Variations and Indications of δ 13 C SOC and δ 15 N SON in Soil Profiles in Karst Critical Zone Observatory (CZO), Southwest China

Man Liu, Guilin Han, Qian Zhang and Zhaoliang Song
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Man Liu: Institute of Earth Sciences, China University of Geosciences, Beijing 100083, China
Guilin Han: Institute of Earth Sciences, China University of Geosciences, Beijing 100083, China
Qian Zhang: School of Water Resources and Environment, China University of Geosciences, Beijing 100083, China
Zhaoliang Song: Institute of Surface-Earth System Science, Tianjin University, Tianjin 300072, China

Sustainability, 2019, vol. 11, issue 7, 1-16

Abstract: Soil carbon and nitrogen storage and stabilization are the key to solving the problems of mitigation of global warming and maintaining of crop productivity. In this study, the contents of soil organic carbon (SOC) and soil organic nitrogen (SON) and their stable isotope compositions (δ 13 C SOC and δ 15 N SON ) in soil profiles were determined in two agricultural lands (including a farmland and an abandoned farmland) and four non-agricultural lands (including two shrub-grass lands and two shrub lands) in the karst critical zone observatory (CZO), Southwest China. The contents of SOC and SON were used for research on the effects of land use on SOC and SON storage, and the change of δ 13 C SOC and δ 15 N SON values in soil profiles were used to indicate SOC and SON stabilization. The results showed that agricultural activities reduced SOC and SON storage in the whole soil layers of farmland compared to non-agricultural lands, and farmland abandonment slightly increased SOC and SON storage. Crop rotation between peanut (C 3 ) and corn (C 4 ) affected the δ 13 C SOC in surface soils of agricultural lands (−21.6‰), which were intermediate between shrub lands (−22.7‰) and shrub-grass lands (−19.6‰). 15 N-depleted SON in surface soils in farmland compared to those soil in other lands possibly associated with synthetic N fertilizer application. In soil layers below 30 cm depth the δ 13 C SOC deceased with depth, while the δ 15 N SON displayed irregular fluctuation. The change in δ 13 C SOC and δ 15 N SON through soil profiles in karst soils were more intensive than those in semiarid grassland soils indicating the less stabilization of SOC and SON in karst soils.

Keywords: soil C and N cycling; stable C and N isotope; karst CZO; Southwest China (search for similar items in EconPapers)
JEL-codes: O13 Q Q0 Q2 Q3 Q5 Q56 (search for similar items in EconPapers)
Date: 2019
References: View references in EconPapers View complete reference list from CitEc
Citations: View citations in EconPapers (4)

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