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Carbonate Stimulation with Biodegradable Chelating Agent Having Broad Unique Spectrum (pH, Temperature, Concentration) Activity

机译:碳酸盐刺激具有具有广义独特谱(pH,温度,浓度)活性的可生物降解的螯合剂

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The use of chelating agents to stimulate carbonate reservoirs has continued to increase since their first inception. A distinct chelant is presented in this paper. The new chelant is fully biodegradable and can be used in fluid formulations that specifically target the formation characteristics. The chelating agent can be used in concentrations from 0.2 to 0.6 M, with a pH of 1, 2, or 4, and is effective from 125 to 350°F. The specific fluid composition is a function of the mineralogy and rock lithology as well as temperature. Core flow testing at less than 200°F shows optimum dissolution with low-concentration, low-pH fluid; while, at temperatures >200°F, higher concentrations of chelant is optimum. The representative pore volume (PV) breakthrough curves provide an indication of the distinct reactivity of this chelant to other known chelants. Analytical characterization of the spent fluid (elemental analysis, pH) and of the core (CT imaging) are used to show that the activity in which the fluid displays on select limestone (calcite or dolomite) cores can be exploited to enhance wormhole structure generation. Core permeabilities ranged from 0.4 to 10 md, and core dimensions (radius × length) corresponded to 1- × 4-in., 1.5- × 6-in, and 2- × 6- or 10-in., respectively. The chelating fluid maintains in solution dissolved calcium, a property that is magnified because of the ease with which the acidic fluid spends as it is transported through the limestone matrix. The concentration of the chelant can be optimized to a specific pH to maximize its dissolution capacity. Overall, the new chelating agent affords superior complexation capacity from low pH to near neutral pH values while dissolving the minimum amount of mineral and effectively increasing porosity. The chelant expands the range of available options in the area of treating fluids for carbonate stimulation.
机译:自首次成立以来,使用螯合剂刺激碳酸盐储层仍在继续增加。本文提出了一个独特的螯合剂。新的螯合剂是完全可生物降解的,可用于专门针对地层特征的流体制剂中。螯合剂可以以0.2至0.6μm的浓度为0.2-0.6μm,pH为1,2或4,从125-350°F有效。特定的流体组合物是矿物学和岩石岩性以及温度的函数。核心流动测试小于200°F,显示出低浓度低pH流体的最佳溶解;虽然,在温度> 200°F时,较高浓度的螯合剂是最佳的。代表性孔体积(PV)突破性曲线提供了该螯合剂与其他已知螯合剂的不同反应性的指示。废液(元素分析,pH)和核心(CT成像)的分析表征用于表明可以利用在选择石灰石(方解石或多粒管)芯上的流体显示器的活性来增强虫洞结构的产生。核心渗透率范围为0.4至10 md,核心尺寸(半径×长度)分别对应1×4英寸,1.5×6英寸和2×6-或10英寸。螯合液在溶液中保持溶解钙,由于酸性流体在通过石灰石基质中运输而易于放大的性质。螯合剂的浓度可以优化至特定的pH以最大化其溶解能力。总体而言,新的螯合剂在低pH下至溶解的最小矿物质和有效增加孔隙率的同时提供优异的络合能力。螯合剂扩大了用于碳酸盐刺激的液体区域中的可用选项的范围。

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