4.7 Article

Soil organic carbon pool changes in relation to slope position and land-use in Indian lower Himalayas

Journal

CATENA
Volume 166, Issue -, Pages 171-180

Publisher

ELSEVIER
DOI: 10.1016/j.catena.2018.04.006

Keywords

C sequestration; Soil erosion; Labile C; Recalcitrant C; Grasslands; Croplands; Land-use; Macro-aggregates

Funding

  1. Indian Council of Agricultural Research National Professor project

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The increase in the atmospheric abundance of CO2 has raised interest in the potential of soils to sequester carbon (C), which inter alia depends on antecedent C level. While inventories of soil organic carbon (SOC) have been developed for different ecosystems at field or global scales, studies at hill-slope level where SOC redistributes by erosion remain scarce. In addition, quantitative information on the variation in SOC stocks and organic matter quality within hill-slopes would allow to make more realistic estimations of the C sequestration potential of landscapes while suggesting improved land management. The main objective of this study was to evaluate the impact of slope position and land-use (grassland versus cropland) on SOC stocks and organic matter quality (proportion of aggregate associated C and labile pools; water extractable, WEOC; hot water soluble, HWC; potassium permanganate oxidizable, KMnO4-C; microbial biomass, MBC). A total of 108 soil samples from the 0-0.15 m layer were collected from 4 slope positions (forested hilltops, middle slope with bare soils, backslopes under grasslands, cropped bottomlands) at nine catenas with 3 replicates per position. The greatest SOC stocks were found at hilltops and backslopes with respectively 10.1 +/- 0.64 and 10.1 +/- 0.57 Mg C ha(-1). SOC stocks decreased by 17% to 8.4 +/- 0.65 Mg C ha(-1) in bottomlands and by 58% to 4.2 +/- 0.26 Mg C ha(-1) at backslopes. The soil organic matter from the hilltops showed the greatest proportion of recalcitrant components (62%) followed by the backslope and bottomland positions with similar to 42%, and middle slope position with 9%. In addition to showing a greater occurrence of labile C fractions, bare and eroded backslope soils were also depleted in water soluble C (WEOC and HWC), KMnO4-C and microbial biomass C. The results showed that there is considerable potential for C sequestration at middle and backslope position through land rehabilitation by either planting trees or vegetation by grass.

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