土壤持水曲线van Genuchten模型求参的Matlab实现   总被引：15，自引：2，他引：15       下载免费PDF全文

魏义长  刘作新  康玲玲  王云璋  时明立 《土壤学报》2004,41(3):380-386

土壤持水曲线是研究土壤水力学性质必不可少的 ,在已经建立的众多数学模型中 ,vanGenuchten模型是目前运用最广泛的模型 ,而运用该模型的关键是其 4个参数的求解。为此 ,本文对同一组东北褐土的土壤水吸力和对应的土壤含水量数据较详细地介绍了Matlab软件的非线性拟合和非线性回归函数的运用 ,得出了该土壤vanGenuchten模型的 4个参数值 ,分别建立了该土壤的vanGenuchten模型 ,并利用Mat lab强大的绘图功能对它们进行了直观比较。最后运用方差分析和残差分析对该模型的计算值与实测数据进行了分析 ,结果表明 :非线性拟合和非线性回归函数求参结果的显著水平均达到p<0 0 0 0 1,残差平方和均小于 0 0 0 0 5 ,其中非线性回归函数的求参结果较非线性拟合好。因此 ,运用Matlab软件的非线性拟合和非线性回归函数对土壤持水曲线的vanGenuchten模型进行求参是切实可行的 ,从而为土壤学工作者寻求出了一条运用数值计算方法的新途径。  相似文献   

南北方粘质土壤密度对土壤水分特征van Genuchten模型的影响研究     

吕殿青  王玲  潘云  王宏 《灌溉排水学报》2010,29(3)

以南北方典型粘质土壤红壤和塿土为试验土样,通过水平入渗试验进行了土壤密度变化对土壤水分特征van Genuchten模型参数的影响研究。研究结果表明,特征湿润长度、吸力、饱和含水量、滞留含水量、饱和导水率均随土壤密度增加而减小;土壤水分特征van Genuchten模型参数n随着土壤密度的增加而递增,而参数α随着土壤密度的增加而减小,与土壤密度成反比;参数n和参数α随土壤密度变化关系可用幂函数来描述。为建立吸力、土壤密度、质量含水率三变量的土壤水分特征曲面提供新的途径,有助于完善土壤水动力学理论。  相似文献   

农田土壤水分特征曲线参数拟合及其剖面变异特性研究     

车政  王仰仁  王永红  牛永华  罗朋 《灌溉排水学报》2016,(7):22-27

在天津农学院西校区和山西大同阳高试验基地,采用环刀取原状土方法分层、分垂直和水平2个方向取土样,采用高速离心机(CR22GⅡ)方法得到了土壤水分特征曲线数据,利用Van Genuchten模型对实测数据进行了拟合,并运用Excel软件规划求解与模式搜索法交替迭代进行参数拟合优化求解。结果表明,根据实测数据所选的参数初始值和优化值之间有明显差异,以残余含水率差异最大,参数n差异最小;参数优化过程中不同参数随迭代次数的增加有不同的变化规律;不同深度的参数优化值有显著差异,不同方向参数值有一定差异;取样误差对参数的优化结果也有一定的影响。  相似文献   

土壤持水特性参数与土壤质地尺度关系的联合多重分形分析     

WANG Zheng-Ying  SHU Qiao-Sheng  XIE Li-Y  LIU Zuo-Xin  B. C. SI 《土壤圈》2011,21(3):373-379

Soil water-retention characteristics at measurement scales are generally different from those at application scales, and there is scale disparity between them and soil physical properties. The relationships between two water-retention parameters, the scaling parameter related to the inverse of the air-entry pressure (αvG, cm-1) and the curve shape factor related to soil pore-size distribution (n) of the van Genuchten water-retention equation, and soil texture (sand, silt, and clay contents) were examined at multiple scales. One hundred twenty-eight undisturbed soil samples were collected from a 640-m transect located in Fuxin, China. Soil water-retention curves were measured and the van Genuchten parameters were obtained by curve fitting. The relationships between the two parameters and soil texture at the observed scale and at multiple scales were evaluated using Pearson correlation and joint multifractal analyses, respectively. The results of Pearson correlation analysis showed that the parameter αvG was significantly correlated with sand, silt, and clay contents at the observed scale. Joint multifractal analyses, however, indicated that the parameter αvG was not correlated with silt and sand contents at multiple scales. The parameter n was positively correlated with clay content at multiple scales. Sand content was significantly correlated with the parameter n at the observed scale but not at multiple scales. Clay contents were strongly correlated to both water-retention parameters because clay content was relatively low in the soil studied, indicating that water retention was dominated by clay content in the field of this study at all scales. These suggested that multiple-scale analyses were necessary to fully grasp the spatial variability of soil water-retention characteristics.  相似文献   

NaCl胁迫对两种铁线子属果树叶片生理特性的影响   总被引：1，自引：0，他引：1  

刘育梅  胡宏友  童庆宣  李学梅  池敏杰  卢昌义 《热带作物学报》2011,32(9):1679-1682

采用盆栽试验法,对铁线子属果树人心果[Manilkara zapota(L.)van Royen]和古巴牛乳树[Manilkara roxburghiana(Wight)Dubard]进行NaCl胁迫处理,测定叶片的叶绿素、超氧化物歧化酶(SOD)、过氧化物酶(POD)、过氧化氢酶(CAT)、游离脯氨酸、可溶性蛋白等指标及盆土的实际盐度。结果表明,人心果在盐度1.98‰以内、古巴牛乳树在盐度2.42‰以内没有盐害;在NaCl胁迫下,两树种的叶绿素合成受到明显抑制;随着处理浓度增加,人心果叶片的SOD活性升高,各处理浓度下的活性都显著高于对照,但POD和CAT活性呈现先升后降趋势,古巴牛乳树叶片的CAT活性升高,但SOD和POD活性降低,三者活性在各处理浓度下都显著高于对照;人心果叶片的脯氨酸含量在各处理浓度均显著高于对照,可溶性蛋白含量在处理浓度为4‰及以上时显著高于对照,古巴牛乳树叶片的脯氨酸、可溶性蛋白在处理浓度为4‰及以上时显著高于对照,推测脯氨酸、可溶性蛋白作为渗透调节物质在人心果、古巴牛乳树受NaCl胁迫过程中起着重要的作用。  相似文献   

