New Tools for Coherent Information Base for IWRM in Arid Regions: The Upper Mega Aquifer System on the Arabian Peninsula

In arid regions like the Arabian Peninsula, available water resources are essentially restricted to groundwater, requiring a detailed understanding of the local and regional hydrogeological conditions and water budgets. In the framework of the IWAS initiative, the 1.8 × 106 km2 large sedimentary Upper Mega Aquifer of the Arabian Peninsula was chosen as a model region to develop concepts and methodologies to quantify water fluxes in such an arid environment. Field and laboratory studies were conducted to analyse (i) precipitation patterns, (ii) groundwater recharge, (iii) the hydrochemical evolution of groundwater and (iv) evaporation particularly from Sabkhas in detail. Results were used as input parameters for a 3D groundwater model for the central part of the Peninsula, which was later extended to the full dimension of the Upper Mega Aquifer. It could be shown that in such a region different components of the water cycle have to be quantified with great care and several methods should be applied to reduce data uncertainty. It was not possible to make use out of satellite products to receive reliable actual precipitation patterns for the peninsula. It was observable; recharge estimations based on average annual precipitation are not applicable but should be based on singular precipitation events. A threshold of 6 mm/event was derived, below of which no recharge in sand seas occurs. The loss of water from UMA, due to sabkha evaporation reaches about 40 mm/a under the given recent climatic conditions.

[1]  T. Dinçer,et al.  Study of the infiltration and recharge through the sand dunes in arid zones with special reference to the stable isotopes and thermonuclear tritium , 1974 .

[2]  T. Schmugge,et al.  Survey of methods for soil moisture determination , 1980 .

[3]  A. Subyani Use of chloride-mass balance and environmental isotopes for evaluation of groundwater recharge in the alluvial aquifer, Wadi Tharad, western Saudi Arabia , 2004 .

[4]  Jeffrey L. Imes,et al.  How wet is wet? Precipitation constraints on late quaternary climate in the southern Arabian Peninsula , 1995 .

[5]  C. Siebert,et al.  The hydrochemical identification of groundwater flowing to the Bet She’an-Harod multiaquifer system (Lower Jordan Valley) by rare earth elements, yttrium, stable isotopes (H, O) and Tritium , 2012 .

[6]  C. Schüth,et al.  Surface and subsurface conceptual model of an arid environment with respect to mid- and late Holocene climate changes , 2013, Environmental Earth Sciences.

[7]  Mamdouh Shahin,et al.  Water Resources and Hydrometeorology of the Arab Region , 2007 .

[8]  E. Rosenthal,et al.  Rare earths and yttrium hydrostratigraphy along the Lake Kinneret–Dead Sea–Arava transform fault, Israel and adjoining territories , 2003 .

[9]  B. Purser The Persian Gulf : Holocene carbonate sedimentation and diagenesis in a shallow epicontinental sea , 1973 .

[10]  Scott B. Jones,et al.  A Review of Advances in Dielectric and Electrical Conductivity Measurement in Soils Using Time Domain Reflectometry , 2003 .

[11]  M. Bau Scavenging of dissolved yttrium and rare earths by precipitating iron oxyhydroxide: experimental evidence for Ce oxidation, Y-Ho fractionation, and lanthanide tetrad effect , 1999 .

[12]  P. Braconnot,et al.  Monsoon response to changes in Earth's orbital parameters: comparisons between simulations of the Eemian and of the Holocene , 2008 .

[13]  P. Möller The distribution of rare earth elements and yttrium in water-rock interactions: field observations and experiments , 2002 .

[14]  Y. Hong,et al.  The TRMM Multisatellite Precipitation Analysis (TMPA): Quasi-Global, Multiyear, Combined-Sensor Precipitation Estimates at Fine Scales , 2007 .

[15]  M. Siddall,et al.  Sea-level fluctuations during the last glacial cycle , 2003, Nature.

[16]  S. Hasiotis,et al.  Paleoclimatic significance of Early Holocene faunal assemblages in wet interdune deposits of the Wahiba Sand Sea, Sultanate of Oman , 2005 .

