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Temporal dynamics of soil water balance components in a karst range in southeastern Spain: estimation of potential recharge.

Authors :
Cantón, Yolanda
Villagarcía, Luis
José Moro, María
Serrano-Ortíz, Penelope
Were, Ana
Javier Alcalá, Francisco
Kowalski, AndrewS.
Solé-Benet, Alberto
Lázaro, Roberto
Domingo, Francisco
Source :
Hydrological Sciences Journal/Journal des Sciences Hydrologiques. 2010, Vol. 55 Issue 5, p737-753. 17p. 3 Charts, 6 Graphs, 1 Map.
Publication Year :
2010

Abstract

This paper analyses the temporal dynamics of soil water balance components in a representative recharge area of the Sierra de Gador (Almeria, southeastern Spain) in two hydrological years. Two approaches are used to estimate daily potential recharge (PR): Approach 1 based on deriving PR from the water balance as the difference between measurements of rainfall (P) and actual evapotranspiration (E) obtained by eddy covariance; and Approach 2 with PR obtained from the dynamic pattern of the soil moisture (θ) recorded at two depths in the site's thin soil (average 0.35 m thickess). For the hydrological year 2003/04, which was slightly drier than the 30-year average, E accounted for 64% of rainfall and occurred mainly in late spring and early summer. The PR estimated by Approach 1 was 181 ± 18 mm year-1 (36% of rainfall), suggesting an effective groundwater recharge in the study area. In the unusually dry hydrological year 2004/05, E was about 215 mm year-1, close to the annual rainfall input, and allowing very little (8 ± 12 mm year-1) PR according to Approach 1. Estimation of PR based on Approach 2 resulted in PR rates lower than those found by Approach 1, because Approach 2 does not take into account the recharge that occurs through preferential flow pathways (cracks, joints and fissures) which were not monitored with the θ probes. Moreover, using Approach 2, the PR estimates differed widely depending on the time scale considered: with daily mean θ data, PR estimation was lower, especially in late spring, while θ data at 30 min resolution yielded a more reliable prediction of the fraction of total PR resulting from the downward movement of soil water by gravity. Citation Canton, Y., Villagarcia, L., Moro, M. J., Serrano-Ortiz, P., Were, A., Alcala, F. J., Kowalski, A. S., Sole-Benet, A., Lazaro, R. & Domingo, F. (2010) Temporal dynamics of soil water balance components in a karst range in southeastern Spain: estimation of potential recharge. Hydrol. Sci. J. 55(5), 737-753. [ABSTRACT FROM AUTHOR]

Details

Language :
English
ISSN :
02626667
Volume :
55
Issue :
5
Database :
Academic Search Index
Journal :
Hydrological Sciences Journal/Journal des Sciences Hydrologiques
Publication Type :
Academic Journal
Accession number :
51981540
Full Text :
https://doi.org/10.1080/02626667.2010.490530