東華大學圖書館 |

Language: English

Help

回圖書館首頁

手機版館藏查詢

Back

Switch To: Labeled | MARC Mode | ISBD

Groundwater and surface water intera...

Mitchell, Katie.

Linked to FindBook

Google Book

Amazon

博客來

Groundwater and surface water interactions at Georgetown Lake, Montana with emphasis on quantification of groundwater contribution.

Record Type:	Electronic resources : Monograph/item
Title/Author:	Groundwater and surface water interactions at Georgetown Lake, Montana with emphasis on quantification of groundwater contribution./
Author:	Mitchell, Katie.
Description:	79 p.
Notes:	Source: Masters Abstracts International, Volume: 53-01.
Contained By:	Masters Abstracts International53-01(E).
Subject:	Hydrologic sciences. -
Online resource:	http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=1556697
ISBN:	9781303924286

Groundwater and surface water interactions at Georgetown Lake, Montana with emphasis on quantification of groundwater contribution.
Mitchell, Katie.

Groundwater and surface water interactions at Georgetown Lake, Montana with emphasis on quantification of groundwater contribution. - 79 p.

Source: Masters Abstracts International, Volume: 53-01.

Thesis (M.S.)--Montana Tech of The University of Montana, 2014.

This item must not be sold to any third party vendors.

Georgetown Lake is a shallow intermontane lake located in southwestern Montana. Georgetown Lake is one of the lakes most used for recreation in the state and therefore research has been and continues to be conducted to ensure its continued quality and quantity. Knowing the contributions of the primary hydrologic parameters of a lake is vital to a lake quality-quantity analysis. Delineation of all of the hydrologic parameters can be difficult in intermontane settings. It is especially difficult to delineate groundwater flux, as groundwater is often subjected to complex flow paths due to irregular topography, and geologic folding and faulting. To account for these complexities, this study attempts to quantify groundwater contributions to the lake using an isotope mass balance. The hydrogeologic parameters of the equation were either sampled and measured or calculated for each month for a one year period and incorporated into an isotope mass balance equation. Utilization of these parameters and the corresponding isotopic compositions in the isotopic mass balance equation resulted in a groundwater inflow quantification of approximately 180 cm/yr, making groundwater flux into the lake approximately 55% of the total inflow to the lake.

ISBN: 9781303924286Subjects--Topical Terms:

3168407
Hydrologic sciences.

Groundwater and surface water interactions at Georgetown Lake, Montana with emphasis on quantification of groundwater contribution.
LDR:02949nmm a2200301 4500 001 2060680
005 20150924074354.5
008 170521s2014 ||||||||||||||||| ||eng d
020 $a 9781303924286
035 $a (MiAaPQ)AAI1556697
035 $a AAI1556697
040 $a MiAaPQ $c MiAaPQ
100 1 $a Mitchell, Katie. $3 3174856
245 1 0 $a Groundwater and surface water interactions at Georgetown Lake, Montana with emphasis on quantification of groundwater contribution.
300 $a 79 p.
500 $a Source: Masters Abstracts International, Volume: 53-01.
500 $a Adviser: Glenn Shaw.
502 $a Thesis (M.S.)--Montana Tech of The University of Montana, 2014.
506 $a This item must not be sold to any third party vendors.
520 $a Georgetown Lake is a shallow intermontane lake located in southwestern Montana. Georgetown Lake is one of the lakes most used for recreation in the state and therefore research has been and continues to be conducted to ensure its continued quality and quantity. Knowing the contributions of the primary hydrologic parameters of a lake is vital to a lake quality-quantity analysis. Delineation of all of the hydrologic parameters can be difficult in intermontane settings. It is especially difficult to delineate groundwater flux, as groundwater is often subjected to complex flow paths due to irregular topography, and geologic folding and faulting. To account for these complexities, this study attempts to quantify groundwater contributions to the lake using an isotope mass balance. The hydrogeologic parameters of the equation were either sampled and measured or calculated for each month for a one year period and incorporated into an isotope mass balance equation. Utilization of these parameters and the corresponding isotopic compositions in the isotopic mass balance equation resulted in a groundwater inflow quantification of approximately 180 cm/yr, making groundwater flux into the lake approximately 55% of the total inflow to the lake.
520 $a This study also presents data and interpretations that give further insight to the groundwater and surface water interactions at the Georgetown Lake study site. First, to further understand groundwater movement in the area, surrounding springs, streams and domestic wells were sampled for stable isotopes in an attempt to determine their connectivity to the lake. Second, this study built upon previous radon research conducted at the lake by attempting to delineate the lateral extent of which groundwater enters the eastern flank of the lake. Third, this study looked at the stratigraphic profiles of the lake water columns during ice cover to observe the field parameter trends as depth increases.
590 $a School code: 1550.
650 4 $a Hydrologic sciences. $3 3168407
650 4 $a Water resources management. $3 794747
690 $a 0388
690 $a 0595
710 2 $a Montana Tech of The University of Montana. $b Geosciences-Hydrogeology Option. $3 3174857
773 0 $t Masters Abstracts International $g 53-01(E).
790 $a 1550
791 $a M.S.
792 $a 2014
793 $a English
856 4 0 $u http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=1556697