基于保压煤心的瓦斯压力演化规律及其计算方法

The evolution law of gas pressure in pressure-preserved coal cores and its calculation method

  • 摘要: 【目的和方法】 煤层原位瓦斯压力是煤矿安全生产以及煤层气资源评估的重要参数。针对现阶段煤层原位瓦斯压力测定周期长、测算结果受多种参数影响等局限,利用自主搭建的保压煤心瓦斯压力演化实验系统,开展了不同含水率下保压煤心等温吸附和扩容解吸实验,在揭示保压煤样瓦斯压力演化规律的基础上,基于“深部煤层原位保压保瓦斯取心工艺”形成的“煤层原位瓦斯压力”理论计算原理,提出了考虑含水率的瓦斯压力计算修正模型,并验证了其可靠性。【结果和结论】 结果表明:(1)受高瓦斯压力影响,保压空间内瓦斯压力更容易达到新的平衡,在等温吸附过程中瓦斯压力呈阶段性演化特征,保压煤心瓦斯压力先快速下降至某一值,升压后再逐渐趋于平衡。(2)受煤样介孔为主、微孔孔容较大孔隙特征的影响,不同含水率保压煤心等温吸附实验中,含水率越高,平衡时间越长,吸附压降越低。(3)基于不同含水率保压煤心扩容解吸实验计算了煤样瓦斯压力,各含水率下瓦斯压力计算结果平均相对误差分别为2.22%、1.29%、0.39%、0.80%,修正后的瓦斯压力计算方法在各含水率下均有较高准确度。在确保计算精度可靠的基础上,采用保压空间内煤心平衡瓦斯压力计算煤层原位瓦斯压力有望为煤层原位瓦斯压力测定提供可靠便捷的计算方法。

     

    Abstract: Objective and Methods Coalbed in-situ gas pressure is a crucial parameter for coal mine safety production and coalbed methane resource assessment. Addressing the current limitations of long measurement cycles and the influence of multiple parameters on the measurement results of in-situ coalbed gas pressure, an experimental system for the evolution of gas pressure in pressure-preserved coal cores was independently constructed. Experiments on isothermal adsorption and expansion desorption of pressure-preserved coal cores under different moisture contents were conducted. Based on revealing the evolution law of gas pressure in pressure-preserved coal samples, a theoretical calculation principle for "in-situ coalbed gas pressure" formed by the "in-situ pressure-preserved gas-preserved coring process for deep coal seams" was proposed. A correction model for gas pressure calculation considering moisture content was developed and its reliability was verified. Results and Conclusions The results indicate that: (1) Influenced by high gas pressure, the gas pressure within the pressure-preserved space more easily reaches a new equilibrium. During the isothermal adsorption process, the gas pressure exhibits a staged evolution characteristic, where the gas pressure in the pressurepreserved coal core first rapidly decreases to a certain value, then increases before gradually stabilizing. (2) Due to the pore characteristics of the coal sample being dominated by mesopores and having a large micropore volume, in the isothermal adsorption experiments of pressure-preserved coal cores with different moisture contents, the higher the moisture content, the longer the equilibrium time and the lower the adsorption pressure drop. (3) The gas pressure of the coal samples was calculated based on the expansion desorption experiments of pressure-preserved coal cores with different moisture contents. The average relative errors of the gas pressure calculation results under various moisture contents were 2.22%, 1.29%, 0.39%, and 0.80%, respectively. The corrected gas pressure calculation method demonstrated high accuracy across all moisture contents. Ensuring reliable calculation accuracy, the use of equilibrium gas pressure within the pressure-preserved space to calculate in-situ coalbed gas pressure is expected to provide a reliable and convenient calculation method for the determination of in-situ coalbed gas pressure.

     

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