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The dynamics of soil redistribution and the implications for soil organic carbon accounting in agricultural south-eastern Australia

机译:澳大利亚东南部农业地区土壤再分配动态及其对土壤有机碳核算的影响

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摘要

Anthropogenically induced change in soil redistribution plays an important role in the soil organic carbon (SOC) budget. Uncertainty of its impact is large because of the dearth of recent soil redistribution estimates concomitant with changing land use and management practices. An Australian national survey used the artificial radionuclide caesium-137 (137Cs) to estimate net (1950s1990) soil redistribution. South-eastern Australia showed a median net soil loss of 9.7tha-1yr-1. We resurveyed the region using the same 137Cs technique and found a median net (19902010) soil gain of 3.9tha-1yr-1 with an interquartile range from -1.6tha-1yr-1 to +10.7tha-1yr-1. Despite this variation, soil erosion across the region has declined as a likely consequence of the widespread adoption of soil conservation measures over the last ca 30years. The implication of omitted soil redistribution dynamics in SOC accounting is to increase uncertainty and diminish its accuracy.
机译:人为诱发的土壤重新分布变化在土壤有机碳(SOC)预算中起重要作用。其影响的不确定性很大,因为最近的土壤再分配估计与土地使用和管理方式的变化相伴而生。澳大利亚的一项全国调查使用了人工放射性核素铯137(137Cs)来估算土壤(1950年代至1990年)的净再分配。澳大利亚东南部的土壤净流失中位数为9.7tha-1yr-1。我们使用相同的137Cs技术对区域进行了调查,发现土壤净中值(19902010)为3.9tha-1yr-1,四分位数范围为-1.6tha-1yr-1至+ 10.7tha-1yr-1。尽管存在这种差异,但由于过去约30年广泛采用土壤保护措施,该地区的土壤侵蚀有所减少。 SOC会计中忽略土壤重新分配动力学的含义是增加不确定性并降低其准确性。

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