CN114184665B - A method for monitoring radioactive water environment in coal-uranium resource overlapping areas - Google Patents
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- 229910052770 Uranium Inorganic materials 0.000 title claims abstract description 140
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Abstract
Description
技术领域Technical Field
本发明涉及水环境调查技术领域,特别是涉及一种煤铀资源叠置区放射性水环境监测方法。The invention relates to the technical field of water environment investigation, and in particular to a method for monitoring radioactive water environment in a coal-uranium resource superposition area.
背景技术Background Art
由于砂岩型铀矿与煤矿成矿环境的相似性,我国北方盆地内产出的铀矿层与煤层在空间上相互叠置,部分地区形成“上铀下煤”的空间地质格局。在煤矿开采的过程中,对上覆含水层的放水降压会改变地下水流场,形成区域地下水位降落漏斗。区域性降落漏斗的形成会改变砂岩铀矿层的地下水流场及铀的迁移条件,可能导致铀矿床范围内高铀浓度的地下水随着煤矿疏干排水进入地表水环境,造成放射性污染。Due to the similarity of the mineralization environment between sandstone uranium deposits and coal mines, the uranium deposits and coal seams produced in the northern basins of my country overlap with each other in space, forming a spatial geological pattern of "uranium above and coal below" in some areas. During coal mining, the release of water and pressure reduction of the overlying aquifer will change the groundwater flow field and form a regional groundwater level drop funnel. The formation of a regional drop funnel will change the groundwater flow field and uranium migration conditions in the sandstone uranium deposit layer, which may cause groundwater with high uranium concentration within the uranium deposit to enter the surface water environment along with the drainage of the coal mine, causing radioactive contamination.
现行的地下水环境监测方法多为围绕地下水常规指标的监测,针对放射性水环境的监测,依赖于实验室测定放射性指标,不能快速有效的确定矿产开发对水环境的影响,也无法系统分析污染产生的影响途径。The current groundwater environment monitoring methods are mostly centered around the monitoring of conventional groundwater indicators. The monitoring of radioactive water environments relies on laboratory measurements of radioactive indicators. These methods cannot quickly and effectively determine the impact of mineral development on the water environment, nor can they systematically analyze the impact pathways of pollution.
发明内容Summary of the invention
基于此,有必要针对现有煤铀资源叠置区放射性水环境监测方法不能快速有效的确定矿产开发对水环境的影响的问题,提供一种煤铀资源叠置区放射性水环境监测方法,所述方法通过系统建立煤铀资源叠置区水环境监测体系,利用水位观测、现场监测结合取样分析等手段,从含水层地下水流场及氧化还原条件的角度出发,及时发现煤铀资源叠置区铀矿含水层放射性水化学条件的变化,在污染可能发生的早期提出预警,适用于“上铀下煤”地层结构的资源叠置区水环境调查评价。Based on this, it is necessary to provide a method for monitoring the radioactive water environment in coal-uranium resource overlapping areas in order to address the problem that the existing radioactive water environment monitoring methods in coal-uranium resource overlapping areas cannot quickly and effectively determine the impact of mineral development on the water environment. The method systematically establishes a water environment monitoring system for coal-uranium resource overlapping areas, utilizes water level observation, on-site monitoring combined with sampling and analysis, and timely discovers changes in radioactive water chemical conditions in uranium aquifers in coal-uranium resource overlapping areas from the perspective of groundwater flow field and redox conditions in the aquifer, and issues early warnings when pollution may occur. The method is suitable for water environment investigation and evaluation in resource overlapping areas with a "uranium above and coal below" stratigraphic structure.
