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Quantifying soil physical condition based on soil solid, liquid and gaseous phases

机译:根据土壤固相,液相和气相定量土壤物理条件

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Soil is a three-component system comprised of solid, liquid, and gas phases distributed in a complex geometry that creates large solid-liquid, liquid-gas, and gas-solid interfacial areas. Three soil phase index (TSPI) was developed to characterize the physical condition of a medium-textured soil based on solid, liquid, and gaseous phases by utilizing the concept of diminishing marginal productivity expressed in the Cobb-Douglas (C-D) production function. The index was defined as TSPI = [(X-s - C)X1Xs](N). Where C and N are the constants for a given soil, Xis volumetric proportion of the soil phases, the subscripts S, L, and G denote solid, liquid and gaseous phases, respectively. The use of TSPI is exemplified with soils under a series of tillage and traffic practices. To evaluate this new concept, the effects of machinery compaction on TSPI values were compared to selected credible methods for characterizing compaction effects on soil structure. A strong positive relationship was observed. TSPI had a significant relationship with selected soil properties, such as bulk density, oxygen diffusion rate, redox potential, and grain yield which were measured in a field experiment reported in the literature. Furthermore, the correlation of TSPI and the soil physical parameters which is defined as the slope of the soil water retention curve at its inflection point was investigated and a significant linear relationship was also found for soil with given water contents. Overall, the primary advantage of TSPI is that it allows characterizing and evaluating the effects of management practices (e.g., tillage and/or traffic) on the three soil phase condition. Additional testing is needed to evaluate the utility of the index for predicting soil productivity under a wide range of conditions. (C) 2014 Elsevier B.V. All rights reserved.
机译:土壤是由三部分组成的系统,包括以复杂几何形状分布的固相,液相和气相,可形成较大的固液,液气和气固界面区域。通过利用柯布-道格拉斯(C-D)生产函数表示的递减边际生产力的概念,开发了三种土壤相指数(TSPI)以表征基于固相,液相和气相的中等质地土壤的物理条件。该索引定义为TSPI = [(X-s-C)X1Xs](N)。其中C和N是给定土壤的常数,土壤相的Xis体积比例,下标S,L和G分别表示固相,液相和气相。在一系列耕作和交通运输方式下,土壤中例举了TSPI的使用。为了评估这一新概念,将机械压实对TSPI值的影响与用于表征土壤结构压实效果的可靠方法进行了比较。观察到强烈的正相关。 TSPI与选定的土壤特性(如堆密度,氧扩散速率,氧化还原电势和谷物产量)具有显着的关系,这些特性是通过文献报道的田间试验测得的。此外,研究了TSPI与土壤物理参数之间的相关性,土壤物理参数定义为土壤保水曲线在拐点处的斜率,并且在给定含水量的土壤中也发现了显着的线性关系。总体而言,TSPI的主要优势在于它可以表征和评估管理实践(例如耕作和/或交通)对三种土壤阶段条件的影响。需要进行其他测试来评估该指数在多种条件下预测土壤生产力的效用。 (C)2014 Elsevier B.V.保留所有权利。

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