The use of isotope methods in the study of groundwater balance (Almeria, Spain)

I. L. Kharkhordin; I. V. Tokarev

Vol 153

Pages:

221-222

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RUS

Research article

Modern problems of geotechnical and hydrogeological surveys

The use of isotope methods in the study of groundwater balance (Almeria, Spain)

Authors:

I. L. Kharkhordin¹

I. V. Tokarev²

About authors

1 — St. Petersburg Branch, Institute of Geoecology RAS
2 — Institute of Geochronology and Precambrian Geology, RAS

Date submitted:

2002-06-20

Date accepted:

2002-07-02

Date published:

2003-03-20

Abstract

Hydrogeochemical and isotopic sampling of groundwater and surface water in the Almansora River basin was carried out in works on groundwater resources estimation in the province of Almeria (Spain). Surface and ground waters sampled in the Almansora River basin coincide with the general trend of atmospheric precipitation isotopic composition of the Mediterranean region, indicating an exclusively meteoric origin of ground and surface waters, the absence of significant isotopic fractionation after atmospheric precipitation, in particular due to evaporation. The insignificant role of transit flow in groundwater recharge within the hydrogeological unit of Auvers is shown.

Хархордин И.Л., Токарев И.В. Использование изотопных методов при изучении баланса подземных вод (Альмерия, Испания) // Записки Горного института. 2003. Т. 153. С. 221-222.

Kharkhordin I.L., Tokarev I.V. The use of isotope methods in the study of groundwater balance (Almeria, Spain) // Journal of Mining Institute. 2003. Vol. 153. p. 221-222.

References

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Craig H. Isotopic variations in meteoric water. Science, 133, 1702-1703.
De Vries J.J., Simmers I. Groundwater recharge: an overview of processes and challenges. Hydrogeology Journal, 2002, 10, 5-17.
Hoefs J. Stable Isotope Geochemistry. Springer, 1997, 201 p.

The use of isotope methods in the study of groundwater balance (Almeria, Spain)

Abstract

References

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