为了实现上述目的,本发明提供如下技术方案:In order to achieve the above object, the present invention provides the following technical solutions:
一种煤铀资源叠置区放射性水环境监测方法,包括如下步骤:A method for monitoring radioactive water environment in a coal-uranium resource overlapping area comprises the following steps:
步骤01、收集煤铀资源叠置区水文地质资料,了解煤铀资源叠置区的铀矿含水层和煤层分布规律,掌握煤铀资源叠置区内不同含水层水化学特征及水环境本底水平;Step 01: Collect hydrogeological data of the coal-uranium resource superposition area, understand the distribution patterns of uranium aquifers and coal seams in the coal-uranium resource superposition area, and master the hydrochemical characteristics and water environment background level of different aquifers in the coal-uranium resource superposition area;
步骤02、根据煤铀资源叠置区的水文地质条件和煤矿铀矿开采规划,布设能够及时反映煤铀资源叠置区内各含水层及地表水体水环境变化的地下水监测体系;Step 02: Based on the hydrogeological conditions of the coal-uranium resource superposition area and the coal and uranium mining plan, a groundwater monitoring system is deployed that can timely reflect the changes in the water environment of each aquifer and surface water body in the coal-uranium resource superposition area;
步骤03、根据煤铀资源叠置区内各含水层地下水补径排条件及动态变化特征,选择地下水长期监测频次,在长期监测频次的基础上,根据煤矿、铀矿开采规划,在煤矿大规模疏干排水或扩大开采规模时增加监测频次;Step 03: According to the groundwater recharge and drainage conditions and dynamic change characteristics of each aquifer in the coal-uranium resource superposition area, select the long-term groundwater monitoring frequency. On the basis of the long-term monitoring frequency, according to the coal and uranium mining plans, increase the monitoring frequency when the coal mine is drained on a large scale or the mining scale is expanded;
步骤04、通过地下水位监测,及时掌握煤铀资源叠置区不同含水层地下水流场变化,及时判断煤矿疏干排水对各含水层的影响。Step 04: Through groundwater level monitoring, timely grasp the changes in groundwater flow fields in different aquifers in the coal-uranium resource superposition area, and timely determine the impact of coal mine drainage on each aquifer.
进一步地,所述地下水监测体系包括:不同含水层的地下水水位观测点,地下水、地表水现场指标监测点,以及地下水、地表水检测样品采集点。Furthermore, the groundwater monitoring system includes: groundwater level observation points in different aquifers, groundwater and surface water on-site indicator monitoring points, and groundwater and surface water detection sample collection points.
进一步地,所述含水层的地下水水位观测点用于监测煤矿放水降压目的层,也就是铀矿含水层的地下水流场变化情况,所述含水层的地下水水位观测点布设在垂直地下水径流方向或自外围向地下水降落漏斗中心。Furthermore, the groundwater level observation points of the aquifer are used to monitor the changes in the groundwater flow field of the target layer for coal mine water release and pressure reduction, that is, the uranium mine aquifer. The groundwater level observation points of the aquifer are arranged in the direction vertical to the groundwater runoff or from the periphery to the center of the groundwater drop funnel.
进一步地,所述地下水、地表水现场指点监测点用于及时发现含水层水环境指标变化,从而对水环境变化做出预警;所述地下水现场指标监测点主要布设在铀矿床范围至煤矿开采区的地下水径流路径上,所述地表水现场指标监测点主要布设在煤矿排水口及排水口下游的地表水体。Furthermore, the groundwater and surface water on-site monitoring points are used to timely detect changes in aquifer water environment indicators, thereby issuing early warnings for water environment changes; the groundwater on-site indicator monitoring points are mainly arranged on the groundwater runoff path from the uranium deposit range to the coal mining area, and the surface water on-site indicator monitoring points are mainly arranged at the coal mine drainage outlet and the surface water bodies downstream of the drainage outlet.
进一步地,所述地下水、地表水检测样品采集点用于掌握水体化学组分含量,分析水环境变化趋势及原因;所述地下水、地表水检测样品采集点应能够反映各含水层水质变化,采样位置包含铀矿含水层、可能受影响的供水含水层、煤矿排水以及地表水。Furthermore, the groundwater and surface water sample collection points are used to grasp the content of chemical components in water bodies and analyze the trends and causes of water environment changes; the groundwater and surface water sample collection points should be able to reflect changes in water quality in each aquifer, and the sampling locations include uranium aquifers, potentially affected water supply aquifers, coal mine drainage and surface water.
