Study on the ecological water level and the ecological groundwater demand in Funing County, Jiangsu Province
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摘要: 苏北平原区浅层地下水与地表水体具有频繁影响、相互制约的特点,地下水的生态属性和环境功能十分重要,因此研究其生态水位及生态需水量盈亏特征对于生态保护具有重要意义。以江苏省阜宁县为例,在分析浅层地下水水位动态的基础上,通过统计分析的方法确定了生态水位的指标体系,研究了地下水生态水位,并基于Arcgis平台评估了浅层地下水生态水量盈亏特征。结果显示:阜宁县大部分地区生态水位埋深上限值为1.5~3 m,生态水位埋深下限值为2.63~3.18 m;2021年1月,25.3%左右的区域地下水位处于非适宜区,生态需水量为589.96万 m3;2021年5月,生态需水量为747.19万 m3。在地下水非适宜区,要结合县域供水现状,调整浅层地下水利用方式,宜禁则禁,宜采则采,实现地下水生态和环境功能的高效管控。Abstract: The shallow groundwater and surface water in northern Jiangsu plain are interacted and inter-conditioned. Due to the importance of the ecological properties and environmental functions of groundwater, it is essential to study its ecological water level and surplus-deficit characteristics of ecological water demand for ecological protection and restoration. Taking Funing County as an example, based on the analysis of shallow groundwater level dynamics, the index system of ecological water level was determined by the method of statistical analysis and the ecological water level of groundwater was studied, as well as the surplus-deficit characteristics of shallow groundwater ecological water were evaluated on Arcgis platform. The results show that the upper limit of burial depth of ecological water level in most areas of Funing County ranges from 1.5 m to 3 m, and the lower limit ranges from 2.63 m to 3.18 m. In January 2021, about 25.3% of the regional groundwater level was in the unsuitable extraction area, and the ecological water demand was 5 899 600 m3. In May 2021, the ecological water demand was 7 471 900 m3. In the groundwater unsuitable extraction area, the groundwater extraction and the prohibition of shallow groundwater use should be adjusted accordingly in combination with the situation of water supply within the county area, so that the ecological and environmental functions of groundwater can be efficiently controlled.
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[1] 贾利民,郭中小,龙胤慧,等.干旱区地下水生态水位研究进展[J].生态科学,2015,34(2):187-193.
JIA L M, GUO Z X, LONG Y H, et al. Research advances in ecological groundwater level in arid areas [J]. Ecological Science, 2015,34(2):187-193.
[2] 吴明辉,宁虎森,王让会,等.克拉玛依地区减排林地下水动态变化及合理生态水位分析[J]. 水土保持通报, 2010,30(4):129-133.
WU M H, NING H S, WANG R H, et al. Dynamic change of groundwater and reasonable ecological groundwater level in karamay artificial carbon-dioxide-capture forest[J]. Bulletin of Soil and Water Conservation, 2010, 30(4):129-133.
[3] 孙宪春,金晓媚,万力.地下水对银川平原植被生长的影响[J].现代地质, 2008,22(2):321-324.
SUN X C, JIN X M, WAN L. Effect of groundwater on vegetation growth in Yinchuan Plain[J].Geoscience, 2008,22(2):321-324.
[4] 李福林,陈华伟,王开然,等.地下水支撑生态系统研究综述[J].水科学进展,2018,29(5):750-758.
LI F L, CHEN H W,WANG K R, et al. Comprehensive review of groundwater-dependent ecosystems[J]. Advances in Water Science, 2018,29(5):750-758.
[5] XIN P, KONG J, LI L, et al. Modelling of groundwater-vegetation interactions in a tidal marsh[J]. Advances in Water Resources, 2013,57(2):52-68.
[6] RUNYAN C W, D’ODORICO P. Ecohydrological feedbacks between salt accumulation and vegetation dynamics: Role of vegetation groundwater interactions[J]. Water Resources Research, 2010,46 (11):W11561.1-W11561.11.
[7] LI X, ZHENG Y, SUN Z, et al. An integrated ecohydrological modeling approach to exploring the dynamic interaction between groundwater and phreatophytes[J]. Ecological Modelling, 2017,356(24):127-140.
[8] 张长春,邵景力,李慈君,等.华北平原地下水生态环境水位研究[J].吉林大学学报(地球科学版), 2003,33(3): 323-326.
