dc.contributor.author |
Poulovassilis, A |
en |
dc.contributor.author |
Kerkides, P |
en |
dc.contributor.author |
Alexandris, S |
en |
dc.contributor.author |
Rizos, S |
en |
dc.date.accessioned |
2014-06-06T06:43:35Z |
|
dc.date.available |
2014-06-06T06:43:35Z |
|
dc.date.issued |
1998 |
en |
dc.identifier.issn |
01671987 |
en |
dc.identifier.uri |
http://dx.doi.org/10.1016/S0933-3630(97)00008-1 |
en |
dc.identifier.uri |
http://62.217.125.90/xmlui/handle/123456789/1377 |
|
dc.subject |
Soil heat flow |
en |
dc.subject |
Soil thermal properties |
en |
dc.subject.other |
heat flux |
en |
dc.subject.other |
soil profile |
en |
dc.title |
A contribution to the study of the water and energy balances of an irrigated soil profile A. Heat flux estimates |
en |
heal.type |
journalArticle |
en |
heal.identifier.primary |
10.1016/S0933-3630(97)00008-1 |
en |
heal.publicationDate |
1998 |
en |
heal.abstract |
In this paper, an attempt is made to estimate heat flux densities according to various methods for a wet and a dry soil profile. Primary data are soil temperature measurements in various depths (2, 5, 10, 20, 50 cm). Data concerning the soft texture and composition as well as data referring to the sod moisture profile for the selected days of this study are also available. Estimates of heat flux densities obtained through the various methods used are compared with actual heat flux densities, as these are measured at the depths of 2 and 10 cm into the soil profile. The comparison has been encouraging and therefore heat flux densities calculation methods may be used for following heat flow into the soft profile. |
en |
heal.journalName |
Soil and Tillage Research |
en |
dc.identifier.issue |
1-2 |
en |
dc.identifier.volume |
45 |
en |
dc.identifier.doi |
10.1016/S0933-3630(97)00008-1 |
en |
dc.identifier.spage |
189 |
en |
dc.identifier.epage |
198 |
en |