首页> 外文期刊>Paddy and Water Environment >Pedo-transfer function for saturated hydraulic conductivity of lowland paddy soils
【24h】

Pedo-transfer function for saturated hydraulic conductivity of lowland paddy soils

机译:坡道传递函数对低地稻田土壤饱和导水率的影响

获取原文
获取原文并翻译 | 示例
           

摘要

In paddy field, soil saturated hydraulic conductivity (K_s) plays as an important component in the calculation of irrigation requirement of the water balance equation and also for irrigation efficiency. Several laboratory and field methods can be usedto determine K_s. Laboratory and field determinations are usually time consuming, expensive and labour intensive. Pedo-transfer functions (PTF) serve to translate the basic information found in the soil survey into a form useful for broader applicationsthrough empirical regression of functional relationships, such as simulation modelling. Since PTFs have not been applied to paddy soils in the study area, a lot of field measurements will require high labour input to determine hence high cost. This study attempts to seek a simplified method for determining values based on common existing soil properties through PTF technique. Soil samples (n = 408 samples) were collected randomly depending on the soil series within the 2,300 ha Sawah Sempadan rice cultivation area. Both field work and laboratory work were carried out. The samples were then analysed for the following properties: dry bulk density (Db), soil particle percentage (Sand-S, Silt-Si and Clay-C), organic matter (OM) and geometric mean diameter(GMD). The measured K_s values were obtained by using the falling head method. The parameters were then used as inputs for developing a model by regression analysis using Statistical Analysis System (SAS) package. Stepwise regression analysis was applied to determine the best fit model based on R~2 and significant level. The results of the study showed that there is a high spatial variability of the saturated hydraulic conductivity in the paddy area. The best regression model for estimating was based on C, D_b, OM and GMD with the dependent variable (K_S in a form of natural logarithm. The model inputs introduced by stepwise regression are commonly available therefore, this model is useful to replace the conventional method.
机译:在稻田中,土壤饱和导水率(K_s)在计算水平衡方程的灌溉需求以及灌溉效率中起着重要的作用。可以使用几种实验室和现场方法来确定K_s。实验室和现场测定通常很耗时,昂贵且劳动强度大。 Pedo传递函数(PTF)用于通过对功能关系进行经验回归(例如模拟建模)将土壤调查中发现的基本信息转换为对更广泛的应用有用的形式。由于PTF尚未应用于研究区域的稻田土壤,因此许多田间测量将需要大量的劳动力投入才能确定高成本。这项研究试图寻求一种简化的方法,通过PTF技术基于现有的常见土壤特性确定值。根据2,300公顷Sawah Sempadan水稻种植区的土壤系列,随机收集土壤样品(n = 408个样品)。进行了现场工作和实验室工作。然后分析样品的以下特性:干堆积密度(Db),土壤颗粒百分比(Sand-S,Silt-Si和Clay-C),有机物(OM)和几何平均直径(GMD)。通过使用落头法获得测量的K_s值。然后将这些参数用作通过使用统计分析系统(SAS)软件包进行回归分析来开发模型的输入。基于R〜2和显着性水平,采用逐步回归分析确定最佳拟合模型。研究结果表明,稻田中饱和导水率的空间变异性很大。最佳的估计回归模型是基于C,D_b,OM和GMD以及因变量(自然对数形式的K_S。通过逐步回归引入的模型输入是通用的,因此,该模型可用于替代常规方法。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号