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Assessment of soil organic carbon in semi-arid Sudan using GIS and the CENTURY model

机译:利用GIS和CENTURY模型评估苏丹半干旱地区的土壤有机碳

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Using the UNFCCC as a basis, and the objectives of estimating soil organic carbon (SOC) changes during the period 1900-2100, a spatially explicit database of climate, land cover and soil texture was compiled for a 262,000km~2 region in semi-arid Sudan. The area is characterized by low input cultivation of millet, sorghum and sesame combined with livestock grazing. By integrating the database with the CENTURY ecosystem model, we were able to estimate historical, current and future pools of SOC as a function of land management and climate. The SOC (upper 20 cm) decrease from 1900 to 2000 was estimated to be 6.8 Mt and the maximum potential carbon sink (SOC increase) for the period 2000 to 2100 was estimated to be 17 Mt. Cropland and grassland lost 293 and 152t SOC km~(-2) respectively whereas the savannahs gained 76 t SOC km~(-2) from 1900 to 2000. The SOC sequestration scenario simulated during 2000-2100 recovered 94, 84 and 75 t km~(-2) for cropland, grassland and savannah respectively. In addition to climate and soils, cropping intensity, fallow periods, fire frequency and grazing intensity also influence cropland SOC variation. Grassland and savannah SOC variations depend on grazing intensity and fire return interval. Land management may affect future amounts of SOC in semi-arid areas thereby turning them from sources into sinks of carbon. SOC estimates were reasonably consistent with measurements (r~2=0.70, n= 13).
机译:以联合国气候变化框架公约(UNFCCC)为基础,并估算1900-2100年期间土壤有机碳(SOC)的变化目标,编制了一个关于空间,土地覆盖和土壤质地的空间明确数据库,该数据库用于半干旱地区的262,000 km〜2地区干旱的苏丹。该地区的特点是小米,高粱和芝麻的低投入种植以及放牧。通过将数据库与CENTURY生态系统模型集成在一起,我们能够根据土地管理和气候来估算SOC的历史,当前和将来。从1900年到2000年的SOC(上20厘米)减少估计为6.8 Mt,从2000年到2100年的最大潜在碳汇(SOC增加)估计为17Mt。从1900年到2000年,耕地和草原分别损失293和152t SOC km〜(-2),而大草原地区增加了76 t SOC km〜(-2)。在2000-2100年模拟的SOC封存情景下恢复了94、84和75 t km 〜(-2)分别表示农田,草原和大草原。除气候和土壤外,耕作强度,休耕期,火灾频率和放牧强度也会影响农田SOC的变化。草原和大草原的SOC变化取决于放牧强度和回火间隔。土地管理可能会影响半干旱地区未来的SOC数量,从而将其从碳源转变为碳汇。 SOC估计值与测量值基本一致(r〜2 = 0.70,n = 13)。

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