Sr are broke up from other ions by eluting an enthusiastic aliquot as a result of a great quartz cation exchange column loaded with Eichrom Sr-Spec resin. The fresh 87Sr/86Sr ratio measurement error are 2σ and relates to the last quantitative put. The fresh B isotopic value within this analysis is shown in the δ, as well as the reproducibility is actually 2σ to own δ11B. The fresh parallel attempt employed for the test are D2811, the newest relative error from parallel samples try less than 15%. Biggest chemicals components of water products had been determined at the Secret Laboratory away from Geothermal Information Innovation and you can Utilization, Sinopec. Levels from biggest cations (Na+, K+, Ca2+, Mg2+, B3+, Si4+, Sr2+and Li+) and you will major anions (F−, Cl−, HCO3−and you may SO42−) had been dependent on ion chromatography (Dionex ICS-1100) having concerns away from less than dos%.
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It’s got certain imaginative bonus provides in it and also by looking for Maxi have fun with the wager for every spin is actually enhanced, reciprocally you will find double nuts icons and you will twice victories. The newest theme includes the brand new classic fruits icons in addition to the quantity 7 icon. Generally, the heat of your own earth is usually enhanced with depth, but the geothermal gradient is going to be influenced by the new rust away from radioactive elements, geological structure, and you can groundwater. Yet not, on the 15 faults try distributed inside YHTF, which enjoy a crucial role inside the groundwater migration and trigger the alteration away from temperatures occupation.
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Magnetotelluric survey and you will seismic prospecting reflected the brand new partially molten stone as the the lowest velocity–high conductive layer close to the BSGZ northwest of one’s YHGF (The newest Geothermal Geological Team away mobile slots with pay by phone bill from Tibet 1990). Simultaneously, with respect to the newest mining out of YHGF, the greatest mentioned heat and you will limit flow capability from deep geothermal liquid had been exposed from the main production well ZK208 within the BSGZ. Therefore, the major temperatures supply of YHGF try magmatic, provided by a top-velocity conductive level nearby the BSGZ found northwest of your YHGF. The brand new chemical compounds composition of the studied oceans and physicochemical parameters such as the heat, pH, and you can overall mixed solids (TDS) is actually placed in Dining table step 1.
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- The newest collection proportion from low cold groundwater and also the reservoir heat of your own YHGF is projected because of the Eqs.
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Weighed against the newest conduction-form of borehole, the fresh geothermal gradient values of the conduction–convection-kind of borehole are relatively large and you may demonstrate the new trait away from straight stratification. Such, the new geothermal gradient of ZK300 try 47.85 ℃/100 yards in the best 0–349 m point and then decreases to a single.72 ℃/100 yards between 349 and 407 yards, to improve once again to 6.56 ℃/100 m anywhere between 407 and 834 m. Due to the seemingly small thermal conductivity distinction away from rock, which change in geothermal gradient isn’t caused by the alteration out of thermal conductivity.
Also, K+ is generally originated from the fresh dissolution away from feldspars and you can micas during the water–stone correspondence. Additionally, On the YHGF, granitic stones including biotite stone porphyry, porphyritic biotite stone, and trachyandesite is generally distributed in the strong, that could provide silicate nutrition. Certain wells are influenced by the new upwelling thermal drinking water, with a convex-type depth–temperatures curve, and you may get into a conduction–convection-kind of borehole.
