首页> 外文期刊>Acta Agriculturae Scandinavica. Section B, Soil and Plant Science >Effects of the implementation of ecological restoration policies on soil organic carbon storage in a discontinuous soil region.
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Effects of the implementation of ecological restoration policies on soil organic carbon storage in a discontinuous soil region.

机译:生态恢复政策的实施对不连续土壤区土壤有机碳储量的影响。

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摘要

Estimating soil organic carbon (SOC) storage for soils with discontinuous distribution in the karst regions of southwest China poses a challenge due to the predominant carbonate bedrock. In addition, it is not clear how effective the ecological restoration and reconstruction policies, which have been conducted in this region since the 1990s, have been in terms of SOC sequestration. In this study, we explored the ability of an empirical model and validated it using field survey data to predict the coverage of discontinuous distribution soil in a karst region in southwest China. Employing the soil coverage map, survey data of SOC at a soil depth of 0-15 cm, and three land use/cover maps in 1990, 2004, and 2011, we estimated the changes of SOC storages in the study area. Results showed that the land use/cover changes induced by the implementation of ecological restoration policies promoted SOC storage in the karst region. The SOC storage increased from 2.34 Tg to 3.01 Tg and soil organic carbon density increased from 2.72 kg/m2 to 3.50 kg/m2 over the study period. The mountain closure policy, Grain for Green program, and migration program currently implemented in the karst region have contributed to a decline in the rate of SOC decomposition and the reduction of soil disturbance, which resulted in carbon sequestration in the global carbon cycle while also improving the ecologically fragile karst environment. SOC storage may have been overestimated by almost twofold while ignoring the discontinuous distribution features of soil cover in the karst region. However, along with an increase in both population and agricultural activities, SOC storage in the nonkarst area declined from 1990 to 2011. With the ecological restoration occurring in the karst area, losses of SOC induced by increased farming activities in the nonkarst area should not be ignored.
机译:由于碳酸盐岩基岩含量较高,因此估算西南喀斯特地区不连续分布的土壤的有机碳(SOC)储量是一个挑战。此外,尚不清楚自1990年代以来在该地区实施的生态恢复和重建政策在SOC隔离方面是否有效。在这项研究中,我们探索了经验模型的能力,并使用现场调查数据对其进行了验证,以预测中国西南喀斯特地区不连续分布土壤的覆盖率。利用土壤覆盖图,土壤深度为0-15 cm的SOC的调查数据以及1990年,2004年和2011年的三幅土地利用/覆盖图,我们估算了研究区域的SOC储量的变化。结果表明,生态恢复政策的实施引起的土地利用/覆盖变化促进了喀斯特地区的SOC储存。在研究期间,SOC储存量从2.34 Tg增加到3.01 Tg,土壤有机碳密度从2.72 kg / m 2 增加到3.50 kg / m 2 。目前在喀斯特地区实施的封山政策,“绿色粮食计划”和移民计划导致了SOC分解速率下降和土壤扰动减少,从而导致全球碳循环中的碳固存,同时也改善了生态脆弱的喀斯特环境。忽略了喀斯特地区土壤覆盖的不连续分布特征,SOC储量可能被高估了将近两倍。但是,随着人口和农业活动的增加,非喀斯特地区的SOC储量从1990年到2011年有所下降。由于喀斯特地区发生了生态恢复,因此不应因非喀斯特地区的农业活动增加而导致SOC的损失。忽略了。

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