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Mapping of soil organic carbon stocks for spatially explicit assessments of climate change mitigation potential

机译:绘制土壤有机碳库,以空间明确地评估气候变化的缓解潜力

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Current methods for assessing soil organic carbon (SOC) stocks are generally not well suited for understanding variations in SOC stocks in landscapes. This is due to the tedious and time-consuming nature of the sampling methods most commonly used to collect bulk density cores, which limits repeatability across large areas, particularly where information is needed on the spatial dynamics of SOC stocks at scales relevant to management and for spatially explicit targeting of climate change mitigation options. In the current study, approaches were explored for (i) field-based estimates of SOC stocks and (ii) mapping of SOC stocks at moderate to high resolution on the basis of data from four widely contrasting ecosystems in East Africa. Estimated SOC stocks for 0–30?cm depth varied both within and between sites, with site averages ranging from 2 to 8?kg?m?2. The differences in SOC stocks were determined in part by rainfall, but more importantly by sand content. Results also indicate that managing soil erosion is a key strategy for reducing SOC loss and hence in mitigation of climate change in these landscapes. Further, maps were developed on the basis of satellite image reflectance data with multiple R-squared values of 0.65 for the independent validation data set, showing variations in SOC stocks across these landscapes. These maps allow for spatially explicit targeting of potential climate change mitigation efforts through soil carbon sequestration, which is one option for climate change mitigation and adaptation. Further, the maps can be used to monitor the impacts of such mitigation efforts over time.
机译:当前评估土壤有机碳(SOC)存量的方法通常不太适合理解景观中SOC存量的变化。这是由于最常用的收集堆积密度核的采样方法的繁琐且耗时的性质,这限制了大面积区域的可重复性,尤其是在需要有关SOC存量与管理和规模相关的空间动态信息的地方在空间上明确针对气候变化缓解方案的目标。在当前的研究中,根据来自东非四个截然不同的生态系统的数据,探索了以下方法:(i)基于实地的SOC储量估算和(ii)中到高分辨率的SOC储量图。站点内部和站点之间估计的SOC深度为0–30?cm均不同,站点平均范围为2到8?kg?m?2。 SOC储量的差异部分取决于降雨,但更重要的是取决于沙含量。结果还表明,控制土壤侵蚀是减少SOC损失并因此减轻这些景观中气候变化的关键策略。此外,基于卫星图像反射率数据(针对独立验证数据集具有0.65的多个R平方值)开发了地图,显示了这些景观中SOC储量的变化。这些地图允许通过土壤固碳来在空间上明确地定位潜在的减缓气候变化的努力,这是减缓和适应气候变化的一种选择。此外,这些地图可用于监视此类缓解措施随时间的影响。

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