| 219 | 0 | 385 |
| 下载次数 | 被引频次 | 阅读次数 |
【目的】莱芜地区泉水出露众多，但未开展过系统研究。为查清该地区泉水特征、泉水系统和形成机理，助力泉水保护工作，依据莱芜泉水普查工作对其进行了系统研究。【方法】采用资料利用分析、水文地质调查、地质钻探、水质分析等工作手段，分析了泉水发育水文地质条件，总结了泉水分布特征、水化学特征及质量特征，进行了泉水系统划分，探讨了泉水形成机理及控制因素。【结果】结果显示：泉水主要分布在莱芜盆地边缘及河流沟谷地区；按含水岩组类型可分为岩溶泉水和裂隙泉水，以下降泉为主，少数上升泉；泉水水化学类型以HCO3-Ca型、HCO3-Ca·Mg型和HCO3·SO4-Ca型为主，主要离子主要来源于水岩相互作用；82%泉水达到地下水III类及以上标准，部分为锶型、偏硅酸型天然矿泉水；泉水形成受地形地貌、地层岩性、断裂构造等地质因素控制，主要以浅层循环为主，水循环速度快。【结论】莱芜地区泉水出露分布受地形变化影响明显；整体泉水水质较好，循环速度快，水量与大气降水密切相关，易受人类活动影响。通过本次对莱芜泉水系统分析，可为当地泉水保护与城市建设和谐共生提供技术支持。
Abstract：[Objective]Numerous springs emerge in the Laiwu region, yet no systematic research has been conducted. To clarify the spring characteristics, spring systems, and their formation mechanisms in this region, and to support spring protection efforts, a systematic investigation was conducted based on the spring survey in Laiwu.[Methods]Method including data utilization analysis, hydrogeological surveys, geological drilling, and water quality analysis were employed to analyze the hydrogeological conditions for spring development. The distribution, hydrochemical, and quality characteristics of the springs were summarized. The spring systems were classified, and the formation mechanisms and controlling factors were examined.[Results]The result showed that the springs were mainly distributed at the margins of Laiwu Basin and in river valleys. Based on aquifer lithology, they could be classified into karst springs and fissure springs, with descending springs being dominant and a few ascending ones. The main hydrochemical types included HCO3-Ca, HCO3-Ca·Mg, and HCO3·SO3-Ca, with major ions primarily derived from water-rock interactions. 82% of the springs met or exceeded the Class III groundwater quality standards, with some being strontium-type or metasilicic acid-type natural mineral water. Spring formation was controlled by geological factors such as topography, stratum lithology, and fault structures, mainly featuring shallow circulation with rapid water cycling.[Conclusion]The spatial distribution of springs in the Laiwu Region is significantly affected by topographic variations. The springs show overall good water quality with rapid circulation. The spring discharge shows strong correlation with precipitation, making it susceptible to human activities. The systematic analysis of the spring systems in Laiwu provides technical support for the coordinated development of spring protection and urban planning in the region.
[1] 贺可强，刘炜金，邵长飞.鲁中南岩溶水资源综合类型及合理调蓄研究[J].地球学报，2002,23(4):369-374.HE K Q,LIU W J,SHAO C F.The comprehensive type classification and proper adjustment of karst water resource in the central-south region of Shandong Province[J].Acta Geosicientia Sinica,2002,23(4):369-374.
[2] 段壮，高明波，高继雷，等.山东莱芜张家洼铁矿床金云母40Ar/39Ar定年及其对成矿构造背景的启示[J].地质学报，2022,96(4):1279-1296.DUAN Z,GAO M B,GAO J L,et al.Phlogopite 40Ar/39Ar dating of the Zhangjiawa iron deposit,Laiwu District,Shandong Province:Implications for regional iron skarn mineralization of North China Craton[J].Acta Geologica Sinica,2022,96(4):1279-1296.
[3] 徐蒙，刘辉，张馨，等.莱芜区上王庄村水文地质参数计算及地下水水质评价[J].徐州工程学院学报(自然科学版),2021,36(4):48-52.XU M,LIU H,ZHANG X,et al.Calculation of hydrogeological parameters and evaluation of groundwater quality in Shangwangzhuang Village,Laiwu District[J].Journal of Xuzhou Institute of Technology (Natural Sciences Edition),2021,36(4):48-52.
