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绥阳双河洞国家地质公园边界优化
引用本文:周文龙,BOTTAZZI Jean,况光显,王德远,罗书文,高占冬,江波,莫贵芬.绥阳双河洞国家地质公园边界优化[J].科学技术与工程,2023,23(27):11540-11549.
作者姓名:周文龙  BOTTAZZI Jean  况光显  王德远  罗书文  高占冬  江波  莫贵芬
作者单位:贵州省山地资源研究所,中国地质学会洞穴专业委员会;French Federation of Speleology;绥阳双河洞国家地质公园管理处
基金项目:贵州省科学技术基金(黔科合基础 [2018]1149、[2017]1172);国家自然科学基金项目后补助“贵州科学院2021年度学术新苗培养及自由探索创新”专项;贵州科学院省级科研专项资金(黔科院科专合字 [2022]03号)。
摘    要:双河洞是世界上最长的白云岩洞系,它构成了绥阳双河洞国家地质公园的主体。随着探测长度的持续增长,现行园区边界已不能满足保护与管理的需求。以双河洞空间分布为参考,运用ArcGIS水文与空间分析工具对池武溪流域及周边数字高程模型(digital elevation model, DEM)数据进行数字河网提取、地表流域分割,并综合考虑自然与人文因素,得到如下认识:(1)园区1∶5万DEM精度下设定1 000 m2的汇流累积量阈值模拟出的数字水系与真实水系一致性高;(2)双河洞系统跨越池武溪地表分水岭,直观反映了地表-地下分水岭不重合的现象;(3)双河洞系统自2018年就已超越现行地质公园边界以及县级行政区界线,核心地质遗迹保护与管理存在真空地带,园区边界优化调整迫在眉睫;(4)园区边界应结合双河洞系统发育界限预判为考量适时进行动态调整,并提出了初步的优化定界方案;(5)未来应加强双河洞区域的示踪试验,更加明确地下分水岭范围,以更加科学、完整地划定园区边界。

关 键 词:双河洞国家地质公园  双河溶洞群  数字高程模型(DEM)  水文分析  边界优化
收稿时间:2022/12/1 0:00:00
修稿时间:2023/9/12 0:00:00

Optimization the Boundary of Shuanghe Cave National Geopark in Suiyang County
Zhou Wenlong,BOTTAZZI Jean,Kuang Guangxian,Wang Deyuan,Luo Shuwen,Gao Zhandong,Jiang Bo,Mo Guifen.Optimization the Boundary of Shuanghe Cave National Geopark in Suiyang County[J].Science Technology and Engineering,2023,23(27):11540-11549.
Authors:Zhou Wenlong  BOTTAZZI Jean  Kuang Guangxian  Wang Deyuan  Luo Shuwen  Gao Zhandong  Jiang Bo  Mo Guifen
Institution:Guizhou Institute of Mountain Resources
Abstract:Shuanghe Cave is the longest dolomite cave system in the world, which constitutes the main body of Shuanghe Cave National Geopark in Suiyang County. With the continuous growth of survey length, the current Geopark boundary can no longer meet the needs of protection and management. Taking the spatial distribution of Shuanghe Cave as a reference, the author uses the hydrological and spatial analysis tools from ArcGIS software to extract the digital river network and divide the surface basin from the digital elevation model data (DEM) of Chiwuxi basin and its surrounding areas, and comprehensively considers the natural and human factors, the following understandings were formed: (1) It is considered that the digital water system simulated by 1000m2 concentration cumulant threshold with 1:50 000 DEM accuracy is highly consistent with the real water system. (2) The Shuanghe Cave system crosses the surface watershed of Chiwuxi, which directly reflects the phenomenon that the surface underground watershed does not coincide. (3) The Shuanghe Cave system has exceeded the boundary of the current Geopark and county-level administrative region since 2018. There is a vacuum in the protection and management of core geological relics, and the optimization and adjustment of the Geopark boundary is imminent. (4) The boundary of the Geopark should be dynamically adjusted in consideration of the prediction of the development boundary of Shuanghe Cave system, and a preliminary optimization and demarcation scheme is proposed. (5) The tracing test of Shuanghe Cave area should be strengthened in the future, and the scope of underground watershed should be more clear, so as to delimit the Geopark boundary more scientifically and completely.
Keywords:
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