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Arsenic in Arizona Ground Water -- Source and Transport CharacteristicsUhlman, Kristine 05 1900 (has links)
4 pp. / Following on the U.S. Environmental Protection Agency's "Arsenic Rule" decision to require public water systems to lower the allowable arsenic content in drinking water from 50 parts per billion (ppb) to 10 ppb by January 23, 2006, private well owners across the state have realized the importance of testing their own water supply for arsenic. Under Arizona law, it is the sole responsibility of the private well owner to determine the quality (potability) of their private well water. This article discusses the geologic prevelance of arsenic across the state, and options available to the well owner to address this water quality concern.
Expected to be the first in a 3-part series on ground water quality issues common in Arizona.
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Comparison of water quality between sources and between selected villages in the Waterberg District of Limpopo Province; South Africa: with special reference to chemical and microbial quality.Makgoka, Seretloane Japhtaline January 2005 (has links)
Thesis (MPH)--University of Limpopo, 2005 / Water and sanitation inadequacy is still an environmental health challenge in several
regions worldwide and a billion people lack access to safe water, while 2.4 billion people
have inadequate sanitation [2].
Assessment of water quality by its chemistry includes measures of elements and
molecules dissolved or suspended in water. Commonly measured chemical parameters
include arsenic, cadmium, calcium, chloride, fluoride, total hardness, nitrate, and
potassium [16]. Water quality can also be assessed by the presence of waterborne
microorganisms from human and animals’ faecal wastes. These wastes contain a wide
range of bacteria, viruses and protozoa that may be washed into drinking water supplies
[21].
Three villages were selected for water quality analysis, based on their critical situation
regarding access to water and sanitation: namely, Matlou, Sekuruwe and Taolome
villages, situated in the Mogalakwena Local Municipality within the Waterberg district of
the Limpopo Province, South Africa. A proposal was written to the Province of North
Holland (PNH) and was approved for funding to start with the implementation of those
projects, with 20% of each village’s budget allocated for water quality research [26].
This was a cross sectional, analytical study to investigate the chemical and microbial
quality of water in Matlou, Sekuruwe and Taolome villages. The study was also
conducted to explore methods used by household members to store and handle water in
storage tanks. Water samples were collected and analysed according to the standard
operating procedures (SOPs) of the Polokwane Municipality Wastewater Purification
Plant in Ladanna, Polokwane City of South Africa. The questionnaire used was adopted
from the one used for cholera outbreak in the Eastern Cape Province of South Africa.
Results show that water from all sources in all the villages had increased total hardness
concentration. Water from the borehole in Matlou village had increased number of total
coliform bacteria. There were increased total and faecal coliform bacteria in storage
tanks samples from Matlou village. Water samples from reservoirs in Sekuruwe and
Taolome villages did not test positive for any microbial contamination. Water from
xiv
informally connected yard taps in Sekuruwe village had increased total coliform bacteria,
while increased total and faecal coliforms were found in households’ storage tanks.
Water samples from communal taps in Taolome village had minimal number of total
coliform bacteria, while water from storage tanks had both increased total and faecal
coliform bacteria.
Matlou village was the only place with increased nitrate concentration at the households’
storage tanks. While all the villages had microbial contamination, Taolome village had
the least number of coliform bacteria in water samples from households’ storage tanks
as compared to Matlou and Sekuruwe villages.
It is concluded that water from sources supplied by the municipalities are safe to be
consumed by humans while water from informally connected taps and households’
storage tanks are not safe to be used without treatment.
It is recommended that a health and hygiene education package be prepared for all the
villages, so that handling of water from the main source into their storage tanks can be
improved. Secondly, it is recommended that water in all sources be treated for total
hardness and water in storage tanks in Matlou village be treated for nitrate. Thirdly, it is
recommended that water be accessed everyday of the week, so that people do not use
unsafe water supplies. / The Province of North Holland, Netherlands.
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Analysis of Groundwater Monitoring of Residential Wells In the Vicinity of Carbon Limestone Landfill, Poland Township, Mahoning County, OhioAlexander, Diana Marie January 2012 (has links)
No description available.
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Modeling Salinity Impact on Ground Water Irrigated Turmeric CropKizza, Teddy January 2013 (has links) (PDF)
Soils in irrigated fields are impacted by irrigation water quality. Salts in the irrigation water may accumulate in the soil depending on amount of leaching, the quality of water and type of ions present. Salinity is an environmental hazard that is known to limit agriculture worldwide. The quality of irrigation water is thus of concern to agriculturists. More so is the impact it has on productivity.
The objective of this study was to quantify the impact due to use of ground water of such quality, with respect to salinity, as found in Berambadi watershed of Southern India, under farmers‟ field conditions. Turmeric (Curcuma Longa L.) was used for the study, based on salt sensitivity, under furrow irrigation.
Study sites were selected basing on quality of water, with respect to salinity, crop and irrigation method. Samples of both soil and water were collected from each site and analyzed in the laboratory. The samples were analysed for salinity, alkalinity, pH and Cations of Magnesium, Sodium, Calcium and potassium as well as Chlorides and Sulfates. In addition soil was analysed for texture and Organic matter content.
Non destructive plant monitoring for Leaf area (Index), number of leaves and plant height was done up to 210 days from planting. Profile, up to 80 cm depth, soil moisture was monitored at six plots using TDR and surface, up to 6cm depth, soil moisture for all the plots using Theta probe.
Potential yield was obtained using STICS 6.9 crop model while field yield was estimated from rhizomes average weight of three plants. For both potential and observed yield estimation, a plant density of 9 plants per M2 was used.
The quality parameters in water were correlated to soil parameters and to crop growth and ultimate yield. Impact due to salinity was then identified and quantified using relative yield.
Identified quality problems in terms of turmeric response were, salinity, alkalinity and pH there was significant positive correlation between irrigation water salinity and soil salinity. Some wide scatter was observed and could be indicative of irrigation management practices, soil texture difference and other local variations.
Observed turmeric yield was significantly negatively correlated to soil salinity. There was a monotonically increasing gap between simulated and observed yield as salinity increased. The maximum observed yield was 71% of the potential.
The highest impact due to salinity was observed at 2.1 dS/m amounting to 44 % yield reduction.
Excessive chlorosis due to iron deficiency occurred at 24.5% as CaCO3 and pH 7.5. Irrigation water pH was normal as per the guidelines. Soil pH was not so varied; it ranged between 7.1-7.9 except for one site where it was 6. Within the 7.1-7.9 range there was no effect on crop and yield observed.
Interaction of stress factors observed was between salinity and alkalinity. The other was rhizome rot disease.
Loss of yield to salinity was significant but farmers have no specific plans to leach out salts nor do they have an idea that ground water quality can actually negatively impact productivity.
Salinity in irrigation water was in the moderately saline range. While that in the soil was low to slightly saline but could increase given the management practices.
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