Identification of plant soil water and soil aeration corequisites: A management tool

Beaulah Pragg, M. M. T. Lakshani, T. K. K. Chamindu Deepagoda, Keith Cameron, Hong Di, Timothy J. Clough, Sam Carrick, Bo Elberling, K. Smits
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Abstract

Plant-available soil-water and adequate soil aeration within the root zone are essential corequisites for successful plant growth. Characterization of these two requirements for plant growth is generally done by independent measurements of water and air phase properties and functions in soil, with limited emphasis on their combined effect. This study investigated soil-water characteristic (SWC) measurements in vadose soil profiles (up to 117-cm depth) in six pasture soils to examine the combined behavior of soil-water and diffusion-controlled aeration within the root zone. The soil moisture measurements were made over matric potentials ranging from −1 to −1500 kPa using tension table and pressure plate apparatus. The van Genuchten model was used to parameterize the measured SWC curve, while the Millington–Quick model was used to derive soil-gas diffusivity from measured soil physical properties. Based on two simple indices, derived to represent plant-available soil-water and soil aeration status at a given moisture content, we propose an assessment matrix, which illustrates how a soil satisfies the corequisites for successful plant growth, as it drains to different matric potentials upon irrigation. Results show a pronounced effect of soil texture and, to a lesser extent, soil structure on satisfying these corequisites. With the aid of the assessment matrix, we observed that loam, sandy loam textures exhibited a good overall performance, while sand, clay loam, and clay soils struggled to meet these corequisites during drainage.

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确定植物土壤水分和土壤通气核心条件:管理工具
植物根区可利用的土壤水和充分的土壤通气是植物成功生长的必要核心条件。对植物生长的这两项要求的特征描述通常是通过对土壤中水相和气相的特性和功能进行独立测量来完成的,而对它们的综合效应的强调却很有限。本研究调查了六种牧场土壤中伏流土壤剖面(最深 117 厘米)的土壤水分特征(SWC)测量结果,以研究根区土壤水分和扩散控制曝气的综合行为。土壤水分测量是使用拉力台和压力板仪器在-1 到 -1500 kPa 的母质电位范围内进行的。Van Genuchten 模型用于对测量的 SWC 曲线进行参数化,而 MillingtonQuick 模型则用于从测量的土壤物理特性推导出土壤-气体扩散率。根据两个简单的指数,我们提出了一个评估矩阵,这两个指数代表了在给定含水量下植物可利用的土壤水分和土壤通气状况,说明了土壤在灌溉后排水到不同的熟化电位时,如何满足植物成功生长的核心条件。结果表明,土壤质地对满足这些核心条件有明显影响,其次是土壤结构。借助评估矩阵,我们观察到壤土、沙壤土的质地表现出良好的整体性能,而沙土、粘壤土和粘土在排水过程中难以满足这些核心条件。
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