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Using live vegetation volume to analyze the effects of plot Pinus massoniana Lamb on water and soil conservation under natural rainfall events
Authors:Zhu-jun GU  Xiao-xia WU  Xiao-lei WANG  Shao-yun PENG  Hao LUO  Xue-zheng SHI  Dong-sheng YU
Institution:[1]School of Bio-Chemical and Environmental Engineering, Nanjing Xiaozhuang University, Nanjing 211171, China [2]School of Bio-Cheemical and Environmental Engineering, Nanjing Xiaozhuang University, Nanjing 211171, China [3]Engineer, Fujian Changting Bureau of soil and water conservation, Changting 366300, China [4]Engineer, Institute of Hydro-geophysical prospecting, Chongqing Research Institute of China Coal Technology & Engineering Group Corporation, Chongqing 400039, China [5]State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008, China
Abstract:The 3-D spatial distributions of vegetation are of great significance for water and soil conservation but are rarely concerned in literatures. The live vegetation volume (LVV) was used to relate to water/soil loss under 144 natural erosive rainfall events from 2007 to 2010 in a typical water-eroded area of southern China. Quadratic polynomial regression models were established for five pure tree (Pinus massoniana Lamb) plots between LVV and water (runoff)/soil conservation effects (RE/SE). RE/SE corresponds to the ratios of runoff depth/soil loss of the pure tree plots to that of the control plot under each rainfall event. Increasing LVV exhibits descending (DS), descending-ascending (DA), ascending-descending (AD), and ascending (AS) trends in the LVV–RE and LVV–SE curves. The effects of soil conservation on the plots were generally more noticeable than the effects of water conservation, and most of the RE and SE values reflected the positive effects of water and soil conservation. The effects were mainly positive under heavy rains (e.g., rainfall erosivity, R = 140 MJ mm ha?1 h, maximum 30 min intensity, I30 = 16 mm h?1), whereas the effects were mainly negative under light rains (e.g., R = 45 MJ mm ha?1 h, I30 = 8 mm h?1). The trees' water/soil conservation effects notably transformed when rainfall erosivity and intensity were lower than the positive or negative effects to a certain threshold. About 50% rainfall events led to obvious transform effects when LVVs were near 0.5 or 0.6. These results are able to aid in the decision making on the forest reconstruction in water-eroded areas.
Keywords:Erosion  Forest  Runoff  Transform live vegetation volume  Water and soil conservation
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