进一步地,为了能够准确反映地下水环境放射性指标变化情况,所述地下水、地表水现场指标监测指标包括溶解氧、氧化还原电位、pH值和水中氡浓度;所述地下水、地表水检测样品采集分析项目包括一般水样简分析或全分析,以及水中铀含量。Furthermore, in order to accurately reflect the changes in groundwater environmental radioactive indicators, the groundwater and surface water on-site indicator monitoring indicators include dissolved oxygen, redox potential, pH value and radon concentration in water; the groundwater and surface water detection sample collection and analysis items include general water sample simple analysis or full analysis, and uranium content in water.
进一步地,在地下水、地表水现场指标监测的过程中,在发现铀矿含水层溶解氧或氧化还原电位升高的情况下,可能引起铀矿含水层水和煤矿排水的水中铀浓度升高,应提出预警并增加铀矿含水层现场监测及采样频次;若发现铀矿含水层溶解氧或氧化还原电位升高的同时,铀矿含水层及煤矿排水的水中氡浓度也升高,则反映了铀矿含水层中铀浓度升高并有向地下水降落漏斗迁移的趋势。Furthermore, in the process of on-site monitoring of groundwater and surface water indicators, if the dissolved oxygen or redox potential of the uranium aquifer is found to be elevated, it may cause an increase in the uranium concentration in the uranium aquifer water and the coal mine drainage water. In this case, an early warning should be issued and the on-site monitoring and sampling frequency of the uranium aquifer should be increased. If it is found that the dissolved oxygen or redox potential of the uranium aquifer is elevated while the radon concentration in the uranium aquifer and the coal mine drainage water is also elevated, it reflects that the uranium concentration in the uranium aquifer is elevated and has a tendency to migrate to the groundwater drop funnel.
本发明的煤铀资源叠置区放射性水环境监测方法适用于“上铀下煤”的煤铀资源叠置区。The radioactive water environment monitoring method of the coal-uranium resource superposition area of the present invention is applicable to the coal-uranium resource superposition area of "uranium above and coal below".
本发明的有益技术效果:Beneficial technical effects of the present invention:
本发明提供的煤铀资源叠置区放射性水环境监测方法,针对“上铀下煤”资源叠置区的特殊水文地质结构,利用氧化还原条件对铀在水中活化迁移的影响,有针对性地布设监测点位,系统地开展了水位监测、现场指标监测以及取样测试,能够在放射性污染早期及时发现煤矿疏干排水层氧化还原条件的变化以及含水层铀浓度的升高现象,为煤铀资源叠置区水环境变化发出预警。The radioactive water environment monitoring method for coal-uranium resource overlapping areas provided by the present invention targets the special hydrogeological structure of the "upper uranium and lower coal" resource overlapping areas, utilizes the influence of redox conditions on the activation and migration of uranium in water, arranges monitoring points in a targeted manner, and systematically carries out water level monitoring, on-site indicator monitoring and sampling testing. It can timely discover changes in the redox conditions of the coal mine drainage layer and the increase in uranium concentration in the aquifer at the early stage of radioactive contamination, and issue early warnings for changes in the water environment in coal-uranium resource overlapping areas.
附图说明BRIEF DESCRIPTION OF THE DRAWINGS
图1为本发明提供的煤铀资源叠置区放射性水环境监测方法的流程图。FIG1 is a flow chart of a method for monitoring radioactive water environment in a coal-uranium resource overlapping area provided by the present invention.
具体实施方式DETAILED DESCRIPTION
砂岩型铀矿床产出于偏还原条件的地下水环境中,而偏氧化的地下水环境有利于铀在水中的活化迁移,因此,利用铀的这一水文地球化学特性,设计相应的监测方法,可以通过含水层氧化还原条件的变化判断地下水中铀的活化迁移,也就是放射性转移的情况。同时,考虑铀衰变链中氡的特性可以进一步判断含水层中铀的活化迁移情况。Sandstone-type uranium deposits are produced in groundwater environments with partial reduction conditions, while partial oxidation groundwater environments are conducive to the activation and migration of uranium in water. Therefore, by using this hydrogeochemical characteristic of uranium and designing corresponding monitoring methods, the activation and migration of uranium in groundwater, that is, the situation of radioactive transfer, can be determined through the changes in the redox conditions of the aquifer. At the same time, considering the characteristics of radon in the uranium decay chain can further determine the activation and migration of uranium in the aquifer.
