al., 2020</xref>). Moreover, the persistent nature of biochar in the soil matrix ensures a sustained positive influence on aggregate formation, thereby promoting long-term soil fertility and resilience. The biochar&#x2019;s role in aggregate formation is considered an important tool to develop a sustainable practices that leverage biochar as a valuable tool for enhancing soil structure and overall agricultural productivity.</p>
</sec>
<sec id="s3-3">
<title>3.3 Stability and resistance to erosive forces</title>
<p>Biochar application induces notable change in the stability and resistance of soil to erosive forces. Its incorporation into the soil matrix enhances soil aggregation and structure, which is developing stable soil aggregates that are less prone to breakdown under erosive forces (<xref ref-type="bibr" rid="B29">Herath et al., 2013</xref>; <xref ref-type="bibr" rid="B15">Curaqueo et al., 2014</xref>). The increased aggregate stability contributes to improved soil structure, reduced susceptibility to compaction, and enhanced resistance to water and wind erosion (<xref ref-type="bibr" rid="B35">Jien and Wang, 2013</xref>; <xref ref-type="bibr" rid="B42">Li et al., 2019</xref>; <xref ref-type="bibr" rid="B71">Xia et al., 2022</xref>). Biochar&#x2019;s ability to improve soil organic matter content and promote microbial activity further strengthens the soil structure, which is fostering the development of a more resilient soil matrix to withstand erosive pressures. Additionally, the water-holding capacity provided by biochar aids in maintaining optimal soil moisture levels, which reduces the impact of water erosion even during heavy rainfall events (<xref ref-type="bibr" rid="B36">Kameyama et al., 2012</xref>). Its long-term persistence in the soil ensures sustained improvements in soil stability, <italic>i.e.</italic>, underscoring its potential as an effective tool for mitigation of soil erosion and development of soil integrity.</p>
</sec>
</sec>
<sec id="s4">
<title>4 Biochar properties on erosion intensity</title>
<p>The properties of biochar play a critical role in influencing erosion intensity in various environmental contexts. The fundamental biochar properties, such as particle size, surface area, porosity, and chemical composition, significantly impact its effectiveness in erosion mitigation (<xref ref-type="table" rid="T1">Table 1</xref>). Biochar with larger particle sizes and increased surface area tends to create a more stable soil structure by reducing the soil susceptibility to erosive forces (<xref ref-type="bibr" rid="B68">Wang et al., 2020</xref>). Its high porosity facilitates the water infiltration and retention, which minimizes the surface runoff and soil detachment during rainfall events (<xref ref-type="bibr" rid="B5">Ahmadi et al., 2020</xref>). Furthermore, the chemical composition of biochar, including its pH, nutrient content, and surface functional groups, influences soil stability and aggregation, thereby reducing the potential for soil loss due to erosion (<xref ref-type="bibr" rid="B69">Wani et al., 2023</xref>). This intricate interplay between biochar properties and erosion intensity is crucial for optimization of its application in erosion-prone areas and sustainable land management practices.</p>
<table-wrap id="T1" position="float">
<label>TABLE 1</label>
<caption>
<p>Soil erosion parameters influences by critical biochar properties.</p>
</caption>
<table>
<thead valign="top">
<tr>
<th align="center">Biochar properties</th>
<th align="center">Impact on soil erosion</th>
<th align="center">References</th>
</tr>
</thead>
<tbody valign="top">
<tr>
<td align="left">Feedstock Type</td>
<td align="left">Influences biochar&#x2019;s porosity, surface area, and chemical composition, affecting soil structure and erosion resistance</td>
<td align="left">
<xref ref-type="bibr" rid="B4">Agegnehu et al., 2016</xref>; <xref ref-type="bibr" rid="B40">Lehmann et al., 2003</xref>
</td>
</tr>
<tr>
<td align="left">Pyrolysis Temperature</td>
<td align="left">Alters biochar&#x2019;s physical and chemical properties, impacting adsorption capacity, porosity, and efficacy in soil erosion control</td>
<td align="left">
<xref ref-type="bibr" rid="B26">Glaser et al., 2001</xref>; <xref ref-type="bibr" rid="B52">Novak et al., 2009</xref>
</td>
</tr>
<tr>
<td align="left">Application Rate</td>
<td align="left">Varied application rates affect soil structure, water retention, and erosion control differently based on biochar properties</td>