[4] 马明，高继雷，高明波，等.鲁西莱芜地区地球物理特征及富铁矿床勘查模型建立[J].华北地震科学，2020,38(2):13-20.MA M,GAO J L,GAO M B,et al.Geophysical characteristics of Laiwu Area in Western Shandong Province and establishment of exploration model for iron rich deposits[J].North China Earthquake Sciences,2020,38(2):13-20.
[5] 刘书锋.山东莱芜地区中生代侵入杂岩特征与成矿关系[J].地质学刊，2020,44(S1):34-47.LIU S F.Characteristics of the Mesozoic intrusive complexes and their relation to metallogeny in Laiwu Area,Shandong Province[J].Journal of Geology,2020,44(S1):34-47.
[6] 王超，张立川，王应强，等.莱芜地区地下水污染研究[J].地下水，2021,43(6):21-24.WANG C,ZHANG L C,WANG Y Q,et al.Study on groundwater pollution in Laiwu Region[J].Ground Water,2021,43(6):21-24.
[7] 刘元晴，文冬光，吕琳，等.沂蒙山区典型断陷盆地岩溶地下水系统特征：以莱芜盆地为例[J].地质科技通报，2022,41(1):157-167.LIU Y Q,WEN D G,LYU L,et al.Characteristics of karst groundwater flow systems of typical faulted basins in Yimeng Mountain Area:A case study of Laiwu Basin[J].Bulletin of Geological Science and Technology,2022,41(1):157-167.
[8] 周乐，刘元晴，李伟，等.莱芜盆地构造演化特征及水文地质意义[J].科学技术与工程，2020,20(2):519-526.ZHOU L,LIU Y Q,LI W,et al.Tectonic evolutionary characteristics and their hydrological geological significance in Laiwu Basin[J].Science Technology and Engineering,2020,20(2):519-526.
[9] 王云燕.山东莱芜地区牛泉矽卡岩型铁矿成矿条件及找矿标志[J].山东国土资源，2021,37(10):23-28.WANG Y Y.Metallogenic conditions and prospecting marks of Niuquan skarn type iron deposit in Laiwu Area in Shandong Province[J].Shandong Land and Resources,2021,37(10):23-28.
[10] 李贵恒，冯建国，鲁统民，等.泰莱盆地地下水水化学特征及水质评价[J].水电能源科学，2019,37(4):52-55,121.LI G H,FENG J G,LU T M,et al.Hydrochemical characteristics and water quality assessment of groundwater in Tailai Basin[J].Water Resources and Power,2019,37(4):52-55,121.
[11] 高宗军，万志澎，贺可强，等.大汶河流域中上游地区岩溶地下水水化学特征及其控制因素分析[J].地质科技通报，2022,41(5):264-272.GAO Z J,WAN Z P,HE K Q,et al.Hydrochemical characteristics and controlling factors of karst groundwater in middle and upper reaches of Dawen River Basin[J].Bulletin of Geological Science and Technology,2022,41(5):264-272.
[12] 李国英.进一步全面深化水利改革为推动水利高质量发展、保障我国水安全作出新的贡献：在2025年全国水利工作会议上的讲话[J].水利发展研究，2025,25(1):1-12.LI G Y.Further comprehensively deepen water conservancy reform to promote high-quality development of water conservancy and safeguard national water security:A speech at the 2025 national water conservancy work conference[J].Water Resources Development Research,2025,25(1):1-12.
[13] 吴丰昌.我国水体污染控制与治理成效、科技支撑与展望[J].水利发展研究，2023,23(12):1-8.WU F C.Effectiveness,scientific and technological support,and prospects for water pollution control and management in China[J].Water Resources Development Research,2023,23(12):1-8.
[14] 李国英.为以中国式现代化全面推进强国建设、民族复兴伟业提供有力的水安全保障：在2024年全国水利工作会议上的讲话[J].水利发展研究，2024,24(1):1-10.LI G Y.Improved water security for China’s efforts to build itself into a stronger country and rejuvenate the Chinese nation on all fronts by pursuing Chinese modernization:Speech at the 2024 National Water Conservancy Work Conference[J].Water Resources Development Research,2024,24(1):1-10.