参见图1,为了系统地、有效地对煤铀资源叠置区实施水环境监测,本发明提供一种煤铀资源叠置区放射性水环境监测方法,包括如下步骤:Referring to FIG1 , in order to systematically and effectively implement water environment monitoring in coal-uranium resource overlapping areas, the present invention provides a method for monitoring radioactive water environment in coal-uranium resource overlapping areas, comprising the following steps:
步骤01、前期资料收集与分析:收集煤铀资源叠置区的水文地质,了解煤铀资源叠置区的铀矿含水层和煤层分布规律,掌握煤铀资源叠置区内不同含水层水化学特征及水环境本底水平。Step 01. Preliminary data collection and analysis: Collect hydrogeological data of the coal-uranium resource superposition area, understand the distribution patterns of uranium aquifers and coal seams in the coal-uranium resource superposition area, and master the hydrochemical characteristics and water environment background levels of different aquifers in the coal-uranium resource superposition area.
步骤02、建立水环境监测体系:根据煤铀资源叠置区的水文地质条件和煤矿铀矿开采规划,布设能够及时反映煤铀资源叠置区内各含水层及地表水体水环境变化的地下水监测体系。Step 02, establish a water environment monitoring system: according to the hydrogeological conditions of the coal-uranium resource overlapping area and the coal mine uranium mining plan, set up a groundwater monitoring system that can timely reflect the changes in the water environment of each aquifer and surface water body in the coal-uranium resource overlapping area.
步骤03、确定监测指标:根据煤铀资源叠置区内各含水层地下水补径排条件及动态变化特征,选择地下水长期监测频次,在长期监测频次的基础上,根据煤矿铀矿开采规划,在煤矿大规模疏干排水或扩大开采规模时增加监测频次。Step 03, determine the monitoring indicators: According to the groundwater recharge and drainage conditions and dynamic change characteristics of each aquifer in the coal-uranium resource superposition area, select the long-term groundwater monitoring frequency. On the basis of the long-term monitoring frequency, according to the coal mine uranium mining plan, increase the monitoring frequency when the coal mine is drained on a large scale or the mining scale is expanded.
步骤04、监测与评价:通过地下水位监测,及时掌握煤铀资源叠置区不同含水层地下水流场变化,及时判断煤矿疏干排水对各含水层的影响。Step 04, Monitoring and Evaluation: Through groundwater level monitoring, timely grasp the changes in groundwater flow fields in different aquifers in the coal-uranium resource superposition area, and timely determine the impact of coal mine drainage on each aquifer.
所述地下水监测体系包括:不同含水层的地下水水位观测点,地下水、地表水现场指标监测点,以及地下水、地表水检测样品采集点。The groundwater monitoring system includes: groundwater level observation points in different aquifers, groundwater and surface water on-site indicator monitoring points, and groundwater and surface water detection sample collection points.
所述含水层的地下水水位观测点用于监测煤矿放水降压目的层,也就是铀矿含水层的地下水流场变化情况,所述含水层的地下水水位观测点布设在垂直地下水径流方向或自外围向地下水降落漏斗中心。The groundwater level observation points of the aquifer are used to monitor the changes in the groundwater flow field of the target layer for coal mine water release and pressure reduction, that is, the uranium mine aquifer. The groundwater level observation points of the aquifer are arranged in the direction vertical to the groundwater runoff or from the periphery to the center of the groundwater drop funnel.