广西岩溶区不同植被类型土壤水分特征及影响因素   总被引：1，自引：1，他引：1  

胡阳  邓艳  蒋忠诚  覃星铭  李衍青 《水土保持通报》2015,35(5):22-27,33

[目的]了解岩溶区不同植被覆盖下的土壤水分特征曲线及其影响因素,为岩溶山区土壤水分运动的定量分析提供理论依据。[方法]通过野外调查与室内分析,研究广西平果果化典型岩溶峰丛洼地荒地、草地、灌丛、林灌4种不同植被覆盖下的土壤水分特征曲线。[结果]van Genuchten模型、Brooks—Corey模型和Gardner 3种模型对土壤水分特征曲线的拟合效果都很好,相关系数均在0.93以上,且残差平方和都小于0.000 5,但van Genuchten模型的拟合效果最好;土壤持水能力与植被的正向演替、饱和含水量、非毛管孔隙度、粉粒含量显著负相关,与土壤容重、黏粒含量、毛管孔隙度、初始含水量和毛管含水量极显著正相关;不同植被类型,相同吸力下,表层和底层土壤的持水能力最强,中间土层的持水能力较差;不同土层深度,相同吸力下,荒地的持水能力最强,林灌的持水能力最差。[结论]同一吸力下的土壤持水能力呈现出随植被的正向演替而不断降低的趋势;研究区影响土壤水分特征曲线的主导因素是非毛管孔隙度。  相似文献   

干旱区膜下滴灌条件下膜孔蒸发特征研究   总被引：1，自引：0，他引：1  

王春霞  王全九  庄亮  单鱼洋  张明 《干旱地区农业研究》2011,29(1):14-21

模拟不同覆膜开孔率下的蒸发试验,研究了蒸发过程中不同覆膜开孔率下土体湿润锋及水盐运移情况的动态分布特征.结果表明:随蒸发历时的延长垂直湿润距离增大,在蒸发1d后垂直湿润距离的增加量最大,蒸发结束时随覆膜开孔率的增大垂直湿润距离减小;随蒸发历时的延长土体剖面内的含水量在减小,表层减小最快,剖面底部边侧含水量有所增加;盐分...  相似文献   

SCALAR LOCALLY UNIQUE SOLUTIONS OF VECTOR VARIATIONAL INEQUALITY     

Li Sheng jie 《保鲜与加工》1996,(1):71-75

This paper first deds with the relations of solutions of vector variational inequality and vector optimization problem. Then, K-T Necessary and sufficient conditions are proved. Finally, scalar locally unique solution is introduced. Under certain conditions,the exitence of scalar locally unique solution of vector variational inequality is proved.  相似文献   

Time-variable soil hydraulic properties in near-surface soil water simulations for different tillage methods     

Andreas Schwen  Gernot Bodner 《Agricultural Water Management》2011,99(1):42-50

Simulating near-surface soil water dynamics is challenging since this soil compartment is temporally highly dynamic as response to climate and crop growth. For accurate simulations the soil hydraulic properties have to be properly known. Although there is evidence that these properties are subject to temporal changes, they are set constant over time in most simulations studies. The objective of this study was to improve near-surface soil water simulations by accounting for time-variable hydraulic properties. Repeated tension infiltrometer measurements over two consecutive seasons were used to inversely estimate the hydraulic properties of a silt loam soil under different tillage - conventional (CT), reduced (RT), and no-tillage (NT). Simulated water dynamics with constant and time-variable hydraulic parameters were compared to observed data in terms of the soil water content and water storage in the near-surface soil profile (0-30 cm). The measurements indicate a considerable temporal variability in the saturated hydraulic conductivity, the field-saturated water content and the parameter α of the van Genuchten/Mualem model. Temporal variability was largest for CT and RT, whereas under NT, replicates of measured water contents and hydraulic properties showed a considerable large spatial variability. Simulations with time-constant hydraulic parameters led to underestimations of soil water dynamics in winter and early spring and overestimations during late spring and summer. The use of time-variable hydraulic parameters significantly improved simulation performance for all treatments, resulting in average relative errors below 13%. Since simulation results agreed with observed water dynamics in two seasons, the applicability of inversely estimated hydraulic properties for soil water simulations is demonstrated. Thus, simulations that address applied questions in agricultural water management may be improved by using time-variable hydraulic parameters. The simulated water balance indicated that RT and NT result in better water storage than CT and therefore may increase water efficiency under water-limited climatic conditions.  相似文献   

基于土壤传递函数的土壤持水特性间接估计及其空间变异性研究   总被引：2，自引：0，他引：2  

LIAO Kai-Hu  XU Shao-Hui  WU Ji-Chun  JI Shu-Hu  LIN Qing 《土壤圈》2011,21(4):413-422

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.  相似文献