ZHANG C C, SHAO J L, LI C J, et al. A study on the ecological groundwater table in the north China plan[J]. Journal of Jilin University(Earth Science Edition),2003,33(3):323-326.
[9] 樊自立,马英杰,张宏,等.塔里木河流域生态地下水位及其合理深度确定[J].干旱区地理,2004, 27(1):8-13.
FAN Z L, MA Y J, ZHANG H, et al. Research of eco-water table and rational depth of groundwater of Tarim River drainage basin[J]. Arid Land Geography, 2004, 27(1):8-13.
[10] 孙才志, 高颖, 朱正如. 基于生态水位约束的下辽河平原地下水生态需水量估算. 生态学报, 2013,33(5): 1513-1523.
SUN C Z,GAO Y,ZHU Z R.Estimation of ecological water demands based on ecological water table limitations in the lower reaches of the Liaohe River Plain, China. Acta Ecologica Sinica, 2013, 33(5): 1513-1523.
[11] 党学亚, 卢娜, 顾小凡,等. 柴达木盆地生态植被的地下水阈值[J]. 水文地质工程地质, 2019,46(3):1-8.
DANG X Y, LU N, GU X F, et al. Groundwater threshold of ecological vegetation in Qaidam Basin[J]. Hydrogeology & Engineering Geology, 2019,46(3):1-8.
[12] 赵海卿. 吉林省西部平原区地下水生态水位及水量调控研究[D].北京:中国地质大学(北京), 2012. ZHAO H Q. Study on ecological groundwater level and the amount of regulation in plain region of Western Jilin Province[D]. Beijing: China University of Geosciences (Beijing), 2012.
[13] 叶茂, 徐海量, 龚君君, 等. 不同胸径胡杨径向生长的合理生态水位研究[J]. 地理科学, 2011,31(2):172-177.
YE M, XU H L, GONG J J, et al. Rational ecological groundwater level of populus euphratica with different diameter in lower reaches of Tarim River [J]. Scientia Georaphica Sinica, 2011,31(2):172-177.
[14] 王让会, 宋郁东, 樊自立, 等. 塔里木流域"四源一干"生态需水量的估算[J]. 水土保持学报, 2001, 15(1): 19-22.
WANG R H, SONG Y D, FAN Z L, et al. Estimation on ecological water demand amount in four sources and one main stream area of Tarim Basin[J]. Journal of Soil and Water Conservation, 2001, 15(1): 19-22.
[15] 玛丽娅·奴尔兰, 刘卫国, 霍举颂, 等. 旱生芦苇对地下水位变化的生态响应及适应机制[J]. 生态学报, 2018,38 (20):7488-7498.
MARIA·N, LIU W G, HUO J S, et al. Ecological response and adaptation mechanism of Phragmites australis to changes in groundwater level [J]. Acta Ecologica Sinica, 2018, 38(20):7488-7498.
[16] 李明, 宁立波, 卢天梅. 土壤盐渍化地区地下水临界深度确定及其水位调控[J]. 灌溉排水学报, 2015,34(5):46-50.
LI M, NING L B, LU T M. Determination and the control of critical groundwater table in soil salinization area [J]. Journal of Irrigation and Drainage, 2015,34(5):46-50.
[17] 孙雅琦. 黑河下游生态需水及生态调度研究[D].西安:西北大学, 2017. SUN Y Q. The study on the ecological water requirement and ecological operation in the Lower Reaches of Heihe River for ecological conservation and restoration [D]. Xi’an: Northwest University, 2017.
[18] 靳婷婷,段学军,邹辉.岸线资源利用变化与影响因素——以长江南京段为例[J].华东地质,2021,42(1):9-20.
JIN T T,DUAN X J,ZOU H. Change and influencing factors of shoreline resources utilization in the Nanjing section of the Yangtze River[J].East China Geology,2021,42(1):9-20.
[19] 王赫生,龚建师,周锴锷,等.淮河流域及东南诸河流域土地利用和蒸散发量的多年时序变化[J].华东地质,2021,42(1):124. WANG H S, GONG J S, ZHOU K E. Multi year temporal changes of land use and evapotranspiration in Huaihe river basin and Southeast river basins[J]. East China Geology, 2021,42(1):124.
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