{"title":"An index value for characterizing hardsetting soils by fall-cone penetration","authors":"H.H. Becher, J. Breuer , B. Klingler","doi":"10.1016/0933-3630(95)00043-7","DOIUrl":null,"url":null,"abstract":"<div><p>The measurement of fall-cone penetration on air-dried and slowly rewetted subsamples (< 1 mm) at different water contents characterizes hardsetting and non-hardsetting soils by differences in their maximum resistance to penetration (RP<sub>max</sub>), the water content (WC<sub>max</sub>) at RP<sub>max</sub>, and the amount of water adsorbed between the two values of 0.5 × RP<sub>max</sub>, called ‘insensitivity’ <em>I</em>. The insensitivity <em>I</em> is strongly correlated with the contents of organic matter and iron oxides which are considered as soil components improving aggregation. The insensitivity may be used to identify hardsetting soils. These have <em>I</em>-values < 7, whereas non-hardsetting soils have <em>I</em>-values > 10.</p></div>","PeriodicalId":101170,"journal":{"name":"Soil Technology","volume":"10 1","pages":"Pages 47-56"},"PeriodicalIF":0.0000,"publicationDate":"1997-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/0933-3630(95)00043-7","citationCount":"28","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Soil Technology","FirstCategoryId":"1085","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/0933363095000437","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 28
Abstract
The measurement of fall-cone penetration on air-dried and slowly rewetted subsamples (< 1 mm) at different water contents characterizes hardsetting and non-hardsetting soils by differences in their maximum resistance to penetration (RPmax), the water content (WCmax) at RPmax, and the amount of water adsorbed between the two values of 0.5 × RPmax, called ‘insensitivity’ I. The insensitivity I is strongly correlated with the contents of organic matter and iron oxides which are considered as soil components improving aggregation. The insensitivity may be used to identify hardsetting soils. These have I-values < 7, whereas non-hardsetting soils have I-values > 10.