期刊
CATENA
卷 229, 期 -, 页码 -出版社
ELSEVIER
DOI: 10.1016/j.catena.2023.107198
关键词
Soil organic carbon density; Topsoil; Diagnostic surface horizon; Chinese Soil Taxonomy; Soil profile; Horizon delineation
This study evaluated the topsoil organic carbon density (TSOCD) of China using a diagnostic surface horizon (DSH)-based topsoil classification method. The results showed that the TSOCD ranged from 0.03 to 74.63 kg m(-2) with a mean value of 4.34 kg m(-2). The study also demonstrated that specific uniform thickness delineations were suitable for particular soil types, climatic conditions, and land use patterns, and that these delineations yielded similar results to those based on DSH.
Accurate assessment of the topsoil organic carbon density (TSOCD) is of great importance for the management and conservation of the topsoil organic carbon pools. The conventional surface horizon (CSH) delineation method, which involves specifying a uniform topsoil thickness for all sampling points across a study area, carries the potential risk of inaccurate TSOCD estimation. Chinese soil scientists developed the definition and deter-mination criteria for diagnostic surface horizon (DSH) in Chinese Soil Taxonomy (CST), which were based on the distinctive characteristics of topsoil in China. This study employed a DSH-based topsoil classification method to evaluate the TSOCD of China, based on the findings of the recent national soil survey. Also, TSOCD was calculated for all sample points based on the CSH method, where the thickness of CSH was defined as 5, 10, 15, 20, 30, and 60 cm from the surface. The results showed that DSH-based TSOCD in China ranged from 0.03 to 74.63 kg m(-2) with a mean value of 4.34 kg m(- 2). The standardized topsoil delineation based on the DSH method shows great potential for improving the accuracy of TSOCD assessment and different DSH types exhibited very significant differences in TSOCD (p < 0.01). There was a significant difference between the TSOCD results based on the six CSH delineation thicknesses (p < 0.01). Excessive or insufficient uniform CSH thickness settings may result in over-or underestimation of TSOCD values in comparison to DSH. This study provides evidence that specific uniform thickness delineations are suitable for particular soil types, climatic conditions, and land use patterns, and that the mean TSOCD results derived from these delineations do not significantly differ (p < 0.01) from those based on DSH. The findings of this study have the potential to support the development of more accurate surface horizon delineation methods for managing and making decisions related to topsoil organic carbon pools.
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