地面核磁共振技术在隐伏火烧区富水性探测中的应用  

Application of surface nuclear magnetic resonance technology in detecting water abundance in concealed burnt zone

作　　者：侯恩科[1] 樊江伟 高利军 王建文 陈德海 迟宝锁 王宏科 HOU Enke;FAN Jiangwei;GAO Lijun;WANG Jianwen;CHEN Dehai;CHI Baosuo;WANG Hongke(College of Geology and Environment,Xi’an University of Science and Technology,Xi’an 710054,China;Shenmu Ningtiaota Coal Mining Company Ltd.,Shaanxi Coal and Chemical Industry Company Ltd.,Yulin 719300,China;Shenfeng Institute of Geological New Technique Application of Shanghai,Shanghai 201702,China;Northern Shaanxi Mining Co.,Ltd.,Yulin 719000,China)

机构地区：[1]西安科技大学地质与环境学院,陕西西安710054 [2]陕煤集团神木柠条塔矿业有限公司,陕西榆林719300 [3]上海申丰地质新技术应用研究所有限公司,上海201702 [4]陕西陕煤陕北矿业有限公司,陕西榆林719000

出　　处：《煤田地质与勘探》2021年第5期230-237,共8页Coal Geology & Exploration

基　　金：国家自然科学基金项目(41472234);陕西煤业化工集团科研计划项目(2017SMHKJ-C-23)。

摘　　要：煤层隐伏火烧区上覆基岩复合含水层(包括风化基岩和烧变岩含水层)是煤层开采的主要威胁之一,明确隐伏火烧区的富水性对矿井水害防治具有重要意义。基于此,以发生过较大突水事故的柠条塔煤矿为研究对象,利用地面核磁共振(SNMR)技术开展隐伏火烧区含水层富水性探测并对其进行分析和验证。结果表明,隐伏火烧区共有2个含水层位,分别为第四系松散砂层含水层和1-2上煤上覆基岩含水层;第四系砂层含水层富水性受地表地形及其下隔水层顶部起伏形态影响水平变化较大;1-2上煤上覆基岩含水层富水性总体西南较低、北东较高,该含水层厚度9~30m,局部相对较厚,推测为1-2上煤火烧区风化基岩和烧变岩含水层的叠加反映;研究区内1-2上煤上覆基岩含水层总体呈现出西部及中部偏东南区域富水性相对较大,其余区域富水性相对较小。利用SNMR得到的含水层富水程度与探放水孔及水文孔的涌水量结果大致相同,表明该方法的勘探结果相对可靠,可用于隐伏火烧区富水性的探测。The overlying bedrock composite aquifer(including weathered bedrock and burnt rock aquifer) in the concealed burnt zone of coal seams is one of the main threats to coal mining. It is of great significance to clarify the water enrichment of the concealed burnt zone for the prevention and control of coal mine water hazards. Ningtiaota Coal Mine, which has experienced a large water inrush accident, was used as the research object, and the Surface Nuclear Magnetic Resonance(SNMR) was used to detect the water enrichment of the aquifer in the concealed burnt area. The results show that there are two aquifers in the concealed burnt zone, namely Quaternary loose sand aquifer and 1-2 coal overlying bedrock aquifer. The water enrichment of the Quaternary sand aquifer is affected by the topography of the surface and the top undulating shape of the lower aquifer, and the level changes greatly. The water content of the bedrock aquifer overlying 1-2 coal is generally lower in the southwest and higher in the northeast.The thickness of the aquifer is 9-30 m, relatively thicker parts, which is presumed to be the superimposed reflection of weathered bedrock and burnt rock aquifer in the burnt area. In the study area, the overlying bedrock aquifer of 1-2 coal generally shows relatively larger water quantity in the western and central southeast regions and relatively weaker water abundance. The conclusions obtained by using SNMR are roughly the same as the results of water inflows from water detection holes and hydrological holes, which indicates that the exploration results of this method are relatively reliable and can be used for the detection of water enrichment in hidden burnt areas.

关 键 词：地面核磁共振 隐伏火烧区 含水层 富水性 

分 类 号：P641.7[天文地球—地质矿产勘探]