所述地下水、地表水现场指点监测点用于及时发现含水层水环境指标变化,从而对水环境变化做出预警;所述地下水现场指标监测点主要布设在铀矿床范围至煤矿开采区的地下水径流路径上,所述地表水现场指标监测点主要布设在煤矿排水口及排水口下游的地表水体。The groundwater and surface water on-site monitoring points are used to timely detect changes in aquifer water environment indicators, thereby issuing early warnings for water environment changes; the groundwater on-site indicator monitoring points are mainly arranged on the groundwater runoff path from the uranium deposit range to the coal mining area, and the surface water on-site indicator monitoring points are mainly arranged at the coal mine drainage outlet and the surface water bodies downstream of the drainage outlet.
所述地下水、地表水检测样品采集点用于掌握水体化学组分含量,分析水环境变化趋势及原因;所述地下水、地表水检测样品采集点应能够反映各含水层水质变化,采样位置包含铀矿含水层、可能受影响的供水含水层、煤矿排水以及地表水。The groundwater and surface water sample collection points are used to grasp the content of chemical components in water bodies and analyze the trends and causes of water environment changes; the groundwater and surface water sample collection points should be able to reflect changes in water quality in each aquifer, and the sampling locations include uranium aquifers, potentially affected water supply aquifers, coal mine drainage and surface water.
为了能够准确反映地下水环境放射性指标变化情况,所述地下水、地表水现场指标监测指标包括溶解氧、氧化还原电位、pH值和水中氡浓度;所述地下水、地表水检测样品采集分析项目包括一般水样简分析或全分析,以及水中铀含量。In order to accurately reflect the changes in groundwater environmental radioactive indicators, the groundwater and surface water on-site monitoring indicators include dissolved oxygen, redox potential, pH value and radon concentration in water; the groundwater and surface water detection sample collection and analysis items include general water sample simple analysis or full analysis, and uranium content in water.
在地下水、地表水现场指标监测的过程中,在发现铀矿含水层溶解氧或氧化还原电位升高的情况下,可能引起铀矿含水层水和煤矿排水的水中铀浓度升高,应提出预警并增加铀矿含水层现场监测及采样频次;若发现铀矿含水层溶解氧或氧化还原电位升高的同时,铀矿含水层及煤矿排水的水中氡浓度也升高,则反映了铀矿含水层中铀浓度升高并有向地下水降落漏斗迁移的趋势。During the on-site monitoring of groundwater and surface water indicators, if the dissolved oxygen or redox potential of the uranium aquifer is found to be elevated, it may cause an increase in the uranium concentration in the uranium aquifer water and the coal mine drainage water. In this case, an early warning should be issued and the on-site monitoring and sampling frequency of the uranium aquifer should be increased. If it is found that the dissolved oxygen or redox potential of the uranium aquifer is elevated while the radon concentration in the uranium aquifer and the coal mine drainage water is also elevated, it reflects that the uranium concentration in the uranium aquifer is elevated and has a tendency to migrate to the groundwater drop funnel.
本发明的煤铀资源叠置区放射性水环境监测方法适用于“上铀下煤”的煤铀资源叠置区。The radioactive water environment monitoring method of the coal-uranium resource superposition area of the present invention is applicable to the coal-uranium resource superposition area of "uranium above and coal below".
下面结合附图和实施例对本发明作进一步详细地描述。The present invention will be further described in detail below with reference to the accompanying drawings and embodiments.
实施例1Example 1
以我国北方某鄂尔多斯盆东北部皂火壕地区为例,在该地区分布的铀矿床与矿床西部王家塔煤矿开采范围叠置,叠置面积约20km2,约占铀矿床面积80%以上。在该煤铀资源叠置区以西,为鄂尔多斯市东胜区供水水源地,而煤矿疏干排水口位于水源地流域范围。由于铀矿所处的含水层覆盖在煤层之上,成为煤矿放水降压的目的层,随着煤矿开采范围的扩大,当疏干排水的影响范围扩大至铀矿体时,很有可能导致含水层铀活化迁移,并随着疏干排水排出地表,造成放射性污染。Taking the Zaohuohao area in the northeast of the Ordos Basin in northern China as an example, the uranium deposits distributed in this area overlap with the mining area of the Wangjiata coal mine in the west of the deposit, with an overlapping area of about 20km2 , accounting for more than 80% of the uranium deposit area. To the west of the coal-uranium resource overlapping area is the water source for Dongsheng District, Ordos City, and the drainage outlet of the coal mine is located in the water source basin. Since the aquifer where the uranium mine is located covers the coal seam, it has become the target layer for water release and pressure reduction in the coal mine. With the expansion of the coal mining area, when the influence of drainage is expanded to the uranium ore body, it is very likely to cause the activation and migration of uranium in the aquifer, and discharge it to the surface with drainage, causing radioactive pollution.