<td align="left">
<xref ref-type="bibr" rid="B48">Major et al. (2010)</xref>
</td>
</tr>
</tbody>
</table>
</table-wrap>
<sec id="s4-1">
<title>4.1 Feedstock type for biochar</title>
<p>The choice of feedstock/biomass for biochar production significantly influences its effectiveness in reduction of erosion intensity. The microscopic image of biochar synthesized from selected feedstock types is illustrated in <xref ref-type="fig" rid="F3">Figure 3</xref>. They illustrate the unique surface roughness for biochar developed using different biomasses. Various feedstock materials, such as wood chips, agricultural residues, and organic waste, yield biochar with distinct physical and chemical properties that would impact its erosion control capabilities. Feedstocks with high lignin and cellulose content, such as woody biomass, produce biochar with enhanced structural stability and a higher resistance to erosive forces (<xref ref-type="bibr" rid="B68">Wang et al., 2020</xref>). This type of biochar effectively strengthens the soil aggregates by reducing soil detachment and erosion risk. The relationship between feedstock type and biochar properties would be essential for the selection of suitable feedstocks to maximize biochar&#x2019;s efficacy in erosion-prone environments.</p>
<fig id="F3" position="float">
<label>FIGURE 3</label>
<caption>
<p>Morphology of biochar produced from different types of feedstock: <bold>(A)</bold> mesquite wood (Trigo et al., 2016); <bold>(B)</bold> corn stalk (Ma et al., 2016); <bold>(C)</bold> chicken manure (Joseph et al., 2010); <bold>(D)</bold> sewage sludge (Song et al., 2014); <bold>(E)</bold> anaerobic digestate (Tang et al., 2019); <bold>(F)</bold> coconut husk (Suman and Gautam, 2017) <bold>(G)</bold> paddy straw <bold>(H)</bold> tea residue.</p>
</caption>
<graphic xlink:href="fenvs-12-1373287-g003.tif"/>
</fig>
</sec>
<sec id="s4-2">
<title>4.2 Pyrolysis temperature for biochar synthesis</title>
<p>The pyrolysis temperature employed in biochar production significantly impacts its effectiveness in mitigating erosion intensity. Different pyrolysis temperatures yield biochar with varying physical and chemical properties that influence its stability and performance in erosion control. Biochar produced at higher pyrolysis temperatures tends to have higher carbon content, increased aromaticity, and a more condensed structure (<xref ref-type="bibr" rid="B74">Yang et al., 2019b</xref>), which is improving the resistance to degradation and erosive forces. Such biochar exhibits enhanced stability, higher surface area, and improved water-holding capacity (<xref ref-type="bibr" rid="B68">Wang et al., 2020</xref>). It is evident that higher pyrolysis temperatures significantly impact the nutrient and mineral content of feedstocks. When biomass is pyrolyzed at high temperatures, there is a greater likelihood of thermal decomposition, which is leading to the loss of volatile organic compounds and a reduction in the overall nutrient content of the resulting biochar (<xref ref-type="bibr" rid="B74">Yang et al., 2019b</xref>). The high temperatures facilitate the breakdown of complex organic compounds, <italic>i.e</italic>., loss of volatile nitrogen compounds and the transformation of phosphorus into less plant-available forms (<xref ref-type="bibr" rid="B45">Liu et al., 2023</xref>; <xref ref-type="bibr" rid="B80">Zhao et al., 2024</xref>). The severity of this impact varies based on the feedstock type and the specific pyrolysis conditions. Generally, higher temperatures tend to result in biochar with lower concentrations of nutrients and minerals. Studies have shown that at elevated pyrolysis temperatures, such as above 600&#xb0;C, biochar tends to have reduced nitrogen and phosphorus content (<xref ref-type="bibr" rid="B79">Zhang et al., 2022b</xref>).</p>
<p>While biochar has been extensively studied as a soil amendment, it is crucial to recognize that the implication of high-temperature pyrolysis on nutrient retention might vary across different contexts and applications. The effectiveness of biochar as a soil amendment tool depends on factors such as soil type, climate, and the specific goals of the agricultural or environmental management system. Therefore, interpretations of biochar&#x2019;s applicability should consider these contextual variations, and cautious consideration is needed when extrapolating findings from one study to another. The impact of pyrolysis temperature on biochar properties is essential for optimizing its production to yield biochar with the desired characteristics for effective erosion control. The future research should explore the relationships between pyrolysis temperature, biochar properties, and erosion intensity systematically in order to develop a tailored pyrolysis protocol for producing biochar which effectively mitigates the erosion and preserve soil quality.</p>
