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פותח על ידי קלירמאש פתרונות בע"מ -
Limnology of dual purpose reservoirs in the coastal area and Jordan valley of Israel
Year:
1994
Authors :
מילשטיין, אנה
;
.
צורן, מירון
;
.
Volume :
46
Co-Authors:
Zoran, M.
Milstein, A.
Krambeck, H.J.
Zoran, M., Fish Cult.Res.Stn, Dor, Israel
Milstein, A., Fish Cult.Res.Stn, Dor, Israel
Krambeck, H.J., Fish Cult.Res.Stn, Dor, Israel
Facilitators :
From page:
64
To page:
75
(
Total pages:
12
)
Abstract:
Shallow reservoirs (about 3-4 m deep) developed a daily pattern of thermal and oxygen stratification with full nocturnal mixing. Deep reservoirs (5-8 m deep) developed, in addition to the daily pattern at the upper layers (2-3 m), a seasonal stratification. This led to the formation of an anoxic hypolimnion which lasted until midseason when the water level decreased to about 5 m due to irrigation. The daily wind (west sea breeze) induced movement of the upper oxygenated layer eastward. This layer downwelled in the east of the reservoir and the subsurface layer upwelled in the west, leading to a horizontal oxygen gradient in which the dissolved oxygen concentration in the east was higher and reached a greater depth than in the west. Differences in weather between the geographic locations led to stronger stratification in the Jordan Valley. -from Authors
Note:
Related Files :
anoxic hypolimnion
dissovled oxygen
Israel
Israel, Jordan Valley
reservoir limnology
Stratification
water temperature
עוד תגיות
תוכן קשור
More details
DOI :
Article number:
0
Affiliations:
Database:
סקופוס
Publication Type:
מאמר
;
.
Language:
אנגלית
Editors' remarks:
ID:
28145
Last updated date:
02/03/2022 17:27
Creation date:
17/04/2018 00:37
You may also be interested in
Scientific Publication
Limnology of dual purpose reservoirs in the coastal area and Jordan valley of Israel
46
Zoran, M.
Milstein, A.
Krambeck, H.J.
Zoran, M., Fish Cult.Res.Stn, Dor, Israel
Milstein, A., Fish Cult.Res.Stn, Dor, Israel
Krambeck, H.J., Fish Cult.Res.Stn, Dor, Israel
Limnology of dual purpose reservoirs in the coastal area and Jordan valley of Israel
Shallow reservoirs (about 3-4 m deep) developed a daily pattern of thermal and oxygen stratification with full nocturnal mixing. Deep reservoirs (5-8 m deep) developed, in addition to the daily pattern at the upper layers (2-3 m), a seasonal stratification. This led to the formation of an anoxic hypolimnion which lasted until midseason when the water level decreased to about 5 m due to irrigation. The daily wind (west sea breeze) induced movement of the upper oxygenated layer eastward. This layer downwelled in the east of the reservoir and the subsurface layer upwelled in the west, leading to a horizontal oxygen gradient in which the dissolved oxygen concentration in the east was higher and reached a greater depth than in the west. Differences in weather between the geographic locations led to stronger stratification in the Jordan Valley. -from Authors
Scientific Publication
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