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首页> 外文期刊>American Chemical Society, Division of Fuel Chemistry, Preprints >FORMULATING MIXTURES OF NANOPARTICLES, POLYMERS AND SURFACTANTS TO STABILIZE HIGH VISCOSITY HIGH INTERNAL PHASE CO2-INWATER FOAMS
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FORMULATING MIXTURES OF NANOPARTICLES, POLYMERS AND SURFACTANTS TO STABILIZE HIGH VISCOSITY HIGH INTERNAL PHASE CO2-INWATER FOAMS

机译:配制纳米颗粒,聚合物和表面活性剂的混合物以稳定高粘度高内相二氧化碳室内泡沫

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Hydraulic fracturing is ubiquitous and allows production of oilnand gas from unconventional reservoirs that previously were deemednas uneconomical for production. Hydraulic fracturing fluids arenrequired in this process to build up the pressure to fracture thenreservoir rock and also transport proppants deep into the newlynopened fractures to keep the fractures being open after the pumpingnstops. Water-based fracturing fluids such as slick-water and waterbasedngels which contain ~99% v/v of water are widely usednnowadays and lead to huge fresh water consumption. In averagenabout 5 million gallons of water were consumed per fracture job, andnin total the water consumed in drilling & completions accounts forn0.3% of US fresh water consumption each year. Large amount ofnwater consumption has a series of potential problems such as thenlimitations of water supply due to government regulations. Alsonespecially in offshore production, the water quality of the waternsupply may not meet the water quality required for hydraulicnfracturing operations and thus additional cost of water treatment.nFurther, it is observed that water-based hydraulic fracturing fluidsngive less than expected production in some reservoirs due to variousnmechanisms such as water-blocking in water-wet fractures, claynswelling and gel damage of the proppant bed.
机译:水力压裂是无处不在的,它允许从以前认为是不经济的非常规储层中开采石油和天然气。在此过程中,需要液压压裂液来增加压力,以使裂缝破裂,然后使储层岩石破裂,并将支撑剂输送到新近打开的裂缝中,以使裂缝在泵送停止后保持打开状态。如今,含水压裂液(如滑水和水基含胶量约99%v / v的水)被广泛使用,并导致大量的淡水消耗。每个压裂作业平均消耗约500万加仑水,而在钻探和完井中所消耗的水总计占美国每年淡水消耗量的0.3%。大量的水消耗具有一系列潜在的问题,例如由于政府法规导致的供水限制。另外,特别是在海上生产中,水源的水质可能无法满足水力压裂作业所需的水质,因此无法支付额外的水处理费用。各种机制,例如水湿裂缝中的阻水,黏土膨胀和支撑剂床的凝胶破坏。

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