</sec>
<sec id="s4-3">
<title>4.3 Application rate on agricultural land</title>
<p>Biochar provides a stable soil structure to agricultural soil. The long-lasting soil amendment of biochar enhances the soil structure, water retention, and nutrient availability; however, the application rate of biochar should be carefully determined based on the specific soil properties, crop types, and local environmental conditions for effective soil erosion control (<xref ref-type="bibr" rid="B24">Gholamahmadi et al., 2023</xref>). Optimal application rates typically range from 10 to 50 tons per hectare, depending on the severity of erosion, soil texture, and organic matter content (<xref ref-type="bibr" rid="B8">Bista et al., 2019</xref>). The biochar application rate for different soil types is indicated in <xref ref-type="table" rid="T2">Table 2</xref>. This range allows formation of a stable soil structure and improved water infiltration by reducing surface runoff and effectively minimizing erosion (<xref ref-type="bibr" rid="B69">Wani et al., 2023</xref>). However, it is crucial to consider the potential impact of excessive biochar application on soil pH, nutrient availability, and plant growth by emphasizing the need for site-specific assessments and careful monitoring to ensure sustainable agricultural practices and long-term soil health.</p>
<table-wrap id="T2" position="float">
<label>TABLE 2</label>
<caption>
<p>Effects of biochar treatment (type and doses) on different soil types for erosion control.</p>
</caption>
<table>
<thead valign="top">
<tr>
<th align="left">Soil type</th>
<th align="left">Sand (%)</th>
<th align="left">Silt (%)</th>
<th align="left">Clay (%)</th>
<th align="left">Rainfall rate (mm h<sup>-1</sup>)</th>
<th align="left">Biochar type</th>
<th align="left">Biochar dose</th>
<th align="left">Soil loss rate (g m<sup>-2</sup> min<sup>-1</sup>)</th>
<th align="left">References</th>
</tr>
</thead>
<tbody valign="top">
<tr>
<td rowspan="3" align="left">Poorly graded sand</td>
<td rowspan="3" align="left">82</td>
<td rowspan="3" align="left">2</td>
<td rowspan="3" align="left">0</td>
<td rowspan="3" align="left">60</td>
<td rowspan="3" align="left">Water hyacinth</td>
<td align="left">0%</td>
<td align="left">2.27</td>
<td rowspan="3" align="left">
<xref ref-type="bibr" rid="B11">Cai et al. (2020)</xref>
</td>
</tr>
<tr>
<td align="left">5%</td>
<td align="left">1.05</td>
</tr>
<tr>
<td align="left">10%</td>
<td align="left">1.47</td>
</tr>
<tr>
<td rowspan="2" align="left">Loam</td>
<td rowspan="2" align="left">45.6</td>
<td rowspan="2" align="left">31.1</td>
<td rowspan="2" align="left">23.3</td>
<td rowspan="2" align="left">100</td>
<td rowspan="2" align="left">Oak tree</td>
<td align="left">0&#xa0;Mg&#xa0;ha<sup>-1</sup>
</td>
<td align="left">0.19</td>
<td rowspan="2" align="left">
<xref ref-type="bibr" rid="B39">Lee et al. (2015)</xref>
</td>
</tr>
<tr>
<td align="left">10&#xa0;Mg&#xa0;ha<sup>-1</sup>
</td>
<td align="left">0.15</td>
</tr>
<tr>
<td rowspan="2" align="left">Calcareous loam</td>
<td rowspan="2" align="left">41</td>
<td rowspan="2" align="left">39</td>
<td rowspan="2" align="left">20</td>
<td rowspan="2" align="left">55</td>
<td rowspan="2" align="left">Wood chips</td>
<td align="left">0%</td>
<td align="left">18.62</td>
<td rowspan="2" align="left">
<xref ref-type="bibr" rid="B3">Abrol et al. (2016)</xref>
</td>
</tr>
<tr>
<td align="left">2%</td>
<td align="left">14.02</td>
</tr>
<tr>
<td rowspan="4" align="left">Aeolian sandy</td>
<td rowspan="4" align="left">46.83</td>
<td rowspan="4" align="left">37.47</td>
<td rowspan="4" align="left">15.7</td>
<td rowspan="4" align="left">90</td>
<td rowspan="4" align="left">Coconut shell</td>
<td align="left">0%</td>
<td align="left">8.92</td>
<td rowspan="4" align="left">
<xref ref-type="bibr" rid="B14">Chen et al. (2019)</xref>
</td>
</tr>
<tr>
<td align="left">0.1%</td>
<td align="left">7.89</td>
</tr>
<tr>
<td align="left">0.7%</td>
<td align="left">6.61</td>
</tr>
<tr>
