Plastic limits of agricultural soils as functions of soil texture and organic matter content

被引:79
|
作者
Keller, Thomas [1 ,2 ]
Dexter, Anthony R. [3 ]
机构
[1] Agroscope Reckenholz Tanikon Res Stn ART, Dept Nat Resources & Agr, CH-8046 Zurich, Switzerland
[2] Swedish Univ Agr Sci, Dept Soil & Environm, SE-75007 Uppsala, Sweden
[3] Inst Soil Sci & Plant Cultivat IUNG PIB, PL-24100 Pulawy, Poland
关键词
Atterberg consistency limits; clay; liquid limit; pedo-transfer function; plasticity index; ALTERNATIVE TEST PROCEDURES; LINEAR-REGRESSION MODELS; MECHANICAL-PROPERTIES; I[!text type='JS']JS[!/text]SELMEER POLDERS; WATER CONTENT; TOP SOILS; TILLAGE; REEXAMINATION; COMPRESSION; COMPACTION;
D O I
10.1071/SR11174
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
The plastic limits (lower plastic limit, PL; and liquid limit, LL) are important soil properties that can yield information on soil mechanical behaviour. The objective of this paper is to study the plastic limits of agricultural soils as functions of soil texture and organic matter (OM) content. The plastic limits were highly related to the clay content. The LL was more strongly correlated with clay than was PL, but the reasons are unclear. Interestingly, PL was virtually unaffected by clay content for soils with clay contents below similar to 35%. The OM had a strong effect on the plastic limits. This effect was clearly demonstrated when analysing soils of similar texture with a range of OM. We present equations (pedotransfer functions) for estimation of PL, LL, and plasticity index (PI) from soil texture and OM. Finally, we predict that the clay content must be >= 10% for soils without OM to be plastic; however, soils with <10% clay can be plastic if OM is present. More research is needed to investigate OM effects on soil consistency.
引用
收藏
页码:7 / 17
页数:11
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