Characterization of soil moisture dynamics in Colombian agricultural areas

Francisco Javier Hernández-Guzmán, J. Cleves-Leguízamo, Eliecer David Díaz-Almanza
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引用次数: 1

Abstract

Seasonal dynamics in edaphic humidity are influenced by different environmental factors, such as topography, physical and chemical soil conditions, type of vegetation cover and climatic classification. Data from 105 agrometeorological stations in the IDEAM network, distributed throughout Colombia, with records from January, 2001 to April, 2020, were studied. A non-parametric Spearman rank correlation test was used to evaluate the relationship between soil moisture and atmospheric variables. Simultaneously, the behaviors of seasonal dynamics were analyzed, along with their interaction with atmospheric, physical soil and vegetation cover variables. The results showed that soil moisture is more significantly influenced by frequency than by intensity of precipitation; this variable had a seasonal behavior, similar to that of precipitation. The physical variable texture was closely related to the behavior of the soil surface moisture (<10 cm deep). In addition, there was evidence of a surface moisture response to the physical conditions of the soil, topography and availability of plant cover. As the soil depth increased, the soil moisture had less variation because the influence of the atmospheric conditions was greater on the surface and persisted longer over time.
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哥伦比亚农业区土壤水分动态特征
土壤湿度的季节动态受地形、土壤理化条件、植被覆盖类型和气候分类等环境因子的影响。研究了分布在哥伦比亚各地的IDEAM网络105个农业气象站2001年1月至2020年4月的记录数据。采用非参数Spearman秩相关检验评价土壤湿度与大气变量之间的关系。同时,分析了季节动态特征及其与大气、土壤物理和植被覆盖变量的相互作用。结果表明:降水频率对土壤湿度的影响比对降水强度的影响更显著;这个变量具有季节性行为,类似于降水。物理变构与土壤表层水分(<10 cm深)的变化密切相关。此外,有证据表明,地表水分对土壤的物理条件、地形和植物覆盖的有效性有响应。随着土壤深度的增加,土壤湿度的变化较小,因为大气条件对地表的影响更大,持续时间更长。
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