<td align="left">1%</td>
<td align="left">6.10</td>
</tr>
<tr>
<td rowspan="2" align="left">Marl</td>
<td rowspan="2" align="left">42</td>
<td rowspan="2" align="left">43</td>
<td rowspan="2" align="left">15</td>
<td rowspan="2" align="left">50</td>
<td rowspan="2" align="left">-</td>
<td align="left">0&#xa0;g&#xa0;m<sup>-2</sup>
</td>
<td align="left">0.27</td>
<td rowspan="2" align="left">
<xref ref-type="bibr" rid="B60">Sadeghi et al. (2020)</xref>
</td>
</tr>
<tr>
<td align="left">800&#xa0;g&#xa0;m<sup>-2</sup>
</td>
<td align="left">0.23</td>
</tr>
<tr>
<td rowspan="4" align="left">Sandy loam</td>
<td rowspan="4" align="left">53</td>
<td rowspan="4" align="left">32</td>
<td rowspan="4" align="left">14</td>
<td rowspan="4" align="left">50</td>
<td rowspan="4" align="left">Sewage sludge</td>
<td align="left">0&#xa0;t&#xa0;ha<sup>-1</sup>
</td>
<td align="left">19.20</td>
<td rowspan="4" align="left">
<xref ref-type="bibr" rid="B25">Gholami et al. (2019)</xref>
</td>
</tr>
<tr>
<td align="left">0.4&#xa0;t&#xa0;ha<sup>-1</sup>
</td>
<td align="left">4.01</td>
</tr>
<tr>
<td align="left">0.8&#xa0;t&#xa0;ha<sup>-1</sup>
</td>
<td align="left">2.49</td>
</tr>
<tr>
<td align="left">1.6&#xa0;t&#xa0;ha<sup>-1</sup>
</td>
<td align="left">1.65</td>
</tr>
<tr>
<td rowspan="4" align="left">Silt loam</td>
<td rowspan="4" align="left">8.47</td>
<td rowspan="4" align="left">67.98</td>
<td rowspan="4" align="left">23.55</td>
<td rowspan="4" align="left">60</td>
<td rowspan="4" align="left">Wheat straw</td>
<td align="left">0&#xa0;t&#xa0;ha<sup>-1</sup>
</td>
<td align="left">1.58</td>
<td rowspan="4" align="left">
<xref ref-type="bibr" rid="B54">Peng et al. (2019)</xref>
</td>
</tr>
<tr>
<td align="left">7.5&#xa0;t&#xa0;ha<sup>-1</sup>
</td>
<td align="left">1.41</td>
</tr>
<tr>
<td align="left">15&#xa0;t&#xa0;ha<sup>-1</sup>
</td>
<td align="left">1.39</td>
</tr>
<tr>
<td align="left">30&#xa0;t&#xa0;ha<sup>-1</sup>
</td>
<td align="left">1.30</td>
</tr>
<tr>
<td rowspan="2" align="left">Sandy clay loam</td>
<td rowspan="2" align="left">62</td>
<td rowspan="2" align="left">22</td>
<td rowspan="2" align="left">16</td>
<td rowspan="2" align="left">50</td>
<td rowspan="2" align="left">Vinasse</td>
<td align="left">0&#xa0;t&#xa0;ha<sup>-1</sup>
</td>
<td align="left">1.14</td>
<td rowspan="2" align="left">
<xref ref-type="bibr" rid="B59">Sadeghi et al. (2016)</xref>
</td>
</tr>
<tr>
<td align="left">8&#xa0;t&#xa0;ha<sup>-1</sup>
</td>
<td align="left">0.63</td>
</tr>
<tr>
<td rowspan="5" align="left">Hutton</td>
<td rowspan="5" align="left">41</td>
<td rowspan="5" align="left">33.6</td>
<td rowspan="5" align="left">25.4</td>
<td rowspan="5" align="left">360</td>
<td rowspan="5" align="left">Maize residue</td>
<td align="left">0%</td>
<td align="left">17.52</td>
<td rowspan="5" align="left">
<xref ref-type="bibr" rid="B35">Jien and Wang (2013)</xref>
</td>
</tr>
<tr>
<td align="left">2.5%</td>
<td align="left">14.32</td>
</tr>
<tr>
<td align="left">5%</td>
<td align="left">15.04</td>
</tr>
<tr>
<td align="left">7.5%</td>
<td align="left">10.84</td>
</tr>
<tr>
<td align="left">10%</td>
<td align="left">10.10</td>
</tr>
<tr>
<td rowspan="3" align="left">Typic paleudults</td>
<td rowspan="3" align="left">16.2</td>
<td rowspan="3" align="left">40.2</td>
<td rowspan="3" align="left">43.6</td>
<td rowspan="3" align="left">80</td>
<td rowspan="3" align="left">White lead tree</td>
<td align="left">0%</td>
<td align="left">24.3</td>
<td rowspan="3" align="left">
<xref ref-type="bibr" rid="B53">Nyambo et al. (2018)</xref>
</td>
</tr>
<tr>
<td align="left">2.5%</td>
<td align="left">12.17</td>
</tr>
<tr>
<td align="left">5%</td>
<td align="left">8.87</td>
</tr>
</tbody>
</table>
</table-wrap>
</sec>
</sec>
<sec id="s5">
<title>5 Biochar impact on plant</title>
<p>Biochar, with its porous structure and high surface area, has a range of positive effects on plant growth and development. It has demonstrated a significant potential to impact the crop production and agricultural sustainability positively (<xref ref-type="table" rid="T3">Table 3</xref>). Its introduction to the soil enhances the overall soil health and fertility, <italic>i.e</italic>., improving crop yields and quality. Biochar&#x2019;s porous structure aids to increase in water retention and reduction in nutrient leaching, thereby promoting more efficient water and nutrient use by crop efforts (<xref ref-type="bibr" rid="B78">Zhang et al., 2022a</xref>). By fostering a healthier and more balanced soil microbiome, biochar contributes to better plant nutrient availability and uptake.</p>
