dc.contributor.author |
Elmaloglou, S |
en |
dc.contributor.author |
Diamantopoulos, E |
en |
dc.date.accessioned |
2014-06-06T06:49:21Z |
|
dc.date.available |
2014-06-06T06:49:21Z |
|
dc.date.issued |
2009 |
en |
dc.identifier.issn |
03783774 |
en |
dc.identifier.uri |
http://dx.doi.org/10.1016/j.agwat.2008.09.003 |
en |
dc.identifier.uri |
http://62.217.125.90/xmlui/handle/123456789/4547 |
|
dc.subject |
Deep percolation |
en |
dc.subject |
Evaporation |
en |
dc.subject |
Hysteresis |
en |
dc.subject |
Mathematical modelling |
en |
dc.subject |
Total simulation time |
en |
dc.subject |
Trickle irrigation duration |
en |
dc.subject.other |
Elasticity |
en |
dc.subject.other |
Evaporation |
en |
dc.subject.other |
Extraction |
en |
dc.subject.other |
Geologic models |
en |
dc.subject.other |
Groundwater |
en |
dc.subject.other |
Hysteresis |
en |
dc.subject.other |
Mathematical models |
en |
dc.subject.other |
Moisture |
en |
dc.subject.other |
Moisture determination |
en |
dc.subject.other |
Percolation (fluids) |
en |
dc.subject.other |
Permittivity |
en |
dc.subject.other |
Reservoirs (water) |
en |
dc.subject.other |
Silt |
en |
dc.subject.other |
Soil moisture |
en |
dc.subject.other |
Soils |
en |
dc.subject.other |
Solvent extraction |
en |
dc.subject.other |
Solvents |
en |
dc.subject.other |
Underwater soils |
en |
dc.subject.other |
Vapors |
en |
dc.subject.other |
Water content |
en |
dc.subject.other |
Characteristic curves |
en |
dc.subject.other |
Deep percolation |
en |
dc.subject.other |
Discharge rates |
en |
dc.subject.other |
Drip irrigation |
en |
dc.subject.other |
Flow modelling |
en |
dc.subject.other |
Mathematical modelling |
en |
dc.subject.other |
Root zone |
en |
dc.subject.other |
Silt loams |
en |
dc.subject.other |
Soil surfaces |
en |
dc.subject.other |
Soil water retention |
en |
dc.subject.other |
Total simulation time |
en |
dc.subject.other |
Trickle irrigation duration |
en |
dc.subject.other |
Water extraction |
en |
dc.subject.other |
Water loss (WL) |
en |
dc.subject.other |
Irrigation |
en |
dc.subject.other |
discharge |
en |
dc.subject.other |
drip irrigation |
en |
dc.subject.other |
evaporation |
en |
dc.subject.other |
hysteresis |
en |
dc.subject.other |
infiltration |
en |
dc.subject.other |
numerical model |
en |
dc.subject.other |
percolation |
en |
dc.subject.other |
rhizosphere |
en |
dc.subject.other |
soil moisture |
en |
dc.subject.other |
soil water |
en |
dc.subject.other |
water content |
en |
dc.title |
Effects of hysteresis on redistribution of soil moisture and deep percolation at continuous and pulse drip irrigation |
en |
heal.type |
journalArticle |
en |
heal.identifier.primary |
10.1016/j.agwat.2008.09.003 |
en |
heal.publicationDate |
2009 |
en |
heal.abstract |
The infiltration and redistribution of soil moisture under surface drip irrigation considering hysteresis were investigated in two soils (loamy sand and silt loam) of different texture. The effect of continuous versus intermittent application of 1, 2 and 4 l/h to the soils was evaluated in terms of wetting front advance patterns and deep percolation under the root zone. For this purpose, a cylindrical flow model incorporating hysteresis in the soil water retention characteristic curve, evaporation from the soil surface, and water extraction by roots was used. The results show that, compared with continuous irrigation, pulse irrigation slightly reduces the water losses under the root zone in both cases (with and without hysteresis). Also, at the total simulation time, in both types of irrigation, hysteresis reduces significantly the water losses under the root zone. Finally, the effect of hysteresis was found to be greater at higher discharge rate (4 l/h) and consequently at higher water content at the soil surface. © 2008 Elsevier B.V. All rights reserved. |
en |
heal.journalName |
Agricultural Water Management |
en |
dc.identifier.issue |
3 |
en |
dc.identifier.volume |
96 |
en |
dc.identifier.doi |
10.1016/j.agwat.2008.09.003 |
en |
dc.identifier.spage |
533 |
en |
dc.identifier.epage |
538 |
en |