scholarly journals Estimates of natural ground-water discharge and characterization of water quality in Dry Valley, Washoe County, West-Central Nevada, 2002-2003

2004 ◽  
Author(s):  
David L. Berger ◽  
Douglas K. Maurer ◽  
Thomas J. Lopes ◽  
Keith J. Halford
Keyword(s):  
Water Quality ◽  
Ground Water ◽  
Water Discharge ◽  
West Central ◽  
Dry Valley ◽  
Washoe County

Effectiveness of riparian buffers in controlling ground-water discharge of nitrate to streams in selected hydrogeologic settings of the North Carolina Coastal Plain

2004 ◽  
Vol 49 (3) ◽  
pp. 63-70 ◽  
Author(s):  
T.B. Spruill
Keyword(s):  
Water Quality ◽  
North Carolina ◽  
Ground Water ◽  
Coastal Plain ◽  
Water Discharge ◽  
Relative Effectiveness ◽  
Surface Water Quality ◽  
Riparian Buffers ◽  
Flow Paths ◽  
The North

Water-quality and hydrologic information were collected along ground-water flow paths from two well-drained and two poorly drained Coastal Plain settings in North Carolina to evaluate the relative effectiveness of riparian buffers in reducing discharge of nitrate to streams. At one well-drained site with a 100 m buffer, little or no effect was detected on surface-water quality by discharging ground water because extensive woody vegetation in the buffer was able to take up not only most nitrate, but also most ground water before discharging to the stream during the growing season (March-October). At the second well-drained site, ground water discharging to the stream from the side with a buffer contained about 2 mg/L of nitrate-nitrogen after passing through the bed of the stream compared to 6 mg/L in ground water discharging from the side with no buffer. In the poorly drained settings, nitrate in ground water decreased from about 6 mg/L in the recharge area to less than 0.02 mg/L downgradient from the riparian buffer. Ground water discharging from the side with no buffer contained 0.83 mg/L. Riparian buffers appear effective in reducing nitrate in ground water discharging to Coastal Plain streams.

scholarly journals Characterization of Chyulu Hills Watershed Ecosystem Services in South-Eastern Kenya

2016 ◽  
Vol 6 (3) ◽  
pp. 65
Author(s):  
John Warui Kiringe ◽  
Francis Mwaura ◽  
Fiesta Warinwa
Keyword(s):  
Ground Water ◽  
Water Discharge ◽  
Water Source ◽  
Water Volume ◽  
Dry Land ◽  
Shallow Wells ◽  
Water Provision ◽  
Annual Water ◽  
Annual Water Discharge

<p class="1Body">Water is an important good provided by watersheds and is critical in sustaining life and socio-economic development. This study evaluated water provision in the Chyulu Hills watershed which is one of the important dry land water catchments in Kenya. Surface water discharge was mainly through rivers and springs with the latter being more prevalent than the former while ground water provision was primarily through boreholes and shallow wells. Springs discharged the highest water volume annually estimated at 128.14million m<sup>3</sup> or 85.14% of all the water discharged in the watershed, with shallow wells and boreholes discharging the least water. For all the springs found in the watershed, Mzima springs discharged the highest water volume estimated at nearly 113.15 million m<sup>3</sup> annually or 88.30% of the water produced by all the springs; and about 75.19% of the water in the entire watershed. Rivers which were active had a total water discharge of about 20.66million m<sup>3</sup> per year, with Kibwezi River discharging 17.59 million m<sup>3</sup> annually or 85.14% of all the water from rivers. Shallow wells were mainly prevalent at Nthongoni and the Makindu, and their annual water discharge was about 16.96million m<sup>3</sup> per year with boreholes contributing 98.87% (approximately 16.76 million m<sup>3</sup>/yr.) of the ground water, and the rest (19,169.92m<sup>3</sup>/yr.) being contributed by shallow wells. The total amount of water discharged in the watershed by the combined water source types was about 150.49 million m3/yr.</p>

scholarly journals Impact of Hijlan Creek springs on water quality of the Euphrates River and the Hydrochemical characterization of the contamination plumes

2021 ◽  
Author(s):  
Muwafaq Ayesh Rabeea ◽  
Ahmed J. R. Al-Heety ◽  
Mahmmoud Ismail Mohammed ◽  
Adnan Mohammed Fayydh ◽  
Mohamed Elhag
Keyword(s):  
Water Quality ◽  
Water Discharge ◽  
Chloride Content ◽  
Physicochemical Characteristics ◽  
Euphrates River ◽  
Before And After ◽  
Mixing Rates ◽  
Load Discharge

Abstract This work aims to present the hydrochemical mechanisms describing the system of the Euphrates River before and after mixing with groundwater from the springs of Hijlan (western Iraq). Continuously, the data generated from these springs' water have been adapted to provide an updated assessment for future water therapeutic purposes. Physicochemical characteristics of water in the mixing plume of Hijlan Creek and the Euphrates indicate the multi Hydrochemical plumes as revealed by the spatial variation of important parameters related to the ecological parameters including K+, Na+, Ca+ 2, Mg+ 2, HCO3−, SO4 − 2, Cl−, NO3−, PO4 − 3, Pb, Zn, Cd, Fe, Mn, Temp, DO, BOD5, H2S, Turbidity, EC, pH, and TDS. The re-aeration (k2) and de-oxygenation rate (k1) coefficients, as well as the self-purification factor (f) of the mixing plume, are 0.51 sec− 1, 2.03 sec− 1, and 0.25, respectively. The Cl− concentration in the confluence zone changes, due to the chloride content mixing rates of 7.1% and 92.9% for Euphrates and Hijlan creek water, respectively, with water discharge of 316,224 m3/day and chloride load discharge of 420 tons/day. The assessment of the water quality indicates unsuitability for aquaculture purposes. However, the water can be used for therapeutic purposes and to cure multiple diseases.

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