针对上述情况,使用本发明的煤铀资源叠置区放射性水环境监测方法对该煤铀资源叠置区进行水环境放射性监测,包括如下步骤:In view of the above situation, the radioactive water environment monitoring method of the coal-uranium resource overlapping area of the present invention is used to monitor the radioactivity of the water environment in the coal-uranium resource overlapping area, comprising the following steps:
1、收集该煤铀资源叠置区的水文地质和水环境资料,根据收集的该煤铀资源叠置区的水文地质和水环境资料可知,该煤铀资源叠置区的主要含水层为:第四系潜水含水层、白垩系碎屑岩潜水-承压水含水层、中侏罗统直罗组含水层。其中,第四系潜水含水层为水源地供水层位,中侏罗统直罗组含水层为铀矿储层也是煤矿放水降压层位。煤矿开采范围位于铀矿床以西,暂未进入铀矿床范围内。1. Collect the hydrogeological and water environment data of the coal-uranium resource superposition area. According to the collected hydrogeological and water environment data of the coal-uranium resource superposition area, the main aquifers in the coal-uranium resource superposition area are: Quaternary phreatic aquifer, Cretaceous clastic rock phreatic-confined water aquifer, and Middle Jurassic Zhiluo Formation aquifer. Among them, the Quaternary phreatic aquifer is the water source water supply layer, and the Middle Jurassic Zhiluo Formation aquifer is the uranium reservoir and also the coal mine water release and pressure reduction layer. The coal mining area is located to the west of the uranium deposit and has not yet entered the uranium deposit area.
2、根据监测区含水层分布以及煤矿疏干排水条件,分析可知,监测区放射性污染产生的途径主要为煤矿疏干排水将铀矿含水层地下水排出地表,进而产生放射性污染。因此,以铀矿含水层、煤矿排水口以及排水口区域为重点,布设监测点。针对直罗组铀矿含水层,在铀矿床范围内沿地下水径流方向自东向西布设了8个直罗组含水层监测孔;在煤矿排水口,自排水口至下游进入水源地布设3个地表水监测点以及2个第四系含水层监测点;同时,在铀矿床范围内布设两个白垩系含水层监测点。2. According to the distribution of aquifers in the monitoring area and the conditions of coal mine drainage, it can be analyzed that the main way of radioactive contamination in the monitoring area is that the coal mine drainage discharges the groundwater of the uranium aquifer to the surface, thereby causing radioactive contamination. Therefore, monitoring points are set up with a focus on the uranium aquifer, coal mine drainage outlets and drainage outlet areas. For the Zhiluo Formation uranium aquifer, 8 Zhiluo Formation aquifer monitoring holes are set up from east to west along the groundwater runoff direction within the uranium deposit; at the coal mine drainage outlet, 3 surface water monitoring points and 2 Quaternary aquifer monitoring points are set up from the drainage outlet to the downstream water source; at the same time, two Cretaceous aquifer monitoring points are set up within the uranium deposit.
3、水环境监测工作开始于2016年8月,监测初期,煤矿开采形成的地下水位降落漏斗边界位于铀矿床西北,略进入铀矿床边界。铀矿含水层Eh、溶解氧均表现出还原环境,在此条件下,矿层中U元素难以溶解迁移,水中铀含量2.6μg~64μg,水中氡浓度均小于40Bq/L,放射性指标基本与潜水一致。3. Water environment monitoring work began in August 2016. At the beginning of the monitoring, the boundary of the groundwater level drop funnel formed by coal mining was located in the northwest of the uranium deposit, slightly entering the boundary of the uranium deposit. The Eh and dissolved oxygen of the uranium aquifer showed a reducing environment. Under this condition, the U element in the ore layer was difficult to dissolve and migrate. The uranium content in the water was 2.6μg~64μg, and the radon concentration in the water was less than 40Bq/L. The radioactive indicators were basically consistent with diving.