<table-wrap id="T3" position="float">
<label>TABLE 3</label>
<caption>
<p>Effects of biochar addition on crop yield (adopted from <xref ref-type="bibr" rid="B18">Ding et al., 2016</xref>).</p>
</caption>
<table>
<thead valign="top">
<tr>
<th align="left">Biochar type</th>
<th align="center">Biochar rate (t ha<sup>&#x2212;1</sup>)</th>
<th align="left">Crops</th>
<th align="left">Soil type</th>
<th align="center">Yield/biomass increase as compared to control (%)</th>
<th align="left">References</th>
</tr>
</thead>
<tbody valign="top">
<tr>
<td rowspan="3" align="left">Secondary forest wood</td>
<td align="center">68</td>
<td rowspan="2" align="center">Cowpea</td>
<td rowspan="3" align="center">Xanthic Ferralsol</td>
<td align="center">20</td>
<td rowspan="3" align="left">
<xref ref-type="bibr" rid="B27">Glaser et al. (2002)</xref>
</td>
</tr>
<tr>
<td align="center">136.75</td>
<td align="center">100</td>
</tr>
<tr>
<td align="center">68</td>
<td align="center">Rice</td>
<td align="center">50</td>
</tr>
<tr>
<td rowspan="2" align="left">Poultry litter</td>
<td align="center">10</td>
<td rowspan="2" align="center">Radish</td>
<td rowspan="2" align="center">Alfisol</td>
<td align="center">42</td>
<td rowspan="2" align="left">
<xref ref-type="bibr" rid="B12">Chan et al. (2008)</xref>
</td>
</tr>
<tr>
<td align="center">50.5</td>
<td align="center">96</td>
</tr>
<tr>
<td align="left">Orchard pruning</td>
<td align="center">22</td>
<td align="center">Grape</td>
<td align="center">Sandy clay loam</td>
<td align="center">20</td>
<td align="left">
<xref ref-type="bibr" rid="B23">Genesio et al. (2015)</xref>
</td>
</tr>
<tr>
<td align="left">Charcoal</td>
<td align="center">0.5</td>
<td align="center">Moong</td>
<td align="center">Dehli soil</td>
<td align="center">22</td>
<td align="left">
<xref ref-type="bibr" rid="B27">Glaser et al. (2002)</xref>
</td>
</tr>
<tr>
<td align="left">Green waste</td>
<td align="center">100</td>
<td align="center">Radish</td>
<td align="center">Alfisol</td>
<td align="center">266</td>
<td align="left">
<xref ref-type="bibr" rid="B12">Chan et al. (2008)</xref>
</td>
</tr>
<tr>
<td align="left">Cow manure</td>
<td align="center">15</td>
<td align="center">Maize</td>
<td align="center">Sandy soil</td>
<td align="center">150</td>
<td align="left">
<xref ref-type="bibr" rid="B65">Uzoma et al. (2011)</xref>
</td>
</tr>
<tr>
<td align="left">Logs of <italic>Eucalyptus deglupta</italic>
</td>
<td align="center">30</td>
<td align="center">Rice</td>
<td align="center">Inceptisol</td>
<td align="center">294</td>
<td align="left">
<xref ref-type="bibr" rid="B51">Noguera et al. (2010)</xref>
</td>
</tr>
<tr>
<td align="left">Wheat straw</td>
<td align="center">40</td>
<td align="center">Rice</td>
<td align="center">Paddy soil</td>
<td align="center">14</td>
<td align="left">
<xref ref-type="bibr" rid="B77">Zhang et al. (2010)</xref>
</td>
</tr>
<tr>
<td rowspan="3" align="left">Hardwood</td>
<td align="center">19</td>
<td rowspan="3" align="center">Maize</td>
<td rowspan="3" align="center">Midwestern mollisols</td>
<td align="center">10</td>
<td rowspan="3" align="left">
<xref ref-type="bibr" rid="B58">Rogovska et al. (2014)</xref>
</td>
</tr>
<tr>
<td align="center">38</td>
<td align="center">17</td>
</tr>
<tr>
<td align="center">58</td>
<td align="center">48</td>
</tr>
<tr>
<td rowspan="2" align="left">Wheat straw</td>
<td align="center">40</td>
<td align="center">Rapeseed</td>
<td rowspan="2" align="center">Upland red soil</td>
<td align="center">36.02</td>
<td rowspan="2" align="center">
<xref ref-type="bibr" rid="B47">Liu et al. (2014)</xref>
</td>
</tr>
<tr>
<td align="center">40</td>
<td align="center">Sweet potato</td>
<td align="center">53.77</td>
</tr>
<tr>
<td rowspan="3" align="left">Black carbon</td>
<td align="center">20</td>
<td rowspan="3" align="center">Maize</td>
<td rowspan="3" align="center">Oxisol</td>
<td align="center">28 (the second year)</td>
<td rowspan="3" align="center">
<xref ref-type="bibr" rid="B48">Major et al. (2010)</xref>
</td>
</tr>
<tr>
<td align="center">20</td>
<td align="center">30 (the third year)</td>
</tr>
<tr>
<td align="center">20</td>
<td align="center">140 (the fourth year)</td>
</tr>
</tbody>
</table>
</table-wrap>
