中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
陕北黄土丘陵沟壑区人工草地的土壤水分植被承载力

文献类型:期刊论文

作者王延平 ; 邵明安
刊名农 业 工 程 学 报
出版日期2012
卷号28期号:18页码:134-141
关键词土壤水分 soil moisture 蒸散量 evaporation 动态分析 dynamic analysis 陕北黄土区 loess region in Northern Shaanxi 苜蓿 alfalfa 土壤水分植被承载力 vegetation
其他题名Vegetation soil water carrying capacity of artificial pasture in loess
中文摘要土壤水分植被承载力是黄土高原生态环境建设和可持续发展的核心。该文根据陕北黄土区4种不同立地条件下苜蓿地(MedicagosativaL.)连续3a的降雨、径流、土壤水分动态和生物产量的小区定位观测结果,研究分析了自然降水与土壤水分补给、土壤水分补给与地上部生物量、地上部生物量与土壤水分消耗的关系;并采用FAO法和水量平衡法分别计算出了苜蓿地土壤水分的承载力。结果表明:苜蓿地土壤水分补给量与地上部生物量呈线性关系,地上部生物量与土壤水分消耗量呈二次函数关系。用FAO法估算可得陕北黄土区土壤水分可承载的苜蓿最大产量为3992.2~4173.7kg/hm2;而根据水量平衡原理计算可得陕北黄土区苜蓿地可承载的地上部生物量为2600~3500kg/hm2,比FAO法低16.07%~33.52%。坡向、坡位相同时,坡度增大,承载力降低;坡向、坡度相同时,下坡承载力大于上坡;坡度、坡位相同时,南坡承载力小于北坡。
英文摘要Vegetation carrying capacity of soil water is the key of the ecological environmental construction and
sustainable development in the Loess Plateau. Based on local monitoring data of rainfall, runoff, soil moisture
dynamics and Biomass under condition of 4 different sites in loess region of Northern Shaanxi from 2008 to 2010,
relationships between natural precipitation and soil water supply, soil water supply and biomass, biomass and soil
water consumption were analysed and established in this paper, and Soil Water Carrying Capacity of alfalfa had
been separately calculated by FAO method and water balance method. The results showed that: in alfalfa land
replenishment of soil moisture in alfalfa land and biomass showed a linear relationship; biomass and soil moisture
consumption was a quadratic function. By using FAO method, it could be estimated that the maximum alfalfa
yield of soil moisture can bear was 3 992.2 to 4 173.7 kg/hm2 in Northern Shaanxi’s Loess Plateau; however, the
biomass was estimated by water balance method was 2 600 to 3 500 kg/hm2, it was 16.07% to 33.52% less than
the result estimated with FAO method. With the same aspect and position, capacity reduced while slope was
increasing. With the same aspect and position, capacity downhill was larger than that uphill. With the same slope
and position, capacity in southern slope was smaller than that in northern slope.
语种中文
公开日期2014-06-24
源URL[http://ir.iswc.ac.cn/handle/361005/5329]  
专题水土保持研究所_水保所知识产出(1956-2013)
推荐引用方式
GB/T 7714
王延平,邵明安. 陕北黄土丘陵沟壑区人工草地的土壤水分植被承载力[J]. 农 业 工 程 学 报,2012,28(18):134-141.
APA 王延平,&邵明安.(2012).陕北黄土丘陵沟壑区人工草地的土壤水分植被承载力.农 业 工 程 学 报,28(18),134-141.
MLA 王延平,et al."陕北黄土丘陵沟壑区人工草地的土壤水分植被承载力".农 业 工 程 学 报 28.18(2012):134-141.

入库方式: OAI收割

来源:水土保持研究所

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