Groundwater circulation by hydrochemistry and isotope method

2015 ◽  
pp. 23-26 ◽  
Keyword(s):  
Isotope Method ◽  
Groundwater Circulation

EFFECT OF HEPARIN ON THE CORTICOSTERONE SECRETION RATE WITH A DESCRIPTION OF THE DOUBLE ISOTOPE METHOD USED

1967 ◽  
Vol 56 (1_Suppl) ◽  
pp. S140 ◽  
Author(s):  
A. F. Casparie ◽  
Th. J. Benraad ◽  
P. W. C. Kloppenborg ◽  
C. L. H. Majoor
Keyword(s):  
Secretion Rate ◽  
Isotope Method ◽  
Corticosterone Secretion ◽  
Double Isotope

scholarly journals Estimation of recharge in mountain hard-rock aquifers based on discrete spring discharge monitoring during base-flow recession

2021 ◽  
Author(s):  
Stefano Segadelli ◽  
Maria Filippini ◽  
Anna Monti ◽  
Fulvio Celico ◽  
Alessandro Gargini
Keyword(s):  
Hard Rock ◽  
Monitoring Program ◽  
Base Flow ◽  
Low Flow ◽  
Reliable Estimate ◽  
Spring Discharge ◽  
Aquifer Recharge ◽  
Clear Cut ◽  
Groundwater Circulation ◽  
Hard Rock Aquifers

AbstractEstimation of aquifer recharge is key to effective groundwater management and protection. In mountain hard-rock aquifers, the average annual discharge of a spring generally reflects the vertical aquifer recharge over the spring catchment. However, the determination of average annual spring discharge requires expensive and challenging field monitoring. A power-law correlation was previously reported in the literature that would allow quantification of the average annual spring discharge starting from only a few discharge measurements in the low-flow season, in a dry summer climate. The correlation is based upon the Maillet model and was previously derived by a 10-year monitoring program of discharge from springs and streams in hard-rock aquifers composed of siliciclastic and calcareous turbidites that did not have well defined hydrogeologic boundaries. In this research, the same correlation was applied to two ophiolitic (peridotitic) hard-rock aquifers in the Northern Apennines (Northern Italy) with well-defined hydrogeologic boundaries and base-outflow springs. The correlation provided a reliable estimate of the average annual spring discharge thus confirming its effectiveness regardless of bedrock lithology. In the two aquifers studied, the measurable annual outputs (i.e. sum of average annual spring discharges) could be assumed equal to the annual inputs (i.e. vertical recharge) based on the clear-cut aquifer boundaries and a quick groundwater circulation inferable from spring water parameters. Thus, in such setting, the aforementioned correlation also provided an estimate of the annual aquifer recharge allowing the assessment of coefficients of infiltration (i.e. ratio between aquifer recharge and total precipitation) ranging between 10 and 20%.

Estimating NOx removal capacity of urban trees using stable isotope method: A case study of Beijing, China

2021 ◽  
Vol 290 ◽  
pp. 118004
Author(s):  
Cheng Gong ◽  
Chaofan Xian ◽  
Bowen Cui ◽  
Guojin He ◽  
Mingyue Wei ◽  
...  
Keyword(s):  
Stable Isotope ◽  
Urban Trees ◽  
Nox Removal ◽  
Removal Capacity ◽  
Isotope Method ◽  
Beijing China

Changes in isotope ratios during domestic wastewater production

2007 ◽  
Vol 55 (4) ◽  
pp. 93-101 ◽  
Author(s):  
R.P.S. Schilperoort ◽  
H.A.J. Meijer ◽  
C.M.L. Flamink ◽  
F.H.L.R. Clemens
Keyword(s):  
Drinking Water ◽  
Catchment Area ◽  
High Efficiency ◽  
Domestic Wastewater ◽  
Isotopic Ratios ◽  
Small Catchment ◽  
Sewer Systems ◽  
Isotope Method ◽  
Catchment Areas ◽  
Large Heterogeneity

This paper presents considerations for the application of the natural water isotope method on catchment areas. For the estimation of the amount of infiltration and inflow in sewer systems the paper shows two applications in the Netherlands: one successful application on a relatively small catchment area with a simple geo-hydrological groundwater system and one unsuccessful application in an area that shows a large heterogeneity of δ18O values in groundwater. Also, the paper focuses on the validity of the assumption that the isotopic ratios of drinking water are equal to those of strict domestic wastewater. In the transition from drinking water to strict wastewater it is shown that changes in isotopic composition of the water due to evaporation in common household appliances and effects inside the human body are insignificant. However, the presence of high-efficiency condensing boilers in an area can significantly influence the δ18O value of strict wastewater, especially in winter months. This effect should be taken into account when applying the isotope method in such areas.

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