<p>Additionally, its influence on soil structure and aeration facilitates root growth and penetration, further supporting the plant development. The biochar&#x2019;s ability to sequester carbon in the soil also contributes to climate change mitigation and aids in the long-term stability and sustainability of agricultural ecosystems (<xref ref-type="bibr" rid="B2">Abhishek et al., 2022</xref>). Nevertheless, while biochar has shown significant promise, its effect on crops is influenced by factors such as the specific crop type, soil conditions, biochar properties, and application methods. Therefore, a careful consideration of these variables is crucial for maximizing the potential benefits of biochar in sustainable crop production system.</p>
<sec id="s5-1">
<title>5.1 Development and growth of plant roots</title>
<p>The development and growth of plant roots on land, where biochar has been applied, demonstrate several promising effects that contribute to improved plant performance. Biochar amendments enhance the soil&#x2019;s physical structure by promoting better aeration and water retention, which in turn fosters more extensive and vigorous root systems efforts (<xref ref-type="bibr" rid="B78">Zhang et al., 2022a</xref>). The porous nature of biochar provides a conducive habitat for beneficial soil microorganisms by creating a symbiotic relationship that aids in nutrient cycling and availability, thereby facilitating robust root development. Furthermore, the increased water-holding capacity of biochar-amended soil supports sustained root growth, particularly during dry spells by helping the plants to withstand drought stress. Studies also suggest that biochar amendments influence the rhizosphere&#x2019;s microbial community composition, <italic>i.e</italic>., potentially improving nutrient acquisition and overall plant health (<xref ref-type="bibr" rid="B43">Liao et al., 2013</xref>; <xref ref-type="bibr" rid="B72">Yan et al., 2022</xref>). However, the specific effects of biochar on root development may vary depending on factors such as biochar properties, application rates, and soil conditions. Therefore, a comprehensive research is necessary to optimize biochar application strategies for enhanced root growth and sustainable agricultural practices that promote resilient plant-root systems and long-term soil health.</p>
</sec>
<sec id="s5-2">
<title>5.2 Reinforcement of vegetation cover</title>
<p>The reinforcement of vegetation cover due to biochar application plays a vital role in promoting ecosystem stability and resilience. Biochar amendments enhance the soil fertility and structure, fostering an environment conducive to robust plant growth and establishment. The improved water-holding capacity of biochar-amended soil helps to mitigate the negative impacts of water stress on vegetation, allowing plants to maintain optimal physiological functions even during periods of limited water availability (<xref ref-type="bibr" rid="B67">Wang et al., 2021</xref>). Moreover, biochar&#x2019;s ability to promote nutrient retention and availability in the soil supports vegetation&#x2019;s sustained growth and vitality, aiding in establishing dense and healthy vegetation cover (<xref ref-type="bibr" rid="B6">Alkharabsheh et al., 2021</xref>; <xref ref-type="bibr" rid="B37">Kochanek et al., 2022</xref>). This reinforcement of vegetation cover not only helps to prevent soil erosion but also contributes to the conservation of biodiversity and the overall stability of the ecosystem. However, the effectiveness of biochar in reinforcing vegetation cover may depend on various factors, including the specific biochar properties, application methods, and local environmental conditions. Therefore, a comprehensive understanding of these factors is essential to maximize the benefits of biochar application for sustainable ecosystem management and conservation.</p>
</sec>
<sec id="s5-3">
<title>5.3 Reduction of erosion susceptibility</title>
