岩溶作用过程试验方法研究

方雨; 蒋忠诚; 张卫; 章程

doi:10.11932/karst20230103

岩溶作用过程试验方法研究——以岩溶作用仪研制为例

doi: 10.11932/karst20230103

方雨^1,,
蒋忠诚^2, ,,
张卫¹,
章程²

1.
中国地质大学(武汉), 湖北武汉 430074
2.
中国地质科学院岩溶地质研究所/自然资源部、广西岩溶动力学重点实验室, 广西桂林 541004

详细信息

作者简介:
方雨（1997－），女，硕士研究生，主要从事岩溶地质研究。E-mail：824874595@qq.com

通讯作者:
蒋忠诚（1962－），男，博士，研究员，主要从事岩溶地质研究。E-mail：jzhongcheng@mail.cgs.gov.cn

中图分类号: P642.25
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出版历程
- 收稿日期: 2022-04-21
- 刊出日期: 2023-02-25

Study on test method of karstification process: Take the development of karstification instrument as an example

1.
China University of Geosciences, Wuhan, Hubei 430074, China
2.
Institute of Karst Geology, CAGS/Key Laboratory of Karst Dynamics, MNR & GZAR, Guilin, Guangxi 541004, China

摘要

摘要: 通过对前人试验装置的分析，以岩溶作用原理及其影响因素为基础，结合仪器使用单位的试验需求，研制岩溶作用仪。通过分析不同的CO₂起源、岩溶发育深度、不同pH条件以及地下水循环深度的地质环境条件，提出了仪器的基本功能和适用条件，进行岩溶作用仪功能模块的论证设计和研制，并进行了验证性试验，且达到预期目标。得到如下成果：提出了四种岩溶作用模式，研制了五个岩溶作用功能模块，总结分析了功能模块与岩溶作用内在关系以及功能模块组合原则，提供不同地质环境条件下的岩溶作用试验。仪器可以实现：模拟地下水循环深度0~200 m，环境温度0~70 ℃，CO₂起源：表生、内生起源Pco₂=0.0~2.0 MPa，不同酸度背景条件：pH可控，不同水流速度条件下的沉积作用可控，岩溶裂隙张开度的沉积作用（可组合）。
- 岩溶作用仪 /
- 岩溶作用过程模拟 /
- 溶液制备装置 /
- 岩溶沉积器 /
- 地质环境背景
Abstract: In recent years, with the construction of national economy and the need to achieve the "double carbon goal", a large number of increasingly complex problems on karst science have been encountered, which need to be solved by simulating the process of karst action in different geological environment conditions. In the past, karst simulation was mainly carried out under normal temperature, normal pressure and certain pH conditions to determine the basic characteristics of karst and parameters such as the rate of karst, which could not effectively simulate karst under different geological conditions. Therefore, a comprehensive set of instruments for simulating karst action under different geological environmental conditions (e.g., ambient temperature of 0-70 ℃, subsurface depth of 200 m, different CO₂ origins and different saturation levels, etc.) is needed to solve a series of scientific problems such as karst dissolution and sedimentation in different geological environmental contexts. Based on the principle of karstification, this paper defines the functions and parameters of the instrument by analyzing the geological environment conditions of different CO₂ origins, karst development depths, different pH conditions and groundwater circulation depths. Based on the requirement of the karstification instrument, the parameters and modules of karstification instrument have been designed according to the instrument functions, karstification control factors and karstification principle. After the design of each part and the overall development of the instrument were completed, a verification test was carried out to illustrate the feasibility of the instrument. Finally, the following results are obtained. (1) Four karstification models are proposed, i.e., the origin of CO₂in the supergene zone—the shallow circulation karstification model of groundwater; CO₂ origin of supergene zone—cyclic karstification model of groundwater depth; the origin of CO₂ in the deep—the model of karst process of groundwater depth circulation; and the mode of groundwater circulation karstification under the biological action of supergene zone (such as the change of pH value of humic acid). (2) According to the basic principle of karstification and the four models of karstification, five karstification function modules are developed, CO₂ (pH) solution function module of different geological environment origins, water circulation depth module, environmental background temperature module, dissolution module and sedimentation module. (3) The internal relationship between functional modules and karstification together with the combination principle of functional modules has been summarized and analyzed to provide karstification tests under different geological environment conditions. Finally, according to the principle of karstification, taking the computer as the basic control unit, the test parameters of different functional modules have been monitored by sensors and controlled by PLC, and the functional modules have been organically connected and controlled to meet the requirement of fully automatic karstification tests under different geological environment conditions.Basic parameters of karstification instrument are listed as follows: (1) simulated groundwater circulation depth of 0-200 m; (2) ambient background temperature of 0-70 ℃; (3) CO₂ origins—supergene origin Pco₂=0.0 MPa and endogenous origin Pco₂=0.0-2.0 MPa; (4) different acidity background conditions—pH value is controllable; (5) sedimentation that can be controlled under different flow velocities; (6) sedimentation of the opening degree of karst fissures (can be combined).However, due to the limitations of time and cost, the instrument can be further improved. For example, in order to improve the preparation efficiency of saturated CO₂ solution, the contact area between CO₂ and water can be increased. A dual solution preparation system can be designed to prepare the solution so that the efficiency of the test can be increased. The maximum safe pressure of this instrument is 2 MPa (water circulation depth of 200 m). If a simulation of a greater water circulation depth is needed, the thickness of stainless-steel materials for solution preparation, dissolution reaction kettle and deposition reactor (meeting the requirements of high-pressure vessel specifications) can be increased, and a pressure pump with a larger pressure rise will be used.
- karstification instrument /
- simulation of karstification process /
- solution preparation device /
- karst sedimentary apparatus /
- geological environment background