[17]  P. Hoelzmann,et al.  Precipitation estimates for the eastern Saharan palaeomonsoon based on a water balance model of the West Nubian Palaeolake Basin , 2000 .

[18]  P. Smedley The geochemistry of rare earth elements in groundwater from the Carnmenellis area, southwest England , 1991 .

[19]  M. Noori,et al.  Hydrogeology of the Umm Er Radhuma aquifer, Saudi Arabia, with reference to fossil gradients , 1982, Quarterly Journal of Engineering Geology.

[20]  K. Kupfer,et al.  Ortsauflösende Feuchtemessung mit Time-Domain-Reflektometrie (Spatial Water Content Measurement with Time-Domain Reflectometry) , 2007 .

[21]  Marios Sophocleous,et al.  Groundwater recharge estimation and regionalization: the Great Bend Prairie of central Kansas and its recharge statistics , 1992 .

[22]  B. Scanlon,et al.  Assessing controls on diffuse groundwater recharge using unsaturated flow modeling , 2005 .

[23]  A. Martín,et al.  Late Permian to Holocene Paleofacies Evolution of the Arabian Plate and its Hydrocarbon Occurrences , 2001, GeoArabia.

[24]  G. Gee,et al.  Estimating recharge rates for a groundwater model using a GIS , 1996 .

[25]  H. Stewart Edgell,et al.  Arabian Deserts: Nature, Origin and Evolution , 2006 .

[26]  Impact of Preboreal to Subatlantic shifts in climate on groundwater resources on the Arabian Peninsula , 2013, Environmental Earth Sciences.

[27]  J. Janowiak,et al.  CMORPH: A Method that Produces Global Precipitation Estimates from Passive Microwave and Infrared Data at High Spatial and Temporal Resolution , 2004 .

[28]  G. Clarke Topp,et al.  State of the art of measuring soil water content , 2003 .

[29]  Marios Sophocleous,et al.  From safe yield to sustainable development of water resources—the Kansas experience , 2000 .

[30]  N. Klasen,et al.  The early Holocene humid period in NW Saudi Arabia – Sediments, microfossils and palaeo-hydrological modelling , 2012 .

[31]  A. P. Annan,et al.  Electromagnetic determination of soil water content: Measurements in coaxial transmission lines , 1980 .

[32]  T. D. Mitchell,et al.  An improved method of constructing a database of monthly climate observations and associated high‐resolution grids , 2005 .

[33]  N. Grevesse,et al.  Abundances of the elements: Meteoritic and solar , 1989 .

[34]  W. Edmunds,et al.  Groundwater recharge estimation using chloride, stable isotopes and tritium profiles in the sands of northwestern Senegal , 1996 .

[35]  K. Johannesson,et al.  Rare earth element fractionation and concentration variations along a groundwater flow path within a shallow, basin-fill aquifer, southern Nevada, USA , 1999 .

[36]  William M. Shehata,et al.  Preconstruction solution for Groundwater rise in Sabkha , 1993 .

[37]  W. Edmunds,et al.  Published online in Wiley InterScience (www.interscience.wiley.com) DOI: 10.1002/hyp.6335 Global synthesis of groundwater recharge in semiarid andaridregions , 2022 .

[38]  Jeffrey P. Walker,et al.  In situ measurement of soil moisture: a comparison of techniques | NOVA. The University of Newcastle's Digital Repository , 2004 .

[39]  Warren W. Wood,et al.  Chloride mass-balance method for estimating ground water recharge in arid areas: examples from western Saudi Arabia , 1996 .

[40]  Manfred Mudelsee,et al.  Holocene Forcing of the Indian Monsoon Recorded in a Stalagmite from Southern Oman , 2003, Science.

[41]  P. Cook,et al.  Spatial variability of groundwater recharge in a semiarid region , 1989 .

[42]  Robert Jacob,et al.  Simulating the transient evolution and abrupt change of Northern Africa atmosphere–ocean–terrestrial ecosystem in the Holocene ☆ , 2007 .