New insights on the kinetics of the hydrochloric acid – carbonate rock reaction in the presence of sepiolite/palygorskite impurities

UDK: 552.54:622.276.1/.4
DOI: 10.24887/0028-2448-2024-8-42-47
Key words: acid treatment, carbonates, dolomite, sepiolite, palygorskite, rotating disk method, scanning electron microscopy (SEM)
Authors: E.S. Batyrshin (RN-BashNIPIneft LLC, RF, Ufa) A.A. Nikolaev (RN-BashNIPIneft LLC, RF, Ufa) D.R. Nikolaeva (RN-BashNIPIneft LLC, RF, Ufa) Yu.I. Timirov (RN-BashNIPIneft LLC, RF, Ufa) S.P. Sametov (RN-BashNIPIneft LLC, RF, Ufa)

The paper presents the results of an experimental study of the influence of trace amounts of sepiolite/palygorskite clay impurities on the hydrochloric acid – dolomite reaction. Acid dissolution studies were carried out using a rotating disk reactor at a temperature of 30°C and pressure of 10 MPa, which ensured the preservation of carbon dioxide, formed during the acid–rock reaction, in dissolved form. It has been found that the acid dissolution of dolomites that do not contain clay impurities is characterized by high rates and diffusion coefficients, comparable to the characteristics for limestones. At the same time, the presence of a small amount of clay leads to a decrease in the reaction rate by an order of magnitude. Scanning electron microscopy studies showed that a layer of transformed clay residues was formed on the surface of the samples. The presence of this layer prevents acid from reaching the rock surface and significantly reduces the rate of its dissolution. The founded effect of clays on the acid dissolution of carbonates is poorly understood, and for the case of sepiolite/palygorskite is described for the first time. The data obtained can be useful in selecting candidates for acid treatments and improvement of design development. In addition, the research results are intended to stimulate the search for new acid compositions and operating regimes during carbonate rocks acidizing in the presence of clay impurities.

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