HTML

图 1 岩溶作用过程

Figure 1. Karstification process

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图 2 岩溶发育深度分区图

Figure 2. Zoning map of karst development depth

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图 3 pH与溶解无机碳组分的关系^[33]

Figure 3. Relationship between pH value and dissolved inorganic carbon components

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图 4 CO₂溶解量、溶液pH与温度变化关系^[34]

Figure 4. Relationship between dissolved CO₂, pH and temperature

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图 5 CO₂溶解量、溶液pH与Pco₂变化关系图^[34]

Figure 5. Relationship between dissolved CO₂, pH and Pco₂

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图 6 裂隙表面，实际（左）、假设（右）

Figure 6. Fracture surface, actual (left), assumed (right)

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图 7 岩溶作用仪示意图

Figure 7. Schematic diagram of karstification apparatus

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图 8 仪器运行流程图

注：K1-K5为电磁阀开关；W1-W3为水位传感器。

Figure 8. Instrument operation flow chart

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图 9 岩溶作用仪实物图

注：现已安装于桂林国际岩溶中心试验场。

Figure 9. Physical drawing of karstification apparatus

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图 10 水溶液制备系统原理图

Figure 10. Schematic of preparation of saturated CO₂ solution

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图 11 溶液\溶蚀反应釜、传感器示意图

1.进水口 2.出水口 3.进气口 4.传感器

Figure 11. Solution/dissolution reaction kettle and sensor diagram

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图 12 溶蚀作用系统原理图

Figure 12. Schematic diagram of dissolution system

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图 13 岩溶沉积器剖面示意图、平面示意图

Figure 13. Karst sedimentator profile diagram and plane diagram

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图 14 岩溶沉积装置原理示意图

Figure 14. Schematic diagram of karst deposition device

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图 15 控制流程图

Figure 15. Control flow chart

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图 16 岩溶作用仪控制柜实物图

Figure 16. Physical drawing of karstification instrument control cabinet

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图 17 岩溶作用仪控制面板

Figure 17. Karstification instrument control panel

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图 18 溶蚀速率随压力变化关系图

Figure 18. Relationship between corrosion rate and pressure

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表 1 仪器模块组成分析

Table 1. Apparatus development theory and process analysis

参与反应的物质	反应场所/实现方法
碳酸盐岩	溶蚀场所	不同地质环境背景岩溶溶蚀作用模拟系统	溶蚀反应釜
碳酸盐岩	沉积场所	不同地质环境背景岩溶沉积模拟系统	岩溶沉积器
CO₂	饱和CO₂溶液制备场所	不同成因CO₂或pH水溶液制备系统	溶液反应釜
水	饱和CO₂溶液制备场所
酸（H⁺）	不同pH值溶液制备场所
压力	加压装置
温度	温度控制装置

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表 2 传感器设置

Table 2. Sensor settings

监测目标	监测设备
温度	温度传感器
压力	压力传感器
水位	水位传感器（最高水位W1、最低水位W2、水位监测W3）

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