Persian
Home | News | Articles | Gallery | FAQ | Contact us | Sitemap | About us
Menu
Geology
Exploration
Geomatics
Chemistry lab
Geology Museum
geological maps
Main Projects
Finance & Official
Publication and Library
Articles
Thesises Index
Environment
Innovation and dehiscence year
uses of Geology
Geotourism
Quarterly Journal Geosciences Index
Geology of Khorassan
mines of Khorasan
book introduction
About us
services and products
Knowledges of Geology
The Eastern sun
Famous geoscientist of Iran
seminars
mashad
Geology and mine laws
Park Museum
Hot Links
Khorassan Geotourism
Khorassan's warm springs
GSINET project
Subsidence in Mashhad plate
Geology Museum
Home » Articles

Articles

Writers : Jafari,Ali;Hafezi,Naser;Kazemi,Gholam Abbas
Refference : 11th Symposium Of Geological Society Of Iran - Mashhad, Ferdowsi University
Publishing Year : 1386

Abstract :

Increase in population and the need for extra water supply from aquifers causes water level decline around cities, leak of consumed water into sewage, leak of consumed water into aquifers, and finally water level rise under cities. Rise in water levels in urban centers leads to groundwater contamination, reduction in ground strength, problems for underground structures like subway train and liquefaction risk. Water level decline results in land subsidence. Presently, Mashad domestic water is supplied by Torogh and Kardeh dams in the west of the city with an annual rate of 180 Mm3. A large part of this water is discharged into the disposal wells which seeps into groundwater and causes both water level rise and pollution.


Subject List : Quantity of Groundwater

E-mail : info [at] gsinet [dot] ir
Last Update: 2010/09/26
Copyright © 2002-2007 GSINET , All rights reserverd.
P.B. : 91735-1166
18 Str. Sarafrazan Blv. Hour Sq., Mashhad - Iran
Tel: + 98 511 8218146-8 / Fax; +98 511 821 6044