Cleanup of Polluted Ground Water - A Solution in Search of the Right Problem

1989 ◽  
Vol 9 (1) ◽  
pp. 5-10
Author(s):  
Arnold Schiffman
2004 ◽  
Vol 4 (3) ◽  
pp. 467-471 ◽  
Author(s):  
A. Bhaumik ◽  
S. Samanta ◽  
N.K. Mal

2019 ◽  
Vol 270 ◽  
pp. 04007
Author(s):  
Susilawati Cicilia Laurentia ◽  
Yulius PK Suni ◽  
Alfred Fredrich Lukas

The problems related to hydro-environmental engineering on small islands are flood and drought, for the less favourable rainfall characteristics. Big rainfall intensity comes and flows immediately as storm runoff to the sea because of short distance, and no chance to infiltrate into the soil as ground-water recharge. Floods and landslides occur during rainy season and drought during the dry season. This research investigates the role of rainwater management in order to overcome these problems. The literature review and field observations of experiences on rainwater management techniques applied on both communal scale and household level. The results show that firstly, rainwater must be managed in ways that small amount of rainwater flows out immediately to the sea. So, it has the chance to infiltrate into the soil as ground-water recharge. This is done by making some water-traps series, harvesting rainwater and storing it into the ponds at the household scale. The water then could be utilized for domestic and agriculture purposes. Secondly, learning from several experiences’ technology implementation as water conservation, it can be found the right way to manage rainwater at communal/household scale. These actions give the rainwater management having contributions to solve problems related to hydro-environments engineering.


2019 ◽  
Vol 5 (1) ◽  
pp. 9-16
Author(s):  
Ninik Fadhillah ◽  
Muh. Ma’arif ◽  
Hanik Faizah ◽  
Latifatoel Chilmi

UIN Sunan Ampel requirements of water are fulfilled from groundwater sources. The groundwater sources of UIN Sunan Ampel are from wells where the water is taken with a water pump. The main problem related to the use of groundwater as a fulfillment of water needs is the decline of its quality. The purpose of this study is to analyze the quality of groundwater at UIN Sunan Ampel, to know the quality of groundwater in UIN Sunan Ampel reviewed by Minister of Health Regulation No. RI. 32 of 2017, Formulating the right steps in improving the quality of ground water at Sunan Ampel UIN towards ECO CAMPUS. This research is a descriptive study, in this study the quality of groundwater sources in Sunan Ampel Surabaya UIN will be described base on 3 parameters of water quality (physics, chemistry and biology). The results indicate differences in groundwater quality at UIN Sunan Ampel in terms of physical, chemical and biological parameters. The quality of groundwater sources in UIN Sunan Ampel Surabaya 95% fulfills the standard of environmental health standards and water health requirements for government sanitation hygiene requirements based on physics parameters, but it do not fulfilled the quality standards based on chemical parameters (in the form of pH) and also biology parameters. Improving the quality of ground water at UIN Sunan Ampel Surabaya is needed by improving the management system of sewers and latrines as well as standard construction of wells.


1998 ◽  
Vol 3 (1) ◽  
Author(s):  
Lutz Prager ◽  
Reiner Mehnert ◽  
Axel Sobottka ◽  
Helmut Langguth ◽  
Werner Baumann ◽  
...  

AbstractPilot-plant studies with strip-gas from a ground water remediation site at Dusseldorf, Germany (gas throughput 1000 m


2001 ◽  
Vol 16 (9-10) ◽  
pp. 1129-1137 ◽  
Author(s):  
Erik G Søgaard ◽  
Remigijus Aruna ◽  
Joanna Abraham-Peskir ◽  
Christian Bender Koch

1945 ◽  
Vol S5-XV (7-8) ◽  
pp. 563-585
Author(s):  
Henri Schoeller

Abstract Although the geologic structure of both banks of the Saoura river, Algeria, is essentially the same, no ground-water aquifers occur on the right bank due to the absence of covering sands such as are present on the left bank where an extensive aquifer occurs in Pliocene limestones overlain by dunes and sands of the western Grand Erg. Formation of the aquifer is due to accumulation of rain waters which have percolated through the desert sands and not to infiltration of waters from intermittent streams descending the slopes of the Atlas mountains.


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