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The Moon, 1975
Comminution, agglutination, and replenishment processes in a lunar soil are modeled by a system of time-dependent linear differential equations. In the model, a soil is subdivided into coarse-particle, fine-particle, and agglutinate fractions. The relative mass abundance of each component in a mature soil is found to be proportional to rates for the ...
W. W. Mendell, D. S. McKay
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Comminution, agglutination, and replenishment processes in a lunar soil are modeled by a system of time-dependent linear differential equations. In the model, a soil is subdivided into coarse-particle, fine-particle, and agglutinate fractions. The relative mass abundance of each component in a mature soil is found to be proportional to rates for the ...
W. W. Mendell, D. S. McKay
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Soils and Quaternary Landscape Evolution
The Geographical Journal, 1985This book examines a period of spectacular environmental change, the Quaternary, with respect to soil-landscape relationships in Western Europe, the British Isles and North America. The possibilities for using soils as climatic indicators in the same way as fossils are discussed.
A. S. Goudie, John Boardman
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2004
Soils and archaeological sites are intimately related to the landscape. Investigating soils across past and present landscapes provides a means of reconstructing and understanding the regional environmental and geomorphic context of archaeological site settings and specific site locations, regional site formation processes, and aspects of the resources
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Soils and archaeological sites are intimately related to the landscape. Investigating soils across past and present landscapes provides a means of reconstructing and understanding the regional environmental and geomorphic context of archaeological site settings and specific site locations, regional site formation processes, and aspects of the resources
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THE NATURAL EVOLUTION OF A BURNED SOIL
Soil Science, 1987ABSTRACT Some years ago we performed an experimental burning on a Sardinian soil, characterized by surficial layers of soil that repel water slightly, to clarify the effect of fire on some factors associated with soil erodibility. The experimental plot, after the fire, remained protected by anthropic interference and was subject only to natural ...
G. GIOVANNINI, S. LUCCHESI, M. GIACHETTI
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Use of Soil Maps to Interpret Soil-Landform Assemblages and Soil-Landscape Evolution
2023Soils are a key link to the surficial sedimentologic system(s) that originally deposited the unconsolidated parent material, or to the weathering system that formed the residual parent material. In young soils, i.e., those formed since the end of the Pleistocene, parent materials can often be identified as to type, enabling accurate links to their past
Miller, Bradley +2 more
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Pedogenic evolution of paddy soils in different soil landscapes
Geoderma, 2003Paddy soils are Hydragric Anthrosols and are an important soil resource for food production. They are widely distributed in China and Asia. Soils that can be used for paddy cultivation vary considerably but basically are grouped into three kinds of landscape, i.e., well-drained sloping uplands, alluvial plains with groundwater fluctuation, and poorly ...
Gan-Lin Zhang, Zi-Tong Gong
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Evolution and Biodedegradation of PCB’s in Soil
1995Biphenyls Polychlorids is the generic name of the family of molecules gathering all the isomers resulting of the chlorination of the biphenyle molecule. Each of the 209 different molecules is known as a “congeneer”.
Bernard Chaurial, Jean-Guy Faugere
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Natural products in soil microbe interactions and evolution
Natural Product Reports, 2015Gram positive bacteria from the soil have historically been a deep source of useful natural products. This article considers how natural products may mediate microbial interactions in the soil environment.
Matthew F, Traxler, Roberto, Kolter
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Influence of the soil on certain dermatophytes and their evolutional trend
Mycopathologia et Mycologia Applicata, 1963From our experiments it could be seen that a quite definite relationship exists between various dermatophytes and the soil which is expressed on the one side by antagonistic action of the microflora in the soil inhibiting the growth of dermatophytes and on the other, by ability of some dermatophytes to persist in the soil or to use the soil as habitat ...
E I, GRIN, L, OZEGOVIC
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Evolution of Riser-Soil Stiffness in a Soil Crust Layer
2018Site investigation data have shown that a crust layer may occur at the surface of many seabeds, with the crust exhibiting undrained strengths up to an order of magnitude higher than that of underlying normally consolidated sediments. This may affect the fatigue life assessment of steel catenary riser (SCR) as a result of riser-soil interaction.
Zhechen Hou +3 more
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