Abstract

By using proximate analysis, X-ray diffraction mineral analysis, scanning electron microscope, contact angle measurement, and settlement simulation experiment, the coal fines produced from the coalbed methane wells of Binchang area were used to study the characteristics including particle size distribution, composition, morphology, wettability, and settleability. The results show that the particle size of coal fines produced from coalbed methane wells are mainly >20 mesh, ranging of 1-400 μm, and the particle size distribution curve is mainly dominated by the main-secondary bimodal type, with the main peak of 30-300 μm. The particle size from large to small is drill cutting coal fines, flowback coal fines, bailing coal fines, and pipeline filter coal fines. In terms of ash content, coal fines are higher than coal seam, and drilling cuttings are higher than bailing coal fines, while the fixed carbon content of the former is lower than that of the latter. The minerals of coal fines are mainly kaolinite, illite, quartz, and other 6 minerals, and the mineral types of drilling coal fines are the most abundant, while the bailing coal fines only contain illite and quartz. The roundness of coal fine particles ranges from excellent to poor in the order of bailing coal fines, pipeline filter coal fines, flowback coal fines, and drilling cuttings. However, the sorting of drilling cuttings is excellent, and the particle edges are straight, neat, and smooth, while the sorting of bailing coal fines is poor, and the particle edges are curved, uneven, and rough. The contact angles of coal fines are 40.25°-69.5°, indicating hydrophilous. The wettability of bailing coal fines is better than that of drilling cuttings. The particle size has a negative correlation with the wettability effect. The more obvious the modification effect of positive wetting agent is, the worse the modification effect of negative wetting agent is. The modification of surfactant has nothing to do with the particle size of the coal fines, but is closely related to organic components and minerals. The larger the coal particle size, the higher the settling rate, and the higher the ash content and the lower the fixed carbon content, the faster the settling rate. With the dividing point 150 mesh, the settling rate of large particles is mainly affected by particle size, while that of small particles is affected by the composition.

Highlights

  • Coal has the characteristics of low compressive strength, small Young’s modulus, small Poisson’s ratio, fragile, poor cementation, and easy to collapse

  • The screening results of drilling cutting coal fines (ZX) and bailing coal fines (LS) show (Figure 4) that the particle size distribution of coal fines is wide, and it is distributed from millimeter to micron

  • The micron particles in the drill cutting coal fines are mainly 20-80 mesh and 80-150 mesh, and the particle size is relatively coarse, especially the 80-150 mesh particles account for 66.67%, while the small size particles >150 mesh account for less than 10%

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Summary

Introduction

Coal has the characteristics of low compressive strength, small Young’s modulus, small Poisson’s ratio, fragile, poor cementation, and easy to collapse. The other type is caused by factors such as hydrodynamic denudation, coal destruction, and mechanical differences in different microscopic coal and rock components This type of coal fines has a small particle size and is mostly produced in the drainage and gas recovery process of coalbed methane (CBM) wells [10,11,12]. Based on the actual development of low-rank coalbed methane in the Binchang area of the southern Ordos Basin, the author conducts a comprehensive study on the particle size distribution, material composition, morphological characteristics, wettability, and subsidence of coal fines produced from coalbed methane wells. It is hoped to provide a reference for formulating reasonable coal fine control measures to avoid the adverse effects of coal fines on production

Geological Settings
Samples and Methods
Particle Size Distribution
Material Composition
Topographic Characteristics
Wettability
Settleability
Conclusions
Full Text
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