首页 | 本学科首页   官方微博 | 高级检索  
     检索      


Temporal dynamics of soil water balance components in a karst range in southeastern Spain: estimation of potential recharge
Authors:Yolanda Cantón  Luis Villagarcía  María José Moro  Penelope Serrano-Ortíz  Ana Were  Francisco Javier Alcalá
Institution:1. Departamento de Edafología y Química Agrícola , Universidad de Almería, Carretera de Sacramento s/n, La Ca?ada de San Urbano , E-04120, Almería, Spain ycanton@ual.es;3. Departamento de Sistemas Físicos y Químicos , Universidad Pablo de Olavide, Carretera de Utrera Km1 , E-41013, Sevilla, Spain;4. Departamento de Ecología , Universidad de Alicante , Apdo 99, Alicante, Spain;5. Centro Andaluz de Medio Ambiente (CEAMA), Av. del Mediterráneo s/n , E-18006, Granada, Spain;6. Department of Biology , University of Antwerp, Universiteitsplein 1 , B-2610, Wilrijk, Belgium;7. Department of Hydrology and Geo-environmental Sciences , Vrije Universiteit Amsterdam, De Boelelaan 1085 , 1081 HV, Amsterdam, The Netherlands;8. Estación Experimental de Zonas Aridas, Carretera de Sacramento s/n, La Ca?ada de San Urbano , E-04120, Almería, Spain
Abstract:Abstract

This paper analyses the temporal dynamics of soil water balance components in a representative recharge area of the Sierra de Gádor (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 Cantón, Y., Villagarcía, L., Moro, M. J., Serrano-Ortíz, P., Were, A., Alcalá, F. J., Kowalski, A. S., Solé-Benet, A., Lázaro, 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.
Keywords:potential recharge  evapotranspiration  soil moisture  soil water balance  Mediterranean  Sierra de Gádor
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号