使用田间形态评级系统对南艾米利亚土壤进行的土壤学发育。

IF 1.9 Q3 SOIL SCIENCE EGYPTIAN JOURNAL OF SOIL SCIENCE Pub Date : 2021-12-01 DOI:10.21608/ejss.2022.116491.1486
A. Zayed, H. El-Tapey, Abd Monem Al-Toukhy
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引用次数: 0

摘要

本研究采用田间形态评定量表,通过测定土壤的相对水平差异(RHD)和相对剖面发育(RPD)来评价土壤发育。由于气候环境的不同影响,土壤形成过程和因素会对成土因素产生影响,因此利用一些化学和物理性质来评价成土因素。RHD评级是通过对相邻层位的比较得出的。自然地理单元水平上RHD评级的平均值表明,风积沙的土壤比湖积平原的土壤更古老。RPD评级是通过将C水平与剖面中高于C水平的水平进行比较而得出的。Aridisols目下湖相平原的平均RPD等级低于风积沙,风积沙大部分地区属于Entisols目。因此,对土壤发育的研究需要更多的尝试,以包含国际土壤发育的不同特征。
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Pedological development of South El-Amiria soils using field morphology rating system.
he current study was used the field morphological rating scale for evaluating pedological development through determining the Relative Horizons Distinctness (RHD) and the Relative Profile Development (RPD) of soil . Some chemical and physical properties were used to evaluate the pedogenic factors as a result of being affected by process and factors of soil formation due to the distinct effect of climatologically environment. The RHD ratings were made by a comparison of adjacent horizons. Average of RHD ratings on the level of physiographic unit show that soils of windblown sand older than soils of lacustrine plains. The RPD ratings were made by a comparison of the C horizon to the horizons above it in the profile. The average RPD ratings of lacustrine plains under Aridisols order were less than windblown sand, which most area belong to Entisols order. So, studies of pedological development need more attempts to include different features of the international soil development.
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