[15] 高峰，王振涛，靳丰山，等.山东省莱芜盆地岩溶塌陷风险性评价[J].中国人口·资源与环境，2016,26(S2):359-362.GAO F,WANG Zhentao,JIN F S,et al.Risk assessment of karst collapse in the Laiwu of Shandong Province[J].China Population,Resources and Environment,2016,26(S2):359-362.
[16] 张增奇，张成基，王世进，等.山东省地层侵入岩构造单元划分对比意见[J].山东国土资源，2014,30(3):1-23.ZHANG Z Q,ZHANG C J,WANG S J,et al.Views on classification and contrast of tectonic units in strata in Shandong Province[J].Shandong Land and Resources,2014,30(3):1-23.
[17] 许立青，李三忠，郭玲莉，等.郯庐断裂带对鲁西隆升过程的影响：磷灰石裂变径迹证据[J].岩石学报，2016,32(4):1153-1170.XU L Q,LI S Z,GUO L L,et al.Impaction of the Tan-Lu fault zone on uplift of the Luxi Rise:Constraints from apatite fission track thermochronology[J].Acta Petrologica Sinica,2016,32(4):1153-1170.
[18] 刘元晴，周乐，李伟，等.山东莱芜盆地西北缘古近系半固结含水岩组的特征及其成因[J].地球学报，2018,39(6):737-748.LIU Y Q,ZHOU L,LI W,et al.The characteristics and genetic analysis of the Paleogene semi-consolidated water-bearing formation on the northwestern margin of Laiwu Basin,Shandong Province[J].Acta Geoscientica Sinica,2018,39(6):737-748.
[19] 叶婷婷，颜照坤，李勇，等.渤海湾盆地沧东凹陷新生代原型盆地构造演化[J].科学技术与工程，2023,23(14):5914-5921.YE T T,YAN Z K,LI Y,et al.Tectonic evolution process of Cenozoic prototype basin in Cangdong Sag,Bohai Bay Basin[J].Science Technology and Engineering,2023,23(14):5914-5921.
[20] 李波，王金晓，吴璇，等.山东莱芜盆地东部水文地质条件及富水块段特征[J].中国岩溶，2020,39(5):637-649.LI B,WANG J X,WU X,et al.Hydrogeological conditions and characteristics of water-rich sections in the eastern Laiwu basin,Shandong Province[J].Carsologica Sinica,2020,39(5):637-649.
[21] 李波，于大潞，王楠，等.莱芜盆地岩溶地下水富集规律[J].地质力学学报，2024,30(4):691-702.LI B,YU D L,WANG N,et al.Karst groundwater enrichment law in Laiwu Basin[J].Journal of Geomechanics,2024,30(4):691-702.
[22] 孙逊，王克红，孙启堂，等.鲁中南山区岩溶裂隙水富水带类型及分布特征[J].工程勘察，2010,38(2):52-56.SUN X,WANG K H,SUN Q T,et al.Types and distribution of Karst fissure water in central and southern Shangdong Province[J].Geotechnical Investigation & Surveying,2010,38(2):52-56.
[23] 马振民，刘立才，陈鸿汉，等.山东泰安岩溶水系统地下水化学环境演化[J].现代地质，2002,16(4):423-428.MA Z M,LIU L C,CHEN H H,et al.Hydrochemical environmental evolution of karst water system in Tai’an,Shandong Province[J].Geoscience,2002,16(4):423-428.
[24] 李波，王金晓，赵无忌，等.莱芜盆地牟汶河流域水体同位素特征与分析[J].山东国土资源，2019,35(7):58-63.LI B,WANG J X,ZHAO W J,et al.Analysis on isotopic characteristics of water body of Muwen River Basin in Laiwu Basin[J].Shandong Land and Resources,2019,35(7):58-63.
[25] 李波，李常锁，王楠，等.山东莱芜地区泉水水化学特征及形成机制[J].环境化学，2024,43(5):1621-1631.LI B,LI C S,WANG N,et al.Hydrochemical characteristics and formation mechanism of spring water in Laiwu,Shandong Province[J].Environmental Chemistry,2024,43(5):1621-1631.
