高碱煤中碱性金属的有机赋存形式及其地质意义

Organic association of alkali and alkaline earth metals in a high alkali coal and its geological significance

  • 摘要:
    目的 煤中碱性金属影响煤加工利用,通过水洗、浮选、重液分离等可去除大部分水溶态和矿物中的碱性金属,而与有机质结合的碱性金属难以脱除。为探究高碱煤中碱性金属的有机赋存形式,选取不同镜惰比的新疆准东煤田高碱煤样,通过逐级化学提取,结合23Na CP/MAS NMR和TEM-EDS等实验手段,系统分析煤中碱性金属的含量、分布规律和赋存状态。
    结果 (1)准东煤中碱性金属以水溶态和离子交换态为主,其中Na+和Ca2+因含量显著高于其他碱性金属离子,更易通过离子交换与煤分子相互作用。(2)水溶态和离子交换态碱性金属主要通过与煤有机质中的含氧官能团(羰基、羧基、酚羟基)通过吸附结合。量子化学计算结果表明,Na主要通过与羧酸根或羰基结合形成羧酸Na或配位结构(−C=ONa+);大部分Ca以化学吸附形式与有机分子结合,表现出较强的离子键作用。随镜质组含量的增加,离子交换态Na从28.3%增加到30.9%,离子交换态Ca从62.3%增加到70.1%,表明镜质组更易与碱性金属结合。(3)碱性金属离子随地下水流动发生迁移,在含氧官能团附近吸附,吸附能力受控于煤的显微组分,这种显微组分−官能团−吸附能力的级联控制,是碱性金属离子差异性富集的根本原因。
    结论 碱性金属Na、Ca的有机赋存规律提供了明确的地质意义,为预测煤层垂向碱性金属富集层位提供了重要的煤岩学依据;同时,碱性金属离子占据含氧官能团的吸附位点,对煤层气吸附产生不利影响。未来需重点探究碱性金属离子对煤层气竞争吸附的分子抑制机制,为高碱煤的合理清洁开发利用提供理论依据。

     

    Abstract:
    objective The occurrence of alkaline and alkaline earth metals (AAEMs) in coal significantly impacts its processing and utilization. Water-soluble and mineral-hosted AAEMs can be largely removed by water washing, flotation, or heavy-liquid separation, AAEMs organically bound to the coal matrix, however, is difficult to eliminate. To investigate the organic AAEMs in the high-alkali coal, the Zhundong coals with varying vitrinite/inertinite ratios were selected in this work. Using integrating sequential chemical extraction with 23Na CP/MAS NMR and TEM-EDS, the AAEMs’ content, distribution patterns, and occurrences were systematically analyzed.
    Results (1) AAEMs in Zhundong coals primarily exist as water-soluble and ion-exchangeable species. Na+ and Ca2+ exhibit significantly higher concentrations than other AAEM ions and demonstrate stronger interactions with coal molecules via ion exchange. (2) Both types of AAEMs are adsorbed via oxygen-containing functional groups (e.g., carbonyl, carboxyl, and phenolic hydroxyl) in the organic matrix. Quantum chemical calculations indicate that Na+ predominantly binds to carboxylate or carbonyl groups, forming carboxylate-Na complexes or coordination structures (−C=ONa+), whereas Ca2+ chemically adsorbs via robust ionic bonds. As vitrinite content increases, the ion-exchanged Na increased from 28.3% to 30.9%, and the ion-exchanged Ca increased from 62.3% to 70.1%, indicating that the vitrinite enhanced the affinity for AAEMs. (3) Groundwater flow drives AAEMs’ migration, with an adsorption preferentially occurring at oxygen functional groups. This adsorption capacity is controlled by macerals, establishing a macerals-functional groups-adsorption cascade as the fundamental mechanism for differential occurrence.
    Conclusions The organic occurrence of AAEMs (Na, Ca) has clear geological significance, thus providing an essential coal petrological basis for predicting vertical enrichment layers in coal seams. Besides, AAEMs may adversely affect the coalbed methane adsorption by occupying adsorption sites. Future research should prioritize elucidating molecular inhibition mechanisms of AAEMs in CBM competitive adsorption, providing theoretical foundations for the clean utilization of high-alkali coals.

     

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