<p>The application of biochar to land is an effective strategy for reduction of erosion susceptibility and soil conservation. Biochar amendments significantly improve the soil structure and stability, enhancing the soil&#x2019;s resistance to erosive forces such as wind and water (<xref ref-type="bibr" rid="B35">Jien and Wang, 2013</xref>; <xref ref-type="bibr" rid="B42">Li et al., 2019</xref>). The porous nature of biochar increases the soil porosity and aggregation by creating a more stable soil matrix, <italic>i.e</italic>., less susceptible to displacement and runoff (<xref ref-type="bibr" rid="B28">Hao et al., 2022</xref>). By enhancing water retention and infiltration, biochar helps to maintain soil moisture levels and reduces the likelihood of surface crusting and soil detachment, which are common precursors to erosion (<xref ref-type="bibr" rid="B36">Kameyama et al., 2012</xref>; <xref ref-type="bibr" rid="B19">Domingues et al., 2020</xref>; <xref ref-type="bibr" rid="B78">Zhang et al., 2022a</xref>). Additionally, incorporating biochar into the soil promotes the development of a well-structured root system, which is further anchoring the soil and minimizing the risk of erosion. The improved nutrient retention and microbial activity associated with biochar-amended soil also contribute to the establishment of a healthy vegetative cover by providing additional protection against erosion. However, the effectiveness of biochar in reducing erosion susceptibility may vary depending on factors such as biochar properties, application rates, and soil characteristics. Thus, site-specific assessments and sustainable land management practices are essential for harnessing the full potential of biochar in mitigating erosion and ensuring long-term soil conservation.</p>
</sec>
</sec>
<sec id="s6">
<title>6 Potential challenges and opportunities for biochar-based erosion control strategies</title>
<p>While biochar-based erosion control strategies hold significant promise, several challenges and opportunities must be considered for effective implementation. It is important to note that most of these studies are indirect and corelated with their corresponding soil and water properties. The implementation of biochar-based erosion control strategies encounters challenges requiring careful consideration and proactive management. One of the primary challenges lies in the intricate interactions between biochar, soil properties, and local environmental conditions, necessitating site-specific assessments to determine the optimal biochar application rates and methods (<xref ref-type="bibr" rid="B8">Bista et al., 2019</xref>). The cost of large-scale biochar implementation can be prohibitive, particularly for resource-limited agricultural communities, thereby hindering widespread adoption.</p>
<p>Furthermore, ensuring the long-term stability of biochar-amended soils and maintaining their erosion control benefits demand continuous monitoring and management, especially in dynamic and variable environmental contexts. The effectiveness of biochar in erosion control is also influenced by factors such as biochar characteristics, soil type, and climatic variability, underscoring the need for comprehensive research and tailored application techniques (<xref ref-type="bibr" rid="B41">Li and Tasnady, 2023</xref>). Addressing these challenges requires collaborative efforts between researchers, policymakers, and local communities to develop sustainable and cost-effective biochar-based erosion control strategies that are dependent on specific environmental contexts and socioeconomic constraints. Biochar-based erosion control strategies present a fertile ground for various research opportunities to enhance their effectiveness and practical implementation. Firstly, there is a need for comprehensive field studies to assess the long-term impact of biochar on different soil types and under varying climatic conditions by considering its influence on soil structure, water retention, and vegetation cover (<xref ref-type="bibr" rid="B67">Wang et al., 2021</xref>). Soil erosion control through biochar treatments greatly dependent on soil types. The detail of biochar impact and uses on different soil types are highlighted in <xref ref-type="table" rid="T2">Table 2</xref>. The interaction mechanism between biochar and soil microorganisms provide insights into optimizing its potential for enhancing soil stability and erosion resistance.</p>
<p>Additionally, research focusing on development of cost-effective production techniques and biochar formulations to specific soil erosion challenges facilitate the broader adoption in diverse agricultural settings. Exploring the potential synergies between biochar and other soil conservation practices, such as cover cropping and terracing, could offer integrated and sustainable erosion management solutions (<xref ref-type="bibr" rid="B7">Bhattacharyya et al., 2015</xref>). Furthermore, investigating the socioeconomic implications of biochar adoption, including its impact on agricultural productivity and livelihoods, can guide policy development and promote community engagement in erosion control efforts (<xref ref-type="bibr" rid="B57">Rogers et al., 2021</xref>; <xref ref-type="bibr" rid="B41">Li and Tasnady, 2023</xref>). These research opportunities pave the way for the refinement and widespread application of biochar-based erosion control strategies by contributing to the sustainability and resilience of agricultural landscapes worldwide.</p>
