Please use this identifier to cite or link to this item: http://nopr.niscpr.res.in/handle/123456789/17336
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dc.contributor.authorCalla, O P N-
dc.contributor.authorBorah, M C-
dc.contributor.authorVashishtha, P-
dc.contributor.authorMishra, R-
dc.contributor.authorBhattacharya, A-
dc.contributor.authorPurohit, S P-
dc.date.accessioned2013-04-26T08:49:14Z-
dc.date.available2013-04-26T08:49:14Z-
dc.date.issued1999-06-
dc.identifier.issn0975-105X (Online); 0367-8393 (Print)-
dc.identifier.urihttp://hdl.handle.net/123456789/17336-
dc.description109-112en_US
dc.description.abstractMicrowave emission and backscattering of the soil depend on its dielectric constant which is effected by the moisture content in soil. The knowledge of variability of soil moisture is important for agriculture. The properties, chiefly the dielectric constant, comprising both storage and loss of loamy sand having different moisture content by weight, has been studied extensively in the laboratory at a wide range of microwave frequencies from 2 GHz to 20 GHz. The measurements have been made using HP network analyzer and HP dielectric probe employing coaxial probe method. The dielectric constant increases slowly up to certain point and then with the increase of moisture the change is rapid. At higher frequencies the change in loss factor is more than that at lower frequencies.en_US
dc.language.isoen_USen_US
dc.publisherNISCAIR-CSIR, Indiaen_US
dc.rights CC Attribution-Noncommercial-No Derivative Works 2.5 Indiaen_US
dc.sourceIJRSP Vol.28(3) [June 1999]en_US
dc.titleStudy of the properties of dry and wet loamy sand soil at microwave frequenciesen_US
dc.typeArticleen_US
Appears in Collections:IJRSP Vol.28(3) [June 1999]

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