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March 18, 2026Processes2 citationsOpen Access

Geological Controls and Geochemical Responses Governing CBM Well Productivity in the Sigong River Block of the Southern Junggar Basin, China

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LXLexin XuSTShuling TangYZYuanhao Zhi

Key Points

  • This research aims to clarify the geological and geochemical factors affecting coalbed methane well productivity in the Sigong River block.
  • Conducted integrated analysis of geological and hydrogeochemical characteristics.
  • Classified CBM wells into four distinct productivity types based on production performance.
  • Examined relationships between burial depth, structural conditions, gas content, and permeability.
  • Developed a productivity response index model using critical geological and geochemical parameters.
  • Identified four productivity types: Type I (high productivity, low water), Type II (moderate), Type III (high water, low gas), and Type IV (low productivity).
  • Optimal conditions for Type I wells include 700–1000 m burial depth, syncline structure, high gas content, and favorable permeability.
  • Deep coal seams (>1400 m) correlate with low gas and water production.
  • Geochemical signatures differentiate well types, with specific water chemistry indicating productivity.

Abstract

The southern Junggar Basin in Xinjiang is rich in coalbed methane (CBM) resources. Large-scale development is underway in the Sigong River block (SGR block) of the Fukang West Block. Based on an integrated analysis of geological and hydrogeochemical characteristics, this study clarifies the key factors affecting CBM well productivity in the SGR block. Based on gas and water production performance, four distinct productivity types of CBM wells are identified, which are jointly controlled by burial depth, local structural and hydraulic disturbance, and also governed by synergistic interplay between gas content and permeability. The optimal geological combination—comprising the 700–1000 m burial depth, syncline core structure, stagnant hydrodynamic conditions, relatively high gas content, and favorable permeability—collectively contributes to the high-productivity Type I wells with low water production. In contrast, deep coal seams (>1400 m), characterized by reduced gas content and extremely low permeability, correspond to Type IV wells, which exhibit low gas and water production. Type II wells, located in the 1000–1400 m interval, exhibit moderate and variable productivity controlled by the interplay between high gas content and a wide range of permeability. Shallow margins (<700 m) affected by coal combustion and surface water influx produce high-water and low-gas wells (Type III). Geochemical signatures effectively differentiate between these types: closed, stagnant environments (Types I/II) are marked by a Na-Cl-HCO3/Na-HCO3-Cl water type, moderate total dissolved solids, and low sodium chloride coefficients, while open hydrodynamic conditions (Type III) are indicated by Na-SO4-HCO3 water with high sodium chloride coefficients. A δD-H2O/δ18O-H2O ratio of 7–9, combined with favorable TDS and water type, is identified as a key indicator of high productivity. Based on these relationships, a productivity response index model incorporating critical geological and geochemical parameters was developed. This model provides a practical tool for predicting CBM well performance and targeting sweet spots, offering significant value for exploring geologically and hydrologically complex basins.

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Cite This Study

Xu et al. (2026) studied this question.

synapsesocial.com/papers/69ba42fb4e9516ffd37a3b4bhttps://doi.org/10.3390/pr14060936
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