鄂西岩溶槽谷区洼地的水位响应特征及产流阈值估算

廖春来; 罗明明; 周宏

doi:10.11932/karst20200602

鄂西岩溶槽谷区洼地的水位响应特征及产流阈值估算

doi: 10.11932/karst20200602

1.
中国地质大学（武汉）环境学院/自然资源部、广西岩溶动力学重点实验室
2.
中国地质大学（武汉）环境学院/自然资源部/广西岩溶动力学重点实验室
3.
中国地质大学（武汉）地质调查研究院

基金项目: 国家自然科学基金（41807199）；自然资源部、广西岩溶动力学重点实验室开放基金（KDL201702）；湖北省自然科学基金（2018CFB170）；中国地质调查局项目（12120113103800、DD20190824）

计量
- 文章访问数: 1452
- HTML浏览量: 591
- PDF下载量: 238
- 被引次数: 0
出版历程
- 发布日期: 2020-12-25

Water level response characteristics and runoff threshold estimation of karst depressions in a valley region, western Hubei Province

1.
School of Environmental Studies, China University of Geosciences/Key Laboratory of Karst Dynamics,MNR&GZAR, Guilin
2.
School of Environmental Studies, China University of Geosciences/Key Laboratory of Karst Dynamics,MNR&GZAR, Guilin
3.
Institute of Geological Survey of China University of Geosciences

摘要

摘要: 以湖北省兴山县黄粮镇刘家坝和龙湾两处岩溶洼地作为研究对象，利用其降雨、水文和土壤水等监测数据，探讨灌入式补给条件下洼地汇流的水位响应特征和产流特点，并基于降雨量和洼地内明渠流量的关系，采用数学拟合方程，估算两处洼地的降雨产流阈值，进而分析了影响产流阈值的因素。结果表明：降雨强度增大，产流阈值减小；土壤前期含水率越大，越有利于坡面产流；落水洞和岩溶泉水位与降雨有较好的同步响应关系，水位变化曲线随雨强大小分别表现出“陡升陡降”和“缓升缓降”的特点；刘家坝和龙湾洼地的产流阈值分别为7.4 mm和10.6 mm。
- 岩溶洼地 /
- 灌入式补给 /
- 水位响应 /
- 产流阈值
Abstract: Liujiaba and Longwan, Huangliang town, Xingshan county, Hubei Province are two karst depressions in valley region with elevations of 886 m and 997 m, and catchment areas 20.9 km2 and 1.83 km2, respectively. After rainfalls, these karst depressions runoff and transform the surface water into groundwater through the sinkholes which connect to the open channels at the bottom of the depressions, and finally discharge to the Bailong spring. To study such a hydrogeological process, rainfall stations, hydrological monitoring stations and soil-water monitoring equipment were installed in these depressions and a hydrological monitoring station constructed in the Bailong Spring. Rainfall stations record air temperature and rainfall, hydrological stations monitor water level and water temperature in the sinkholes, and soil-water monitoring equipment record the soil moisture content and electrical conductivity. Different methods were used to analyze these observational data, so as to reveal characteristics of water level response and runoff yield and their influencing factors under the condition of concentrated recharge. The results show that， (1) the water level responses in the sinkholes and karst springs have better synchronous relationships with the rainfall, expressing "sudden rise and steep drop" in hydrographs with large rainfall intensity and "slow rise and slow fall" in hydrographs with low rainfall intensity. When very heavy rainfalls happen, karst waterlogging is easy to occur due to the sinkhole’s limited drainage ability. On July 24, 2019 after a rainfall storm (86.5 mm in 3.5 hours), the water level (1.96 m) surpassed the open channel height (1.6 m) in the Longwan karst depression； (2) The Chey-Manning formula was used to transfer the water level of the open channel into flow, then the rainfall and the flow of the open channel was fitted by a mathematical equation to estimate the runoff threshold of the Liujiaba and Longwan depressions, yielding values of 7.4 mm and 10.6 mm, respectively； (3)Through the changes of soil moisture content and electrical conductivity before and after the rainfall event, the influencing factors of runoff threshold were analyzed, indicating the rainfall intensity decreases the runoff threshold, and large antecedent soil moisture could promote slope-runoff. In addition, the yield threshold is also related to the topographic slope and soil material of karst depressions, implying the yield threshold is a multi-factor coupling parameter.
- karst depression /
- concentrated recharge /
- water level response /
- runoff threshold

HTML

参考文献(14)

[1]	李锋瑞.干旱农业生态系统研究［M］.西安：陕西科学技术出版社，1998.
[2]	徐铭泽，杨洁，刘窑军，等.不同母质红壤坡面产流产沙特征比较［J］.水土保持学报，2018，32（2）：34-39.
[3]	艾宁，刘广亮，朱清科，等.基于土壤前期含水量-降雨耦合关系的陕北黄土坡面产流临界降雨值［J］.中国水土保持科学，2018，16（5）：23-29.
[4]	Mandal U K，Rao K V，Mishra P K，et al. Soil infiltration，runoff and sediment yield from a shallow soil with varied stone cover and intensity of rain［J］.European Journal of Soil Science，2005，56（4）：435-443.
[5]	郭星星，吕春娟，陈丹，等.降雨强度和坡度对裸露铁尾矿砂坡面产流产沙的影响［J］.水土保持学报，2019，33（2）：23-29.
[6]	Jain B L，Singh R P. Run-off as influenced by rainfall characteristics，slope and surface treatment of micro-catchments［J］.Annals of Arid Zone，1980，19（1/2）：119-125.
[7]	Kampf S K， Faulconer J， Shaw J R， et al. Rainfall Thresholds for Flow Generation in Desert Ephemeral Streams［J］. Water Resources Research， 2018， 54（12）：9935-9950.
[8]	黄俊，吴普特，赵西宁.多参数非线性降雨产流阈值模型试验研究［J］.北京林业大学学报，2011，33（1）：84-89.
[9]	李小雁，龚家栋，高前兆.人工集水面临界产流降雨量确定实验研究［J］.水科学进展，2001， 12（4）：516-522.
[10]	姜光辉，吴吉春，郭芳，等.森林覆盖的喀斯特地区表层岩溶带的产流阈值［J］.水科学进展， 2008， 19（1）：72-77.
[11]	黄荷，罗明明，陈植华，等.香溪河流域大气降水稳定氢氧同位素时空分布特征［J］.水文地质工程地质，2016，43（4）：36-42.
[12]	罗明明，周宏，陈植华.香溪河流域岩溶水循环规律［M］.北京：科学出版社，2018.
[13]	罗明明，尹德超，张亮，等.南方岩溶含水系统结构识别方法初探［J］.中国岩溶，2015，34（6）：543-550.
[14]	Mingming Luo，Zhihua Chen，Hong Zhou，et al. Identifying structure and function of karst aquifer system using multiple field methods in karst trough valley area，South China［J］.Environmental Earth Sciences，2016，75（9）：824.