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现代隧道技术 2025, Vol. 62 Issue (5) :216-    DOI:
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富水弱胶结砂岩未冻水赋存状态演化规律试验研究#br#
(1.安徽理工大学土木建筑学院,淮南 232001;2.中国科学院西北生态资源环境研究院,兰州 730000;
3.安徽理工大学 深部煤炭安全开采与环境保护全国重点实验室,淮南 232001;
4.中国十七冶集团有限公司,马鞍山 243000)
Experimental Study on the Evolution Mechanism of Unfrozen Water #br# Distribution in Water-rich Weakly Cemented Sandstone
(1. School of Civil Engineering and Architecture, Anhui University of Science and Technology, Huainan 232001;
2. Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou 730000;
3. State Key Laboratory for Safe Mining of Deep Coal Resources and Environment Protection, Anhui University of Science and
Technology, Huainan 232001; 4. China MCC17 Group Co., Ltd., Ma′anshan 243000)
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摘要 随着我国煤炭资源开发西移,富水弱胶结砂岩地层已成为深部煤炭开采面临的重大挑战。然而,针对此类低强度、遇水易软化岩体在深部多场耦合环境中的未冻水动态响应机制,尚缺乏系统研究。文章以鄂尔多斯市苏布尔嘎矿区砂岩为研究对象,系统开展孔隙结构演变、未冻水赋存规律以及核磁成像等研究。结果表明:(1)三类砂岩中的孔隙水在冻结阶段均遵循“自由水—毛细水—吸附水”的冻结顺序;在升温阶段遵循“吸附水—毛细水—自由水”的解冻规律。(2)核磁共振成像显示,细粒砂岩的孔隙水主要富集于左端,冻结过程未出现过冷现象,最终未冻水含量为3.08%;细砾岩与粉砂岩的孔隙水分别呈居中和相对均匀分布,二者均存在过冷阶段(冻结温度为-1.5~-2 ℃),最终未冻水含量分别为6.69%和3.37%;岩石内部微小孔隙占比与冰点呈负相关关系。(3)冻融循环作用促使小、中孔喉数量增加,大孔喉数量减少,加剧了岩体结构劣化。
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张子浩1
3 王 彬1
2
3
4 黄金坤4 荣传新1
3 梁秀玲1
3
关键词核磁共振   未冻水含量   孔隙结构   成像分析   弱胶结砂岩     
Abstract: With the westward shift of coal resource exploitation in China, water-rich and weakly cemented sandstone strata have emerged as a major geotechnical challenge in deep coal mining. However, systematic investigations remain scarce regarding the dynamic response mechanisms of unfrozen water in such low-strength, water-sensitive rock under deep multi-field coupling conditions. In this study, sandstone samples collected from the Suboergai mining area in the Ordos Basin were examined to elucidate pore structure evolution, unfrozen water distribution behavior, and nuclear magnetic imaging characteristics. The results indicate that: (1) During the freezing stage, pore water in all three sandstone types solidifies sequentially as “free water → capillary water → adsorption water”, whereas thawing follows the reverse order “adsorption water → capillary water → free water”. (2) Nuclear magnetic resonance imaging reveals that pore water in fine-grained sandstone is mainly enriched in the lower-T? region, with no supercooling effect observed, and the final unfrozen water content reaches 3.08%. Pore water in fine-gravel sandstone and siltstone exhibits a central-dominant and a relatively uniform distribution, respectively, both experiencing supercooling (freezing temperature −1.5 to −2 °C), with final unfrozen water contents of 6.69% and 3.37%. The proportion of micro-pores inside the rock is negatively correlated with the freezing point temperature. (3) Freeze-thaw cycling promotes an increase in small- and medium-sized pore throats while reducing large pore throats, thereby accelerating structural deterioration of the rock mass.
KeywordsNuclear magnetic resonance,   Unfrozen water content,   Pore structure,   Image analysis,   Weakly cemented sandstone     
基金资助:安徽省自然科学基金(2408085ME147);国家自然科学基金(52378384,52409135) .
作者简介: 张子浩(1999-),男,硕士研究生,主要从事人工地层冻结相关的研究工作,E-mail: 17356035727@163.com.
引用本文:   
张子浩1, 3 王 彬1, 2等 .富水弱胶结砂岩未冻水赋存状态演化规律试验研究#br#[J]  现代隧道技术, 2025,V62(5): 216-
ZHANG Zihao1, 3 WANG Bin1, 2 etc .Experimental Study on the Evolution Mechanism of Unfrozen Water #br# Distribution in Water-rich Weakly Cemented Sandstone[J]  MODERN TUNNELLING TECHNOLOGY, 2025,V62(5): 216-
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