{"title":"The use of pore volume characteristics and soil moisture release curve to determine physical quality of soils with different gypsum contents","authors":"A. Al-Kayssi, A. Salman","doi":"10.52113/mjas04/8.3/30s","DOIUrl":null,"url":null,"abstract":"\"A newly proposed concept of soil physical quality and its development as a guide to assess the extent of soil degradation or improvement and to determine appropriate soil management. The study aimed to: evaluate the soil physical quality index of gypsiferous soils under different management systems as well as determine the optimal pore size distribution and the optimum moisture-tension curve based on the quality of the physical soil properties under different management systems and diagnose the distribution of pore sizes and moisture-tension curves that could be used to predict the changes in the physical quality of gypsiferous soils because of the applied agricultural management pattern. Physical indicators measured on undisturbed soil samples collected from 15 selected sites in Salah Aldeen Governorate, with different gypsum content (30 to 301 g kg-1 soil). The results showed that the best distribution of measured pore size (h) S *, (Normalized pore volume) was for a group of soils that were largely similar in terms of shape and location parameters. Accordingly, the optimal pore distribution considered representative of these soils. The results showed the possibility of using the (Dexter-S) indicator correctly and in coordination with the distribution of pore size and the soil moisture characteristic curve to calculate the physical soil quality in soils of different gypsum content.","PeriodicalId":18776,"journal":{"name":"Muthanna Journal for Agricultural Sciences","volume":null,"pages":null},"PeriodicalIF":0.0000,"publicationDate":"2021-03-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Muthanna Journal for Agricultural Sciences","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.52113/mjas04/8.3/30s","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
"A newly proposed concept of soil physical quality and its development as a guide to assess the extent of soil degradation or improvement and to determine appropriate soil management. The study aimed to: evaluate the soil physical quality index of gypsiferous soils under different management systems as well as determine the optimal pore size distribution and the optimum moisture-tension curve based on the quality of the physical soil properties under different management systems and diagnose the distribution of pore sizes and moisture-tension curves that could be used to predict the changes in the physical quality of gypsiferous soils because of the applied agricultural management pattern. Physical indicators measured on undisturbed soil samples collected from 15 selected sites in Salah Aldeen Governorate, with different gypsum content (30 to 301 g kg-1 soil). The results showed that the best distribution of measured pore size (h) S *, (Normalized pore volume) was for a group of soils that were largely similar in terms of shape and location parameters. Accordingly, the optimal pore distribution considered representative of these soils. The results showed the possibility of using the (Dexter-S) indicator correctly and in coordination with the distribution of pore size and the soil moisture characteristic curve to calculate the physical soil quality in soils of different gypsum content.
“新提出的土壤物理质量及其发展概念,作为评估土壤退化或改善程度和确定适当土壤管理的指南。这项研究的目的是:评价不同管理制度下的石膏质土的土壤物理质量指标,根据不同管理制度下土壤物理性质的质量,确定最佳孔隙大小分布和最佳水分-张力曲线,诊断出孔隙大小和水分-张力曲线的分布,可用于预测应用农业管理模式对石膏质土物理质量的影响。对从Salah Aldeen省15个选定地点收集的未受干扰的土壤样品进行了物理指标测量,这些样品具有不同的石膏含量(30至301 g kg-1土壤)。结果表明,在一组形状和位置参数基本相似的土壤中,测量孔径(h) S *,(归一化孔体积)的最佳分布。因此,最佳孔隙分布被认为是这些土壤的代表性。结果表明,在不同石膏含量的土壤中,正确使用(Dexter-S)指标,并与孔隙大小分布和土壤水分特征曲线相协调,计算土壤物理质量是可能的。