Abstract
Conventional-till (CT) practices can reduce soil organic matter (SOM) and microbial activity and increase soil erosion and compaction. In contrast, no-till (NT) has emerged as a viable option for protecting the soil surface against erosion and degradation. The NT has a lot of advantages such as reduced equipment costs, runoff, and erosion, increased drought resistance of crops, and higher SOM and microbial activity compared to the CT systems. Under the NT system, maintenance of high surface soil cover has resulted in a significant change in soil properties such as bulk density, soil water retention, pore size distribution, infiltration, soil organic C, enzyme activity, and microbial communities. Soil microbial communities are the drivers of SOM decomposition and nutrient cycling including the most limited nutrients for crop growth, N and phosphorus. This chapter mainly focuses on the impact of NT on soil C storage, compaction, and biochemical and microbial activity as compared to the CT systems.
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Financial support for this work was provided by the US Department of Agriculture, Natural Resources Conservation Service (grant no. G17AC00337). We thank the US Geological Survey and South Dakota Cooperative Fish and Wildlife Research Unit for administrative assistance with the research work order (RWO 116) at South Dakota State University.
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Sekaran, U., Kumar, S. (2021). Responses of Soil Carbon Storage, Compaction, and Biological Properties Under No-Till and Conventional-Till Systems. In: Jayaraman, S., Dalal, R.C., Patra, A.K., Chaudhari, S.K. (eds) Conservation Agriculture: A Sustainable Approach for Soil Health and Food Security . Springer, Singapore. https://doi.org/10.1007/978-981-16-0827-8_17
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