Hydrogeologic Framework of the Willamette Lowland Aquifer System, Oregon and Washington Volume 1424, PT. 2

Author:   D G Woodward
Publisher:   Rarebooksclub.com
ISBN:  

9781232160588


Pages:   42
Publication Date:   13 May 2012
Format:   Paperback
Availability:   Not yet available   Availability explained
This item is yet to be released. You can pre-order this item and we will dispatch it to you upon its release.

Our Price $37.33 Quantity:  
Add to Cart

Share |

Hydrogeologic Framework of the Willamette Lowland Aquifer System, Oregon and Washington Volume 1424, PT. 2


Add your own review!

Overview

This historic book may have numerous typos and missing text. Purchasers can download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1998-12 Excerpt: ...the Cooper Mountain-Bull Mountain area was declared a critical ground-water area by the Oregon State Engineer in 1974, and restrictions were placed on both pumping and the construction of new wells. Additionally, in 1974, when the Wolf Creek Irrigation Project began supplying water for irrigation from the Tualatin River, the use of ground water for irrigation further decreased. As a result, water levels in the basalt aquifer in that area began to rise. However, hydrographs from the remaining wells shown on figure 18d indicate a progressive, long-term water-level decline. FIGURE 18a.--Water levels in wells completed in the hydrogeologic units in the Portland Basin and in the Tualatin Basin. Graph number (1-16) is also well number on figure 17. FIGURE 18b.--Water levels in wells completed in the Willamette aquifer, central Willamette Valley. Graph number (1-16) is also well number on figure 17. FIGURE 18c.--Water levels in wells completed in the Willamette aquifer, southern Willamette Valley. Graph number (1-16) is also well number on figure 17. FLOW WITHIN AQUIFERS During the winter and spring, when the regional water table is highest, some wells completed in the Willamette aquifer begin to flow (water levels rise above land surface); these wells usually cease to flow during the summer. In order to eliminate this variation in ground-water flow patterns caused by precipitation variability, water-level measurements collected during the summer and fall, when the water table is lowest, were used to map the water table (pl. 1). The water table mapped in plate 1 coincides with the potentiometric surface of the Willamette aquifer, except in the Tualatin Basin, where it coincides with the potentiometric surface of the Willamette confining unit, and in certain are...

Full Product Details

Author:   D G Woodward
Publisher:   Rarebooksclub.com
Imprint:   Rarebooksclub.com
Dimensions:   Width: 18.90cm , Height: 0.20cm , Length: 24.60cm
Weight:   0.095kg
ISBN:  

9781232160588


ISBN 10:   123216058
Pages:   42
Publication Date:   13 May 2012
Format:   Paperback
Publisher's Status:   Active
Availability:   Not yet available   Availability explained
This item is yet to be released. You can pre-order this item and we will dispatch it to you upon its release.

Table of Contents

Reviews

Author Information

Tab Content 6

Author Website:  

Customer Reviews

Recent Reviews

No review item found!

Add your own review!

Countries Available

All regions
Latest Reading Guide

Aorrng

Shopping Cart
Your cart is empty
Shopping cart
Mailing List