[26] 聂振龙，陈宗宇，程旭学，等.黑河干流浅层地下水与地表水相互转化的水化学特征[J].吉林大学学报(地球科学版),2005,35(1):48-53.NIE Z L,CHEN Z Y,CHENG X X,et al.The chemical information of the interaction of unconfined groundwaterand surface water along the Heihe River,Northwestern China[J].Journal of Jilin University (Earth Science Edition),2005,35(1):48-53.
[27] 秦娜，成文举，董方营，等.东平湖地区地下水化学特征及质量评价[J].科学技术与工程，2022,22(24):10434-10443.QIN N,CHENG W J,DONG F Y,et al.Chemical characteristics and quality evaluation of groundwater in Dongping Lake area[J].Science Technology and Engineering,2022,22(24):10434-10443.
[28] 汪敬忠，吴敬禄，曾海鳌，等.内蒙古河套平原水体同位素及水化学特征[J].地球科学与环境学报，2013,35(4):104-112.WANG J Z,WU J L,ZENG H A,et al.Characteristics of water isotope and hydrochemistry in Hetao Plain of Inner Mongolia[J].Journal of Earth Sciences and Environment,2013,35(4):104-112.
[29] 田原，余成群，雒昆利，等.西藏地区天然水的水化学性质和元素特征[J].地理学报，2014,69(7):969-982.TIAN Y,YU C Q,LUO K L,et al.Water chemical properties and the element characteristics of natural water in Tibet,China[J].Acta Geographica Sinica,2014,69(7):969-982.
[30] 蒋金沛，冯杰，张强，等.响水溪泉岩溶地下水水化学特征及成因[J].科学技术与工程，2023,23(27):11522-11529.JIANG J P,FENG J,ZHANG Q,et al.Hydrochemical characteristics and genesis of karst groundwater in Xiangshuixiquan[J].Science Technology and Engineering,2023,23(27):11522-11529.
[31] 李亮，龚建师，周锴锷，等.基于物元可拓的河南省柘城县浅层地下水质量综合评价[J].华东地质，2022,43(3):355-363.LI L,GONG J S,ZHOU K E,et al.Application of Matter-Element and extension method in the comprehensive evaluation of groundwater environment quality of Zhecheng County,Henan Province[J].East China Geology,2022,43(3):355-363.
[32] 孙涛，潘世兵，李永军.人工神经网络模型在地下水水质评价分类中的应用[J].水文地质工程地质，2004,31(3):58-61.SUN T,PAN S B,LI Y J.Application of artificial neural network model to groundwaterquality assessment and classification[J].Hydrogeology and Engineering Geology,2004,31(3):58-61.
[33] 高菡，宋一心，刘博瀚，等.山东省泰安市岩溶地下水系统划分及循环模式分析[J].水利水电快报，2024,45(2):29-33,43.GAO H,SONG Y X,LIU B H,et al.Analysis on division of karst groundwater system and its circulation model in Tai’an City,Shandong Province[J].Express Water Resources & Hydropower Information,2024,45(2):29-33,43.
[34] 吴芳，马杰，刘博华，等.六盘山西缘前庄地区水资源特征及开发利用建议[J].水利水电技术(中英文),2023,54(10):49-58.WU F,MA J,LIU B H,et al.Water resources characteristics in the Qianzhuang Area,west edge of the Liupan Mountains:Suggestions for development and utilization[J].Water Resources and Hydropower Engineering,2023,54(10):49-58.
基本信息:
DOI：10.13928/j.cnki.wrahe.2025.07.013
中图分类号:P641.5
引用信息:
[1]李波,朱恒华,吴芳,等.莱芜地区泉水系统特征及形成机理研究[J].水利水电技术(中英文),2025,56(07):177-189.DOI:10.13928/j.cnki.wrahe.2025.07.013.
基金信息:
国家自然科学基金项目(42202294); 山东省地质勘查项目(鲁勘字(2024)74号)
2025-05-21
2025-05-21
2025-05-21