南非北开普省(Loopeng地区)的案例研究,证实了运输土壤中存在可塌陷土壤结构

IF 1.2 4区 地球科学 Q2 GEOLOGY
F. Stapelberg
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引用次数: 0

摘要

对南非北开普省最近沉积的砂质粉土沉积物的运输土壤进行了测试,以确定坍塌砂土结构的发生和数量级。各种经验岩土特征,包括:现场土壤剖面结构描述、颗粒级配曲线和粘土含量、土壤分类、,将土壤密度和孔隙比与固结仪测试确定的潜在坍塌值进行比较,以判断经验特征是否能够成功地用于预测湿陷性土壤结构的发生。从结果中可以清楚地看出,在运输的土壤中存在坍塌的砂土结构,与之前对坍塌砂土的研究相比,经验描述符大多正确地指示了具体土壤结构的发生。反映描述符和土壤结构之间相对较差的校正的一个描述符(原位土壤剖面结构描述)被认为是湿陷性土壤结构的较差指标,尘土飞扬的土壤条件和试验坑侧壁非常短暂的完整竖立时间。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Case Study in The Northern Cape (Loopeng Area), South Africa, Confirming Occurrence of a Collapsible Soil Structure in Transported Soils
Testing was performed on transported soils belonging to recently deposited sandy-silty soil deposits occurring in the Northern Cape Province, South Africa in order to determine the occurrence and order of magnitude of a collapsing sand soil structure. Various empirical geotechnical characteristics including: in situ soil profile structure description, particle grading curve and clay content, soil classification, soil density and void ratio were compared to collapse potential values determined with oedometer testing in order to judge the success with which the empirical characteristics can be utilized to predict the occurrence of a collapsible soil structure.From the results it is clear that a collapsing sand structure exists in the transported soils and the empirical descriptors mostly correctly indicate the occurrence or the particular soil structure when compared to previous studies on collapsing sands. The one descriptor which reflects a relatively poor correction between the descriptor and the soil structure (in situ soil profile structure description) is considered to be a poor indicator of the collapsible soil structure due to erroneous or poor in situ soil structure observations resulting from unfavourable local conditions namely dry, dusty soil conditions and very brief intact standup time of test pit side walls.
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来源期刊
CiteScore
3.60
自引率
5.60%
发文量
18
审稿时长
>12 weeks
期刊介绍: The South African Journal of Geology publishes scientific papers, notes, stratigraphic descriptions and discussions in the broadly defined fields of geoscience that are related directly or indirectly to the geology of Africa. Contributions relevant to former supercontinental entities such as Gondwana and Rodinia are also welcome as are topical studies on any geoscience-related discipline. Review papers are welcome as long as they represent original, new syntheses. Special issues are also encouraged but terms for these must be negotiated with the Editors.
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