煤矿排水水中铀含量为0.37μg/L,排出的地下水为高矿化度的Cl·HCO3-Na型水。排水口下游的第四系潜水表现出矿化度、Cl-含量升高。The uranium content in the coal mine drainage water is 0.37μg/L, and the discharged groundwater is highly mineralized Cl·HCO3-Na type water. The Quaternary groundwater downstream of the drainage outlet shows increased mineralization and Cl- content.
4、至2017年初,该煤矿在铀矿床南段扩大开采,监测组增加了地下水位与现场指标监测频次。通过水环境监测发现,自2017年3月煤矿扩大开采至2017年10月,由于疏干排水形成的降落漏斗影响范围扩大至铀矿床中部,且漏斗中心已转移至铀矿床西部。4. By the beginning of 2017, the coal mine expanded mining in the southern part of the uranium deposit, and the monitoring team increased the frequency of groundwater level and on-site indicator monitoring. Through water environment monitoring, it was found that from March 2017, when the coal mine expanded mining, to October 2017, the impact range of the drop funnel formed by drainage expanded to the middle of the uranium deposit, and the center of the funnel has moved to the west of the uranium deposit.
随着铀矿含水层地下水位的下降,矿床中段、东部含水层Eh达到86mV~332mV,表现出氧化环境,水中氡浓度达到26.61Bq/L~989.38Bq/L。通过现场监测指标判断,由于含水层地下水位下降,导致了矿体中的铀活化迁移大量溶解于地下水中,而采样分析数据也说明了这一论证,矿床东段水中铀浓度达到了1061μg/L。As the groundwater level of the uranium aquifer drops, the Eh of the aquifer in the middle and eastern parts of the deposit reaches 86mV~332mV, showing an oxidizing environment, and the radon concentration in the water reaches 26.61Bq/L~989.38Bq/L. Judging from the on-site monitoring indicators, the decline in the groundwater level of the aquifer has led to the activation and migration of uranium in the ore body and its dissolution in the groundwater. The sampling and analysis data also illustrate this argument. The uranium concentration in the water in the eastern part of the deposit has reached 1061μg/L.
煤矿排水口排出的地下水水中铀含量为0.28μg/L,水中氡浓度为13Bq/L,未发生太大变化。这是由于含水层氧化带由东向西推移,暂未到达矿床西部。随着疏干排水的持续进行,氧化带推移至矿床西部放水降压区,高铀浓度的放射性水将会随着煤矿疏干排水排出地表。The uranium content of groundwater discharged from the coal mine drainage outlet is 0.28μg/L, and the radon concentration in the water is 13Bq/L, which has not changed much. This is because the oxidation zone of the aquifer has moved from east to west and has not yet reached the west of the deposit. As drainage continues, the oxidation zone will move to the water release and pressure reduction area in the west of the deposit, and radioactive water with high uranium concentration will be discharged to the surface along with the drainage of the coal mine.
以上所述实施例仅表达了本发明的几种实施方式,其描述较为具体和详细,但并不能因此而理解为对本发明专利范围的限制。应当指出的是,对于本领域的普通技术人员来说,在不脱离本发明构思的前提下,还可以做出若干变形和改进,这些都属于本发明的保护范围。因此,本发明专利的保护范围应以所附权利要求为准。The above-mentioned embodiments only express several implementation methods of the present invention, and the description thereof is relatively specific and detailed, but it cannot be understood as limiting the scope of the patent of the present invention. It should be pointed out that, for ordinary technicians in this field, several variations and improvements can be made without departing from the concept of the present invention, which all belong to the protection scope of the present invention. Therefore, the protection scope of the patent of the present invention shall be subject to the attached claims.
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