Journal of Food, Agriculture and Environment




Vol 6, Issue 3&4,2008
Online ISSN: 1459-0263
Print ISSN: 1459-0255


Movement and flow velocity of groundwater in wells


Author(s):

Funda Dökmen 1*, Cengiz Kurtuluş 2

Recieved Date: 2008-06-22, Accepted Date: 2008-09-02

Abstract:

The movement and the flow velocity of groundwater were determined from data obtained from ten wells drilled in Derince district of Kocaeli, İzmit, Turkey. The data were determined on the basis of Darcy’s law. The depths and groundwater levels of the wells ranged from 16 to 115 m and from 3.90 to 25.10 m, and the maximum and the minimum discharge rates were determined to be 604.8 and 172.8 m3 day-1, respectively. The velocity of the groundwater varied between 21.6 and 75.6 m day-1. The filtration of the aquifer and the hydraulic slope affected the flow of the groundwater strongly. Pumping and the slope of the basement influenced strongly by the velocity of the groundwater.

Keywords:

Discharge rate, filtration, flow velocity, hydraulic slope, movement, stream, groundwater


Journal: Journal of Food, Agriculture and Environment
Year: 2008
Volume: 6
Issue: 3&4
Category: Environment
Pages: 470-472


Full text for Subscribers
Information:

Note to users

The requested document is freely available only to subscribers/registered users with an online subscription to the Journal of Food, Agriculture & Environment. If you have set up a personal subscription to this title please enter your user name and password. All abstracts are available for free.

Article purchasing

If you like to purchase this specific document such as article, review or this journal issue, contact us. Specify the title of the article or review, issue, number, volume and date of the publication. Software and compilation, Science & Technology, all rights reserved. Your use of this website details or service is governed by terms of use. Authors are invited to check from time to time news or information.


Purchase this Article:   20 Purchase PDF Order Reprints for 15

Share this article :