Abstract: Hydrogeochemical maps for uranium, associated trace elements and hydrogeochemical parameters in the surface drainage systems of North Wales: environmental and economic implications

1991 ◽  
Vol 13 (3) ◽  
pp. 141-141
Author(s):  
P. R. Simpson ◽  
N. Breward ◽  
J. Cook ◽  
W. M. Edmunds ◽  
D. Flight ◽  
...  
1991 ◽  
Vol 13 (3) ◽  
pp. 142-142
Author(s):  
P. R. Simpson ◽  
W. M. Edmunds ◽  
N. Breward ◽  
D. Flight ◽  
P. Green ◽  
...  

2021 ◽  
Vol 13 (13) ◽  
pp. 7189
Author(s):  
Beniamino Russo ◽  
Manuel Gómez Valentín ◽  
Jackson Tellez-Álvarez

Urban drainage networks should be designed and operated preferably under open channel flow conditions without flux return, backwater, or overflows. In the case of extreme storm events, urban pluvial flooding is generated by the excess of surface runoff that could not be conveyed by pressurized sewer pipes, due to its limited capacity or, many times, due to the poor efficiency of surface drainage systems to collect uncontrolled overland flow. Generally, the hydraulic design of sewer systems is addressed more for underground networks, neglecting the surface drainage system, although inadequate inlet spacings and locations can cause dangerous flooding with relevant socio-economic impacts and the interruption of critical services and urban activities. Several experimental and numerical studies carried out at the Technical University of Catalonia (UPC) and other research institutions demonstrated that the hydraulic efficiency of inlets can be very low under critical conditions (e.g., high circulating overland flow on steep areas). In these cases, the hydraulic efficiency of conventional grated inlets and continuous transverse elements can be around 10–20%. Their hydraulic capacity, expressed in terms of discharge coefficients, shows the same criticism with values quite far from those that are usually used in several project practice phases. The grate clogging phenomenon and more intense storm events produced by climate change could further reduce the inlets’ performance. In this context, in order to improve the flood urban resilience of our cities, the relevance of the hydraulic behavior of surface drainage systems is clear.


2000 ◽  
Vol 19 (2) ◽  
pp. 95-100 ◽  
Author(s):  
S. D. Khepar ◽  
A. K. Yadav ◽  
S. K. Sondhi ◽  
Arpan Sherring

2021 ◽  
pp. 1-40
Author(s):  
Jasmine Humphrey ◽  
Chris Rowett ◽  
Jonathan Tyers ◽  
Mark Gregson ◽  
Sean Comber

Author(s):  
Gregory Carling ◽  
David Tingey ◽  
Diego Fernandez

Glaciers are a reservoir of mercury (Hg) and other trace elements that have accumulated in the ice during the industrial era. As glaciers continue to melt at an alarming rate, these potentially toxic metals are released to the environment. In order to evaluate the impact of glacier melt on water quality in high elevation catchments in Grand Teton National Park, we sampled transects along the Teton and Middle Teton glaciers and proglacial streams during early-July and mid-August 2013. The glaciers were snow-covered during July, and thus water samples were primarily melt of snowpack from the previous winter. The glacier ice was exposed during August, and thus samples likely represented true glacier melt. These contrasting sample sets allowed for a determination of the impact of snowmelt versus glacier melt on water chemistry. Ten samples were collected during July and August along the Glacier Gulch transect: four of surface drainage on the Middle Teton glacier, three near the terminal moraine, and three downstream of the glacier. Thirteen samples were collected during July and August along the Garnet Canyon transect: one at the Lower Saddle of the Grand Teton, four of surface drainage on the Middle Teton glacier, two near the terminal moraine, two at the moraine of Teepe Glacier, and four samples downstream of the glaciers. All water samples were analyzed for total Hg, a suite of trace elements (including U, Sr, and Mn), and stable water isotopes (δ2H and δ18O). Analyses for methyl Hg, solutes, and tritium (3H) are still underway. Preliminary results indicate that snowmelt and glacier melt was a significant source of total Hg, but additional work is needed to determine the extent of Hg methylation in the proglacial streams. Other trace elements were found in low concentrations in the melt water, but increased substantially downstream of the glaciers due to water-rock interactions.


Author(s):  
Berthelot Curtis ◽  
Roberto Soares ◽  
Diana Podborochynski ◽  
Rielle Haichert ◽  
Duane Guenther

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