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祁连山主要植被下土壤水的时空动态变化特征 被引量:38
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作者 牛云 张宏斌 +2 位作者 刘贤德 张学龙 葛双兰 《山地学报》 CSCD 2002年第6期723-726,共4页
通过对祁连山青海云杉林、祁连圆柏林、亚高山灌丛林、牧坡草地等4种主要植被类型的土壤水测量数据进行分析表明,土壤水的空间垂直动态表现为随深度的增加而减少,可划分为土壤水分易变层、利用层、调节层三个层次;土壤水的时间动态可划... 通过对祁连山青海云杉林、祁连圆柏林、亚高山灌丛林、牧坡草地等4种主要植被类型的土壤水测量数据进行分析表明,土壤水的空间垂直动态表现为随深度的增加而减少,可划分为土壤水分易变层、利用层、调节层三个层次;土壤水的时间动态可划分为土壤失水期、聚水期、退水期、稳水期四个时期。土壤水总的特征是,不同植被地类的土壤水季节变化规律基本一致,主要受降水量及其分配的影响。 展开更多
关键词 祁连山 土壤水分时间特征 土壤水分空间特征 土壤含水量
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Assessing Soil Water Retention Characteristics and Their Spatial Variability Using Pedotransfer Functions 被引量:4
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作者 LIAO Kai-Hua1, XU Shao-Hui2,.2, WU Ji-Chun1, JI Shu-Hua2 and LIN Qing2 XU Shao-Hui +2 位作者 WU Ji-Chun JI Shu-Hua LIN Qing 《Pedosphere》 SCIE CAS CSCD 2011年第4期413-422,共10页
A total of 107 soil samples were taken from the city of Qingdao,Shandong Province,China.Soil water retention data at 2.5,6,10,33,100,300,and 1 500 kPa matric potentials were measured using a pressure membrane apparatu... A total of 107 soil samples were taken from the city of Qingdao,Shandong Province,China.Soil water retention data at 2.5,6,10,33,100,300,and 1 500 kPa matric potentials were measured using a pressure membrane apparatus.Multiple linear regression (MLR) was used to develop pedotransfer functions (PTFs) for single point estimation and van Genuchten parameter estimation based on readily measurable soil properties,i.e.,MLR-based point (MLRP) PTF and MLR-based parametric (MLRV) PTF.The double cross-validation method was used to evaluate the accuracy of PTF estimates and the stability of the PTFs developed in this study.The performance of MLRP and MLRV PTFs in estimating water contents at matric potentials of 10,33,and 1 500 kPa was compared with that of two existing PTFs,the Rawls PTF and the Vereecken PTF.In addition,geostatistical analyses were conducted to assess the capabilities of these PTFs in describing the spatial variability of soil water retention characteristics.Results showed that among all PTFs only the Vereecken PTF failed to accurately estimate water retention characteristics.Although the MLRP PTF can be used to predict retention characteristics through traditional statistical analyses,it failed to describe the spatial variability of soil water retention characteristics.Although the MLRV and Rawls PTFs failed to describe the spatial variability of water contents at a matric potential of 10 kPa,they can be used to quantify the spatial variability of water contents at matric potentials of 33 and 1 500 kPa. 展开更多
关键词 double cross-validation method multiple linear regression soil water content van Genuchten parameter
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