Abstract
A hydrochemical investigation was conducted in the Minqin Basin to identify the groundwater evolution and recharge in the aquifer. The mBr/Cl ratio is strongly depleted (average 0.000451) compared with sea water (0.0035), indicating an evaporite origin. The ionic ration plot, saturation index (SI), and chloro, alkaline indices (CAI) suggest that the dissolution of halite, the glauberite, gypsum, dolomite and calcite determine Na+, Cl-, Ca2+, Mg2+, SO42-, and HCO3- chemistry, but other processes, such as Na+ exchange for Ca2+ and Mg2+, and calcite precipitation also contribute to the water composition. The 6180 and 62 H in precipitation near the study area are linearly correlated, similar to that for the world meteoric water line (WMWL), with an equation of delta H-2 = 7.49 delta O-18 + 5.11 (r(2) = 0.97). According to radiocarbon residence time estimates, the deep groundwater is approximatety 40 ka old, and was recharged during a period when the climate was wetter and colder. The radiocarbon content of shallow groundwater shows a clear evolution along the groundwater flow path. From the beginning of the groundwater flow path to similar to 31 km the radiocarbon values are > 73.6 pmc, whereas beyond this point the values are < 42.9 pmc. Based on radiocarbon content, the shallow groundwater is older than 1 ka, and represents pataeowaters mixed with a limited quality of modern recharge. The rain-fed groundwater direct recharge was estimated by chloride mass balance (CMB) method to range from 1.55 to 1.64 mm yr(-1), with a mean value of 1.6 mm yr(-1). This value represents about 1.5% of local rainfall. The direct recharge volumes is about 0.666 x 10(8) m(3) yr(-1). Indirect recharge volumes by the surface water is about 0.945 x 10(8) m(3) yr(-1). The total natural recharge in the Minqin Basin is 1.6 x 10(8) m(3) yr(-1), whereas the groundwater abstraction has reached 11.6 x 10(8) m(3) yr(-1), far exceeding the groundwater natural recharge. (c) 2006 Elsevier B.V. All rights reserved.
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