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Analysis of Time Scale Influences on Water and Soil Conservation Effects for Trees on Experimental Plots Using Vegetation Fractional Coverage

机译:利用植被分数覆盖率分析时间尺度对试验区树木水土保持效果的影响

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Five plots representing a gradient of vegetative cover with trees (Pinus massoniana Lamb.) and one control plot were built in 2007 in Changting County of Fujian Province, a typical water-eroded area in southern China. From 2007 to 2010, the rainfall characteristics, vegetation fractional coverage (VFC), runoff depth, and soil loss were measured and/or calculated for the plots after each rainfall event. To explore time scale influences on water and soil conservation effects at (rainfall) event, month, season, and year scales, quadratic polynomial regression models were established between VFC and water (soil) conservation effects [WCE (SCE)]. The WCE (SCE) corresponds to the ratio of runoff (soil loss) of experimental plots with trees to that of the control plot. The results show that, with increasing plot VFC, VFC-WCE and VFC-SCE models presented descending and/or ascending trends, showing linear and nonlinear (transition) effects (positive and/or negative function of the vegetation). This indicates that more environmental factors in addition to vegetation should be taken into account in the conservation management. Observed water conservation effects are not obviously influenced by the time scale, whereas observed soil conservation effects are better (smaller SCEs) at longer time scales, indicating that caution must be taken in the comparison of vegetation effects on water and soil conservation at different time scales. At all time scales, water conservation effects transform when VFC was between 0.5 and 0.6, and soil conservation effects transform when VFC was between 0.3 and 0.7, where "transform" means mutual transformation between positive and negative effects. For both water and soil conservation, the differences in rainfall erosivity among the effect types substantially increased with a longer time scale. This result implies that longer time scales may help differentiate rainfall characteristics for water and soil conservation effects.
机译:2007年,在中国南方典型的水蚀地区-福建省长汀县,建立了五块代表植被覆盖梯度(马尾松)的样地和一个对照样地。从2007年到2010年,在每个降雨事件发生后,针对这些样地测量和/或计算了降雨特征,植被覆盖度(VFC),径流深度和土壤流失。为了探索时间尺度对(降雨)事件,月,季节和年尺度的水和土壤保护效应的影响,在VFC和水(土壤)保护效应之间建立了二次多项式回归模型[WCE(SCE)]。 WCE(SCE)对应于带有树木的试验区与对照区的径流(土壤流失)之比。结果表明,随着地块VFC的增加,VFC-WCE和VFC-SCE模型呈现下降和/或上升趋势,显示线性和非线性(过渡)效应(植被的正向和/或负向作用)。这表明在保护管理中除植被外还应考虑更多环境因素。观察到的节水效果不受时间尺度的影响明显,而观察到的水土保持效果在较长的时间尺度上较好(较小的SCE),这表明在比较不同时间尺度上植被对水土保持的影响时必须谨慎。在所有时间尺度上,当VFC在0.5到0.6之间时,节水效果发生变化,当VFC在0.3到0.7之间时,土壤保持效果发生变化,其中“转换”表示正效应和负效应之间的相互转换。对于水土保持,在更长的时间范围内,效应类型之间的降雨侵蚀力差异大大增加。该结果表明,较长的时间尺度可能有助于区分降雨特征,以实现水土保持作用。

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