<p>It is evident from this study that the existing research is limited on the direct use of biochar application for soil erosion control. Instead, the majority of references primarily explore the impact of biochar on various soil parameters which influence the soil erosion either directly or indirectly. This gap highlights the need for more targeted investigations specifically addressing the role of biochar in mitigation of soil erosion to better understand its potential contributions for sustainable land management. Addressing these challenges and capitalizing on the opportunities successfully integrate the biochar-based erosion control strategies into sustainable land management practices and promote the resilient agricultural systems and environmental conservation.</p>
</sec>
<sec sec-type="conclusion" id="s7">
<title>7 Conclusion</title>
<p>In conclusion, biochar application for sustainable soil erosion control holds considerable promise, as evidenced by several research findings. Its ability to enhance soil structure, water retention, and vegetation cover underscores its potential as an effective erosion mitigation strategy. However, the complexities of biochar-soil interactions and the diverse environmental and socioeconomic contexts in which erosion occurs emphasize the need for further research and development. Future efforts should focus on conducting long-term field studies to assess the durability and efficacy of biochar in diverse geographical settings. Additionally, exploring innovative production methods, systematic biochar formulations, and integrated erosion management approaches could unlock new opportunities for maximizing its benefits. Furthermore, addressing the economic feasibility and scalability of biochar adoption and understanding its broader implications for sustainable agricultural practices and ecosystem services are crucial for its successful integration into erosion control strategies. By embracing a multidisciplinary approach and fostering collaboration between researchers, policymakers, and local communities, biochar application can emerge as a pivotal tool in promoting sustainable soil conservation and nurturing resilient agricultural landscapes for generations.</p>
</sec>
</body>
<back>
<sec id="s8">
<title>Author contributions</title>
<p>PS: Conceptualization, Data curation, Formal Analysis, Investigation, Methodology, Validation, Visualization, Writing&#x2013;original draft, Writing&#x2013;review and editing.</p>
</sec>
<sec sec-type="funding-information" id="s9">
<title>Funding</title>
<p>The author(s) declare that no financial support was received for the research, authorship, and/or publication of this article.</p>
</sec>
<sec sec-type="COI-statement" id="s10">
<title>Conflict of interest</title>
<p>The author declares that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.</p>
<p>The author(s) declared that they were an editorial board member of Frontiers, at the time of submission. This had no impact on the peer review process and the final decision.</p>
</sec>
<sec sec-type="disclaimer" id="s11">
<title>Publisher&#x2019;s note</title>
<p>All claims expressed in this article are solely those of the authors and do not necessarily represent those of their affiliated organizations, or those of the publisher, the editors and the reviewers. Any product that may be evaluated in this article, or claim that may be made by its manufacturer, is not guaranteed or endorsed by the publisher.</p>
</sec>
<sec id="s12">
<title>Supplementary material</title>
<p>The Supplementary Material for this article can be found online at: <ext-link ext-link-type="uri" xlink:href="https://www.frontiersin.org/articles/10.3389/fenvs.2024.1373287/full#supplementary-material">https://www.frontiersin.org/articles/10.3389/fenvs.2024.1373287/full&#x23;supplementary-material</ext-link>
</p>
<supplementary-material xlink:href="Image1.JPEG" id="SM1" mimetype="application/JPEG" xmlns:xlink="http://www.w3.org/1999/xlink"/>
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