Abstract

In this research, we examined temporal variations in soil water content (q), infiltration patterns, and potential recharge at three sites with different mountain block positions in a semiarid Mediterranean climate in Baja California, Mexico: two located on opposing aspects (south- (SFS) and north-facing slopes (NFS)) and one located in a flat valley. At each site, we measured daily θ between 0.1 and 1 m depths from May 2014 to September 2016 in four hydrological seasons: wet season (winter), dry season (summer) and two transition seasons. The temporal evolution of θ and soil water storage (SWS) shows a strong variability that is associated mainly with high precipitation (P) pulses and soil profile depth at hillslope sites. Results shows that during high-intensity P events sites with opposing aspects reveal an increase of θ at the soil-bedrock interface suggesting lateral subsurface fluxes, while vertical soil infiltration decreases noticeably, signifying the production of surface runoff. We found that the dry soil conditions are reset annually at hillslope sites, and water is not available until the next wet season. Potential recharge occurred only in the winter season with P events greater than 50 mm/month at the SFS site and greater than 120 mm/month at the NFS site, indicating that soil depth and lack of vegetation cover play a critical role in the transport water towards the soil-bedrock interface. We also calculate that, on average, around 9.5% (~34.5 mm) of the accumulated precipitation may contribute to the recharge of the aquifer at the hillslope sites. Information about θ in a mountain block is essential for describing the dynamics and movement of water into the thin soil profile and its relation to potential groundwater recharge.

Original languageEnglish (US)
Article number1844
JournalWater (Switzerland)
Volume10
Issue number12
DOIs
StatePublished - Dec 13 2018

Fingerprint

Mediterranean Region
Mediterranean region
subversion
bedrock
Mexico
Infiltration
Water content
soil profiles
infiltration (hydrology)
soil water content
recharge
wet season
infiltration
Soil
soil water
hillslope
water content
mountains
Soils
soil water movement

Keywords

  • Aspect
  • Ecohydrology
  • Mountain block
  • Semiarid hydrology
  • Soil moisture

ASJC Scopus subject areas

  • Biochemistry
  • Geography, Planning and Development
  • Aquatic Science
  • Water Science and Technology

Cite this

Variations in soil water content, infiltration and potential recharge at three sites in a Mediterranean mountainous region of Baja California, Mexico. / Del Toro-Guerrero, Francisco José; Vivoni, Enrique; Kretzschmar, Thomas; Runquist, Stephen Holmes Bullock; Vázquez-González, Rogelio.

In: Water (Switzerland), Vol. 10, No. 12, 1844, 13.12.2018.

Research output: Contribution to journalArticle

Del Toro-Guerrero, Francisco José ; Vivoni, Enrique ; Kretzschmar, Thomas ; Runquist, Stephen Holmes Bullock ; Vázquez-González, Rogelio. / Variations in soil water content, infiltration and potential recharge at three sites in a Mediterranean mountainous region of Baja California, Mexico. In: Water (Switzerland). 2018 ; Vol. 10, No. 12.
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abstract = "In this research, we examined temporal variations in soil water content (q), infiltration patterns, and potential recharge at three sites with different mountain block positions in a semiarid Mediterranean climate in Baja California, Mexico: two located on opposing aspects (south- (SFS) and north-facing slopes (NFS)) and one located in a flat valley. At each site, we measured daily θ between 0.1 and 1 m depths from May 2014 to September 2016 in four hydrological seasons: wet season (winter), dry season (summer) and two transition seasons. The temporal evolution of θ and soil water storage (SWS) shows a strong variability that is associated mainly with high precipitation (P) pulses and soil profile depth at hillslope sites. Results shows that during high-intensity P events sites with opposing aspects reveal an increase of θ at the soil-bedrock interface suggesting lateral subsurface fluxes, while vertical soil infiltration decreases noticeably, signifying the production of surface runoff. We found that the dry soil conditions are reset annually at hillslope sites, and water is not available until the next wet season. Potential recharge occurred only in the winter season with P events greater than 50 mm/month at the SFS site and greater than 120 mm/month at the NFS site, indicating that soil depth and lack of vegetation cover play a critical role in the transport water towards the soil-bedrock interface. We also calculate that, on average, around 9.5{\%} (~34.5 mm) of the accumulated precipitation may contribute to the recharge of the aquifer at the hillslope sites. Information about θ in a mountain block is essential for describing the dynamics and movement of water into the thin soil profile and its relation to potential groundwater recharge.",
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AU - Vázquez-González, Rogelio

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