Groundwater Quality Changes Resulting from a Surface Bromide Application to a Pasture

1985 ◽  
Vol 14 (4) ◽  
pp. 543-548 ◽  
Author(s):  
L. B. Owens ◽  
R. W. Van Keuren ◽  
W. M. Edwards
Water ◽  
2020 ◽  
Vol 13 (1) ◽  
pp. 51
Author(s):  
Kyoochul Ha ◽  
Eunhee Lee ◽  
Hyowon An ◽  
Sunghyun Kim ◽  
Changhui Park ◽  
...  

This study was conducted to evaluate seasonal groundwater quality due to groundwater pumping and hydrochemical characteristics with groundwater level fluctuations in an agricultural area in Korea. Groundwater levels were observed for about one year using automatic monitoring sensors, and groundwater uses were estimated based on the monitoring data. Groundwater use in the area is closely related to irrigation for rice farming, and rising groundwater levels occur during the pumping, which may be caused by the irrigation water of rice paddies. Hydrochemical analysis results for two separate times (17 July and 1 October 2019) show that the dissolved components in groundwater decreased overall due to dilution, especially at wells in the alluvial aquifer and shallow depth. More than 50% of the samples were classified as CaHCO3 water type, and changes in water type occurred depending on the well location. Water quality changes were small at most wells, but changes at some wells were evident. In addition, the groundwater quality was confirmed to have the effect of saltwater supplied during the 2018 drought by comparison with seawater. According to principal component analysis (PCA), the water quality from July to October was confirmed to have changed due to dilution, and the effect was strong at shallow wells. In the study areas where rice paddy farming is active in summer, irrigation water may be one of the important factors changing the groundwater quality. These results provide a qualitative and quantitative basis for groundwater quality change in agricultural areas, particularly rice paddies areas, along with groundwater level and usage.


2016 ◽  
Vol 20 (2) ◽  
Author(s):  
Sudarmadji Sudarmadji

Groundwater is the main domestic water supply of the population of the Yogyakarta Special Region, both in the urban and as well as in the rural area due to its quantity and quality advantages. The rapid population growth has caused an increase of groundwater demand, consequently it is facing some problems to the sustainability of groundwater supply. Lowering of groundwater level has been observed in some places, as well as the degradation of groundwater quality. Earthquake which stroke Yogyakarta on 27 May 2006, damaged buildings and other infrastructures in the area, including roads and bridges. It might also damage the underground structures such as septic tanks, and pipes underneath the earth surface. It might cause cracking of the geologic structures. Furthermore, the damage of underneath infrastructures might create groundwater quality changes in the area. Some complains of local community on lowering and increasing groundwater level and groundwater quality changes were noted. Field observation and investigation were conducted, including collection of groundwater samples close to (the) pollution sources. Laboratory analyses indicated that some parameters increased to exceed the drinking water quality standards. The high content of Coli form bacteria possibly was caused by contamination of nearby septic tanks or other pollution sources to the observed groundwater in the dug well.


Author(s):  
V. Yu. Abramov ◽  
B. V. Borevsky ◽  
G. E. Ershov

The hydrogeological, geoecological and economical risks connected with the non-confirmation of groundwater discharge, levels and quality forecast calculations while the evaluation of the reserves, have been considered. Improving the reliability of the forecasts of the potable groundwater quality changes and the corresponding reduction in the risks associated with their non-confirmation, can be achieved by carrying out the special hydrogeochemical researches of operated deposits, including isotope researches. On the basis of such studies, a comparison ofprediction calculations on the observed data of the results of the exploration and actually observed indicators of the quality of groundwater can be made, and the theoretical and methodical bases of subsoil study and forecasting can be performed.


2013 ◽  
Vol 85 (3) ◽  
pp. 553-567 ◽  
Author(s):  
Maneesha P. Ginige ◽  
Anna H. Kaksonen ◽  
Christina Morris ◽  
Mark Shackelton ◽  
Bradley M. Patterson

2016 ◽  
Vol 0 (2) ◽  
pp. 99-106
Author(s):  
N.G. Lyuta ◽  
G.G. Lyutyj ◽  
S.M. Prykhodko

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