OCCURRENCE OF CRYPTOSPORIDIUM IN GROUNDWATER WELLS WITH AND WITHOUT SURFACE WATER INFLUENCE

2018 ◽  
Author(s):  
Joel P. Stokdyk ◽  
◽  
Susan K. Spencer ◽  
Susan K. Spencer ◽  
Anita C. Anderson ◽  
...  
2006 ◽  
Vol 6 (1) ◽  
pp. 39-48 ◽  
Author(s):  
S. Mutl ◽  
P. Polasek ◽  
M. Pivokonsky ◽  
O. Kloucek

This paper summarises the preliminary results from the research into the influence that conditions of agitation have on the progression of the aggregation process and on some of the properties of formed aggregates affecting the efficiency of separation processes. These results show that the applied velocity gradient G, the period of its action T and the distribution of a velocity field in the agitated volume of water influence the number of aggregates, their size and shape in a significant manner. Smaller and denser aggregates of a homogeneous size that are more resistant to breaking up are formed with higher velocity gradient.


2019 ◽  
Vol 53 (7) ◽  
pp. 3391-3398 ◽  
Author(s):  
Joel P. Stokdyk ◽  
Susan K. Spencer ◽  
James F. Walsh ◽  
Jane R. de Lambert ◽  
Aaron D. Firnstahl ◽  
...  

Rural communities often rely on groundwater for potable water supply. In this study, untreated groundwater samples from 28 shallow groundwater wells in Finland (&#x003C;10 m deep and mostly supplying untreated groundwater to &#x003C;200 users in rural areas) were assessed for physicochemical water quality, stable water isotopes, microbial water quality indicators, host-specific microbial source tracking (MST) markers, and bacterial community composition, activity, and diversity (using amplicon sequencing of the 16S rRNA gene and 16S rRNA). Indications of surface water intrusion were identified in five wells, and these indications were found to be negatively correlated, overall, with bacterial alpha diversity (based on amplicon sequencing of the 16S rRNA gene). High levels of turbidity, heterotrophs, and iron compromised water quality in two wells, with values up to 2.98 nephelometric turbidity units (NTU), 16,000 CFU/ml, and 2,300&#x2009;&#x03BC;g/liter, respectively. Coliform bacteria and general fecal indicator <italic>Bacteroidales</italic> bacteria (GenBac3) were detected in 14 and 10 wells, respectively (albeit mostly at low levels), and correlations were identified between microbial, physicochemical, and environmental parameters, which may indicate impacts from nearby land use (e.g., agriculture, surface water, road salt used for deicing). Our results show that although water quality was generally adequate in most of the studied wells, the continued safe use of these wells should not be taken for granted.</p> <p><bold>IMPORTANCE</bold> Standard physicochemical water quality analyses and microbial indicator analyses leave much of the (largely uncultured) complexity of groundwater microbial communities unexplored. This study combined these standard methods with additional analyses of stable water isotopes, bacterial community data, and environmental data about the surrounding areas to investigate the associations between physicochemical and microbial properties of 28 shallow groundwater wells in Finland. We detected impaired groundwater quality in some wells, identified potential land use impacts, and revealed indications of surface water intrusion which were negatively correlated with bacterial alpha diversity. The potential influence of surface water intrusion on groundwater wells and their bacterial communities is of particular interest and warrants further investigation because surface water intrusion has previously been linked to groundwater contamination, which is the primary cause of waterborne outbreaks in the Nordic region and one of the major causes in the United States and Canada. IMPORTANCE Standard physicochemical water quality analyses and microbial indicator analyses leave much of the (largely uncultured) complexity of groundwater microbial communities unexplored. This study combined these standard methods with additional analyses of stable water isotopes, bacterial community data, and environmental data about the surrounding areas to investigate the associations between physicochemical and microbial properties of 28 shallow groundwater wells in Finland. We detected impaired groundwater quality in some wells, identified potential land use impacts, and revealed indications of surface water intrusion which were negatively correlated with bacterial alpha diversity. The potential influence of surface water intrusion on groundwater wells and their bacterial communities is of particular interest and warrants further investigation because surface water intrusion has previously been linked to groundwater contamination, which is the primary cause of waterborne outbreaks in the Nordic region and one of the major causes in the United States and Canada.


Water Policy ◽  
2005 ◽  
Vol 7 (6) ◽  
pp. 597-611 ◽  
Author(s):  
B. S. Chaitra ◽  
M. G. Chandrakanth

The synergistic effects of canals and tanks in groundwater recharge that contribute to an economically sustainable path of groundwater extraction are examined. Thirty farmers each with groundwater wells located in canal command (GWCI), in tank command (GWTI) and in solely well-irrigated areas (devoid of surface water bodies) (GWSI) are studied in Tumkur district of Karnataka. Applying Pontryagin's maximum principle to find the economically sustainable path of groundwater extraction, results indicated that by following the optimal path, the life of groundwater wells will increase by an additional 8, 17 and 24 years, respectively in GWSI, GWTI and GWCI areas over myopic (or uncontrolled) extraction. The additional net present value of benefit realized is US$822, US$1,907 and US$3,636 by optimal extraction in the three well areas. GWCI farmers realized the highest net returns (US$255) per hectare of gross groundwater irrigated area followed by GWTI (US$227.5) and GWSI (US$162.5). In GWTI (GWCI) amortized cost per cubic metre of groundwater was lower by 33% (53%) compared with GWSI, which reflects positive externality owing to the synergistic role of canals and tanks in groundwater recharge.


Author(s):  
John M. Wehrung ◽  
Richard J. Harniman

Water tables in aquifer regions of the southwest United States are dropping off at a rate which is greater than can be replaced by natural means. It is estimated that by 1985 wells will run dry in this region unless adequate artificial recharging can be accomplished. Recharging with surface water is limited by the plugging of permeable rock formations underground by clay particles and organic debris.A controlled study was initiated in which sand grains were used as the rock formation and water with known clay concentrations as the recharge media. The plugging mechanism was investigated by direct observation in the SEM of frozen hydrated sand samples from selected depths.


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