SSSAJ
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


This Article
Right arrow Abstract Freely available
Right arrow Full Text Free
Right arrow Full Text (PDF) Free
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Similar articles in ISI Web of Science
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via ISI Web of Science (2)
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Lin, C.
Right arrow Articles by Banin, A.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Lin, C.
Right arrow Articles by Banin, A.
GeoRef
Right arrow GeoRef Citation
Agricola
Right arrow Articles by Lin, C.
Right arrow Articles by Banin, A.
Related Collections
Right arrow Water Management
Right arrow Hydraulic Conductivity
Right arrow Recharge
Right arrow Infiltration

Temperature dependence of infiltration rate during large scale water recharge into soils

Chunye Lin, Dan Greenwald and Amos Banin*

Dep. of Soil and Water Sci., The Hebrew Univ. of Jerusalem, P.O. Box 12, Rehovot 76100, Israel



View larger version (25K):

[in a new window]
 
Fig. 1. The layout of the infiltration basins in the Soreq site of the Dan wastewater treatment plant near Tel-Aviv, Israel. Infiltration rate was measured from December 1997 to December 1999 in Basin-field 103 (Subbasin 103-4/5, leveled at 40 m above sea level) and from March 2000 to March 2002 in Basin-field 102 (Subbasins 102-1 to 102-5, leveled at 45 m above sea level).

 


View larger version (18K):

[in a new window]
 
Fig. 2. Infiltration rate (IR) per cycle and average effluent temperature (T) per cycle measured in large scale recharge basins at the Shafdan wastewater treatment plant across a 4-yr period. Curves were obtained by smoothing (five-point moving average) of the measured data. Dashed lines indicate recharge regime change in Basin 102 on 1 July 2000 (see Table 1). F = fall, Sm = summer, Sp = spring; W = winter.

 


View larger version (15K):

[in a new window]
 
Fig. 3. Observation-based seasonal changes of measured relative infiltration rate (ORIR) and calculated viscosity-based relative infiltration rate (VRIR) in the Shafdan wastewater treatment plant. RIR = ORIR + VRIR; F = fall; Sm = summer; Sp = spring; W = winter.

 





HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
and Life Sciences Education
Vadose Zone Journal
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 2003 by the Soil Science Society of America.