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

Surface-water and groundwater intera...

Killian, Courtney.

Linked to FindBook

Google Book

Amazon

博客來

Surface-water and groundwater interactions of a stream reach and proposed reservoir within the Pascagoula River Basin: George County, Mississippi.

Record Type:	Electronic resources : Monograph/item
Title/Author:	Surface-water and groundwater interactions of a stream reach and proposed reservoir within the Pascagoula River Basin: George County, Mississippi./
Author:	Killian, Courtney.
Published:	Ann Arbor : ProQuest Dissertations & Theses, : 2015,
Description:	157 p.
Notes:	Source: Masters Abstracts International, Volume: 54-04.
Contained By:	Masters Abstracts International54-04(E).
Subject:	Hydrologic sciences. -
Online resource:	http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=1586976
ISBN:	9781321697865

Surface-water and groundwater interactions of a stream reach and proposed reservoir within the Pascagoula River Basin: George County, Mississippi.
Killian, Courtney.

Surface-water and groundwater interactions of a stream reach and proposed reservoir within the Pascagoula River Basin: George County, Mississippi. - Ann Arbor : ProQuest Dissertations & Theses, 2015 - 157 p.

Source: Masters Abstracts International, Volume: 54-04.

Thesis (M.S.)--Mississippi State University, 2015.

This item is not available from ProQuest Dissertations & Theses.

This research had two main objectives: quantify surface-water and groundwater interactions along a stream reach, and determine the hydraulic conductivity at the site where two reservoirs are proposed. The objectives of this research aim to help maintain stream ecology and increase surface water storage for recreational and industrial purposes. The stream reach, located in the Pascagoula River Basin of southeast Mississippi, begins at Lake Okatibbee and terminates at Pascagoula into the Gulf of Mexico. Four USGS continuous gauging stations provided more than forty years of stream discharge data for a hydrograph base-flow-recession analysis, which determined the baseflow component within the stream. The analysis showed that baseflow decreases along the stream reach and increases again before reaching the Gulf of Mexico. Thirteen borehole samples were collected at the sites of the proposed reservoirs in George County, Mississippi to determine the hydraulic conductivity of the sediments, which showed high a hydraulic conductivity.

ISBN: 9781321697865Subjects--Topical Terms:

3168407
Hydrologic sciences.

Surface-water and groundwater interactions of a stream reach and proposed reservoir within the Pascagoula River Basin: George County, Mississippi.
LDR:02101nmm a2200313 4500 001 2121020
005 20170724102938.5
008 180830s2015 ||||||||||||||||| ||eng d
020 $a 9781321697865
035 $a (MiAaPQ)AAI1586976
035 $a AAI1586976
040 $a MiAaPQ $c MiAaPQ
100 1 $a Killian, Courtney. $3 3283007
245 1 0 $a Surface-water and groundwater interactions of a stream reach and proposed reservoir within the Pascagoula River Basin: George County, Mississippi.
260 1 $a Ann Arbor : $b ProQuest Dissertations & Theses, $c 2015
300 $a 157 p.
500 $a Source: Masters Abstracts International, Volume: 54-04.
500 $a Adviser: Darrel W. Schmitz.
502 $a Thesis (M.S.)--Mississippi State University, 2015.
506 $a This item is not available from ProQuest Dissertations & Theses.
520 $a This research had two main objectives: quantify surface-water and groundwater interactions along a stream reach, and determine the hydraulic conductivity at the site where two reservoirs are proposed. The objectives of this research aim to help maintain stream ecology and increase surface water storage for recreational and industrial purposes. The stream reach, located in the Pascagoula River Basin of southeast Mississippi, begins at Lake Okatibbee and terminates at Pascagoula into the Gulf of Mexico. Four USGS continuous gauging stations provided more than forty years of stream discharge data for a hydrograph base-flow-recession analysis, which determined the baseflow component within the stream. The analysis showed that baseflow decreases along the stream reach and increases again before reaching the Gulf of Mexico. Thirteen borehole samples were collected at the sites of the proposed reservoirs in George County, Mississippi to determine the hydraulic conductivity of the sediments, which showed high a hydraulic conductivity.
590 $a School code: 0132.
650 4 $a Hydrologic sciences. $3 3168407
650 4 $a Geology. $3 516570
650 4 $a Environmental geology. $3 535218
690 $a 0388
690 $a 0372
690 $a 0407
710 2 $a Mississippi State University. $b Geosciences. $3 1018556
773 0 $t Masters Abstracts International $g 54-04(E).
790 $a 0132
791 $a M.S.
792 $a 2015
793 $a English
856 4 0 $u http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=1586976