Predication of Groundwater Level Changes in the Plain of Hamedan-Bahar Using Time Series Model

Aquifer in alluvium of this plain is 520 km2. The aquifer is recharged from direct infiltration of precipitation and surface runoff, return flow from agricultural, industrial and domestic uses and groundwater input and discharged through water abstraction for different consumptions and groundwater o...

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Bibliographic Details
Main Authors: Ali Reza Rahmani, Mortaza Sedehi
Format: Article
Language:English
Published: Water and Wastewater Consulting Engineers Research Development 2005-11-01
Series:آب و فاضلاب
Online Access:http://www.wwjournal.ir/article_2510_dd2cd60a8490fefdcceacca5ad8d4246.pdf