Mecanismo de enriquecimento do gás de carvão no centro e leste da bacia de Ordos e método de previsão de áreas favoráveis

  • role: First author第一作者
  • Affiliation:

    College of Geosciences, China University of Petroleum (Beijing), Beijing 102249, China

    State Key Laboratory of Petroleum Resources and Engineering, Beijing 102249, China

  • Email:putycup@163.com
  • Introduction:蒲庭玉(2000—),男,博士研究生,油气藏形成机制与分布规律。E-mail:putycup@163.com。
PU Tingyu12,  
  • role: Corresponding author通信作者
  • Affiliation:

    College of Geosciences, China University of Petroleum (Beijing), Beijing 102249, China

    State Key Laboratory of Petroleum Resources and Engineering, Beijing 102249, China

  • Email:pangxq@cup.edu.cn
  • Introduction:庞雄奇(1961—),男,教授、博士研究生导师,油气藏形成机理与分布规律、含油气盆地分析与资源评价。E-mail:pangxq@cup.edu.cn。
PANG Xiongqi12*,  
  • Affiliation:

    College of Geosciences, China University of Petroleum (Beijing), Beijing 102249, China

    State Key Laboratory of Petroleum Resources and Engineering, Beijing 102249, China

LIN Hao12,  
  • Affiliation:

    College of Geosciences, China University of Petroleum (Beijing), Beijing 102249, China

    State Key Laboratory of Petroleum Resources and Engineering, Beijing 102249, China

CHEN Yuxuan12,  
  • Affiliation:

    College of Geosciences, China University of Petroleum (Beijing), Beijing 102249, China

    State Key Laboratory of Petroleum Resources and Engineering, Beijing 102249, China

WANG Lei12,  
  • Affiliation:

    College of Geosciences, China University of Petroleum (Beijing), Beijing 102249, China

    State Key Laboratory of Petroleum Resources and Engineering, Beijing 102249, China

ZHANG Ziyin12,  
  • Affiliation:

    College of Geosciences, China University of Petroleum (Beijing), Beijing 102249, China

    PetroChina Coalbed Methane Company Limited, Beijing 100028, China

DING Rong13,  
  • Affiliation:

    Research Institute of Petroleum Exploration and Development, PetroChina, Beijing 100083, China

    Unconventional Petroleum Research Institute, China University of Petroleum (Beijing), Beijing 102249, China

DENG Ze45,  
  • Affiliation:

    Research Institute of Petroleum Exploration and Development, PetroChina, Beijing 100083, China

TIAN Wenguang4,  
  • Affiliation:

    College of Geosciences, China University of Petroleum (Beijing), Beijing 102249, China

    State Key Laboratory of Petroleum Resources and Engineering, Beijing 102249, China

XIAO Huiyi12

Resumo

A exploração do gás de carvão em camadas profundas da bacia de Ordos alcançou um avanço significativo, abrindo um novo campo de desenvolvimento. Atualmente, ainda existem divergências no entendimento do mecanismo de enriquecimento do gás de carvão profundo e das direções favoráveis para exploração, indicando que a pesquisa do mecanismo de enriquecimento precisa ser aprofundada. Tomando a camada de carvão nº 8 do grupo Benxi do Carbonífero da parte centro-leste da bacia de Ordos como objeto de estudo, foram utilizados análise geológica, análise estatística e a teoria do campo dinâmico de petróleo e gás para explorar as condições de enriquecimento do gás de carvão profundo e a distribuição das áreas favoráveis. O estudo mostra que, na fase evolutiva crítica em que o índice de refletância da vitrinita (Ro) é aproximadamente de 1,5% a 2,5%, as condições de geração, armazenamento, condução e preservação do gás de carvão apresentam características evidentes de sobreposição espaço-temporal, exercendo papel controlador principal na formação e distribuição dos “sweet spots” ricos em gás, manifestados nos seguintes quatro pontos: ① nesta fase, a taxa de geração de gás do carvão é alta e a intensidade de geração forte, estabelecendo a base material para o enriquecimento do gás. ② a porosidade do carvão é anormalmente alta, atingindo um segundo pico em Ro cerca de 2,0%, com volume sincronizado de microporos e macroporos aumentando, fornecendo espaço de armazenamento de alta qualidade para o enriquecimento do gás de carvão. ③ o sistema de fraturas do carvão está altamente desenvolvido, com densidade máxima de fraturas em Ro cerca de 1,9%, formando canais eficientes de condução para o acúmulo e migração do gás de carvão. ④ as rochas encaixantes ao redor do carvão estão em campo dinâmico limitado, criando um bom ambiente de preservação para a formação dos sweet spots ricos em gás. Com base nisso, foi construído um modelo integrado de avaliação das áreas favoráveis ao gás de carvão profundo baseado na caracterização quantitativa dos quatro fatores “geração-armazenamento-condução-preservação”, utilizando método de sobreposição multiparâmetro para classificação e previsão hierárquica das áreas favoráveis dentro da área de estudo. Os resultados da previsão dividem a área em regiões favoráveis de classe I, II e III. Os resultados de perfuração indicam que a proporção de poços com alto teor de gás (conteúdo de gás ≥ 18 m³/t) nas áreas favoráveis da classe I chega a 90%, com teor médio de gás de 24,04 m³/t, e as previsões do modelo estão bem alinhadas com os resultados reais da exploração. Os resultados do estudo fornecem base teórica confiável e suporte técnico para a seleção otimizada de áreas favoráveis ao gás de carvão profundo na bacia de Ordos e para o planejamento de explorações futuras, sendo de grande importância para melhorar a eficiência do desenvolvimento de recursos e garantir a segurança energética nacional.

Palavras-chave

Estrutura porosa; Sistema completo de óleo e gás; Previsão de áreas favoráveis; Enriquecimento de óleo e gás; Gás de carvão; Bacia de Ordos

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