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21/05/2025 22:07
Sr are split from other ions by eluting an aliquot because of a quartz cation change line packed with Eichrom Sr-Specification resin. The new 87Sr/86Sr proportion dimension error are 2σ and you can pertains to the final quantitative lay. The newest B isotopic well worth within this analysis is expressed inside δ, as incredible hulk free 80 spins well as the reproducibility are 2σ to have δ11B. The newest parallel try useful for the exam try D2811, the newest cousin error from synchronous examples is actually below 15%. Biggest chemicals elements of drinking water trials had been determined during the Key Research from Geothermal Information Development and you can Usage, Sinopec. Concentrations from biggest cations (Na+, K+, Ca2+, Mg2+, B3+, Si4+, Sr2+and you may Li+) and you may biggest anions (F−, Cl−, HCO3−and you can SO42−) was influenced by ion chromatography (Dionex ICS-1100) that have uncertainties out of below dos%.
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It has certain resourceful incentive have inside and by searching for Maxi play the choice for each spin are enhanced, in exchange you can find twice insane signs and you may double victories. The newest theme contains the fresh vintage good fresh fruit signs in addition to the amount 7 symbol. In general, heat of one’s environment can be improved which have breadth, however the geothermal gradient will likely be affected by the new decay of radioactive aspects, geological construction, and groundwater. But not, in the 15 flaws try delivered inside the YHTF, which enjoy an important role inside the groundwater migration and you can result in the change away from heat profession.
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Magnetotelluric questionnaire and seismic to generate leads shown the new partially molten stone because the a minimal speed–high conductive coating near the BSGZ northwest of your own YHGF (The newest Geothermal Geological People away from Tibet 1990). Simultaneously, depending on the most recent exploration from YHGF, the best measured heat and limit circulate capacity out of strong geothermal fluid had been exposed by main design better ZK208 inside BSGZ. For this reason, the big temperature source of YHGF try magmatic, available with a high-speed conductive coating nearby the BSGZ discovered northwest of one’s YHGF. The newest toxins composition of your examined waters and you may physicochemical details such while the temperature, pH, and you may total demolished solids (TDS) is listed in Table step 1.
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- The fresh collection ratio out of superficial cold groundwater and also the tank temperatures of your YHGF are estimated because of the Eqs.
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In contrast to the newest conduction-kind of borehole, the newest geothermal gradient beliefs of one’s conduction–convection-kind of borehole is relatively highest and you can demonstrate the new feature away from straight stratification. For example, the fresh geothermal gradient out of ZK300 is 47.85 ℃/100 meters on the uppermost 0–349 m point and decrease to a single.72 ℃/100 meters anywhere between 349 and you may 407 meters, to increase once again to help you 6.56 ℃/100 yards anywhere between 407 and you can 834 yards. Considering the relatively short thermal conductivity difference away from stone, so it improvement in geothermal gradient is not caused by the change of thermal conductivity.
Also, K+ is generally originated from the brand new dissolution away from feldspars and you will micas throughout the water–material interaction. Furthermore, In the YHGF, granitic stones such biotite stone porphyry, porphyritic biotite stone, and you can trachyandesite is extensively distributed in the deep, that could provide silicate vitamins. Certain wells are influenced by the new upwelling thermal water, with a convex-form of breadth–temperature contour, and belong to a conduction–convection-type of borehole.