4.8 Article

Soil burial reduces decomposition and offsets erosion-induced soil carbon losses in the Indian Himalaya

Journal

GLOBAL CHANGE BIOLOGY
Volume 28, Issue 4, Pages 1643-1658

Publisher

WILEY
DOI: 10.1111/gcb.15987

Keywords

carbon budget; erosion; Himalaya; priming; soil redistribution; tillage

Funding

  1. University of Exeter
  2. Indian Council of Agricultural Research

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The global debate on whether soil erosion acts as a net source or sink of carbon remains inconclusive, especially in low-input agricultural systems in acknowledged global soil erosion hotspots in developing countries. However, studies in the Indian Himalaya have shown that high rates of soil erosion do not necessarily lead to net carbon loss to the atmosphere at the field scale, and there is potential to promote carbon storage through sustainable agricultural practices.
The extent to which soil erosion is a net source or sink of carbon globally remains unresolved but has the potential to play a key role in determining the magnitude of CO2 emissions from land-use change in rapidly eroding landscapes. The effects of soil erosion on carbon storage in low-input agricultural systems, in acknowledged global soil erosion hotspots in developing countries, are especially poorly understood. Working in one such hotspot, the Indian Himalaya, we measured and modelled field-scale soil budgets, to quantify erosion-induced changes in soil carbon storage. In addition, we used long-term (1-year) incubations of separate and mixed soil horizons to better understand the mechanisms controlling erosion-induced changes in soil carbon cycling. We demonstrate that high rates of soil erosion did not promote a net carbon loss to the atmosphere at the field scale. Furthermore, our experiments showed that rates of decomposition in the organic matter-rich subsoil layers in depositional areas were lower per unit of soil carbon than from other landscape positions; however, these rates could be increased by mixing with topsoils. The results indicate that, the burial of soil carbon, and separation from fresh carbon inputs, led to reduced rates of decomposition offsetting potential carbon losses during soil erosion and transport within the cultivated fields. We conclude that the high rates of erosion experienced in these Himalayan soils do not, in isolation, drive substantial emissions of organic carbon, and there is the potential to promote carbon storage through sustainable agricultural practice.

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