Local-scale variability in groundwater resources: Cedar Creek Watershed, Wisconsin, U.S.A.

2018 ◽  
Vol 20 ◽  
pp. 38-51 ◽  
Author(s):  
Weon Shik Han ◽  
J.P. Graham ◽  
S. Choung ◽  
Eungyu Park ◽  
Woonsup Choi ◽  
...  
2007 ◽  
Vol 36 (2) ◽  
pp. 521-531 ◽  
Author(s):  
M. Larose ◽  
G. C. Heathman ◽  
L. D. Norton ◽  
B. Engel

2014 ◽  
Vol 9 (No. 2) ◽  
pp. 66-76
Author(s):  
H.-Y. Lu

Arsenic contamination in groundwater is a common groundwater problem worldwide. To manage groundwater resources effectively, it is crucial to determine the arsenic source. Taiwan’s Tsengwen Creek watershed is one of the known areas for groundwater arsenic contamination. Water-rock interactions are evaluated on a regional scale. A conceptual hydrogeological framework is first established based on groundwater hydrochemistry. The local aquifer system can be categorized into high-arsenic deep aquifer and low-arsenic shallow aquifer. The average geochemistry of sediments indicates that arsenic and heavy metals are not significantly enriched in the deeper aquifer on the scale of the whole watershed. Therefore, arsenic contamination in the deeper groundwater of the Tsengwen Creek watershed is not simply source-controlled. However, the Fe-Mn oxides in sediments contain slightly more arsenic in the deep aquifer. The long residence time of groundwater could magnify the enrichment and cause natural arsenic contamination in the deep aquifer.


2021 ◽  
pp. 509-527
Author(s):  
Mohsen Sherif ◽  
Abdel Azim Ebraheem ◽  
Ampar Shetty ◽  
Ahmed Sefelnasr ◽  
Khaled Alghafli ◽  
...  

AbstractIn Ras Al Khaimah, UAE, groundwater from the alluvial aquifer in Wadi Bih was the only source of freshwater for various uses prior to the construction of a seawater desalination plant in 1998. This study was conducted to evaluate the effect of the Wadi Bih dam on groundwater resources and to increase knowledge of the hydrodynamics of the aquifer. A local-scale numerical groundwater flow model was developed and used to investigate the impacts of different groundwater management options on groundwater resources. The calibrated and validated model was defined as the base case, and subsequently, simulations were performed to analyze different management scenarios. The simulations indicated that maximum recharge occurred during years of high rainfall (1995–1998). Minimum recharge occurred in 2000, 2002, and 2004. The major contribution to the water balance was from subsurface inflows from the upper wadi zone and the two tributaries. Overall, the annual water balance was negative in most years, with an average net decline of 0.6 MCM per year, indicating a slow but continuous depletion of groundwater resources. At the end of the simulation, the total groundwater recharge due to rainfall and water storage in the ponding area was 9.81 MCM.


Water ◽  
2021 ◽  
Vol 13 (11) ◽  
pp. 1515
Author(s):  
Sadaf Teimoori ◽  
Brendan F. O’Leary ◽  
Carol J. Miller

Groundwater plays a significant role in the vitality of the Great Lakes Basin, supplying water for various sections. Due to the interconnection of groundwater and surface water features in this region, the groundwater quality can be affected, leading to potential economic, political, health, and social issues for the region. Groundwater resources have received less emphasis, perhaps due to an “out of sight, out of mind” mentality. The incomplete characterization of groundwater, especially shallow, near-surface waters in urban centers, is an added source of environmental vulnerability for the Great Lakes Basin. This paper provides an improved understanding of urban groundwater to reduce this vulnerability. Towards that end, two approaches for improved characterization of groundwater in southeast Michigan are employed in this project. In the first approach, we construct a regional groundwater model that encompasses four major watersheds to define the large-scale groundwater features. In the second approach, we adopt a local scale and develop a local urban water budget with subsequent groundwater simulation. The results show the groundwater movement in the two different scales, implying the effect of urban settings on the subsurface resources. Both the regional and local scale models can be used to evaluate and mitigate environmental risks in urban centers.


2009 ◽  
Author(s):  
Reema Padia ◽  
Israel David Parker ◽  
Bailey Sullivan ◽  
R Karthikeyan ◽  
Saqib Mukhtar

Author(s):  
Mark Meyer ◽  
Munsell McPhillips ◽  
Gary T. Moore
Keyword(s):  

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