河北平原地下水资源可持续利用研究
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摘要
水资源是基础自然资源,是生态环境的控制性因素之一。20世纪下半叶以来,世界上许多国家用水量急剧上升,一些地区相继引发水危机,水资源短缺问题在全世界正引起广泛重视,大量的国际会议把水资源问题作为主要议程。21世纪,随着全球社会经济的快速发展,人口普遍增加和城市化进程的加快,人类对水资源的开发利用不断深入,水资源各种利用方式之间的矛盾日益激化,人类面临的水资源紧缺问题日趋严峻。
     河北平原地处华北平原北部,是我国目前水资源供需矛盾最为尖锐的地区之一。由于地表水资源缺乏,地下水资源是河北平原的主要供水水源。随着社会经济和人口对水资源日益增长的需求,进入70年代,由于城乡缺水,河北平原开始大规模开发利用地下水。全省平原区浅层超采区和严重超采区面积分别为33026km2、1717km2,深层地下水超采区和严重超采区面积分别达到12011km2、31216 km2。导致山前局部地区浅部含水层疏干,中东部平原深层地下水水位大幅下降,并诱发了地面沉降等一系列环境地质问题,地下水的超量开采最终导致地面沉降、海水入侵等地质灾害和生态环境的破坏,带来了巨大的经济损失。因此分析河北平原地下水系统的循环机理、研究河北平原地下水资源可持续利用的理论和方法、探讨河北平原地下水持续利用的对策不仅具有重大的现实意义,而且具有深远的历史意义。
     作者通过深入分析河北平原地下水开发现状及造成的环境影响;对河北平原地下水进行了动态模拟,评价了河北平原地下水的脆弱性和水资源与社会经济的协调性,预测了河北平原未来地下水资源量和地下水水位的变化,并在此基础上提出了河北省水资源可持续利用的对策。取得了如下主要成果:
     (1)调查了河北平原地下水开发利用现状及其对环境造成的影响,分析了人为因素的扰动和全球气候变化对河北平原地下水环境的影响,探讨了降水、地下水资源量和径流的变化及它们之间的关系。
     (2)以GIS为平台,利用地统计方法中的变异函数研究了河北平原地下水水位、地下水水质的空间自相关和变异,并分析了二者在不同时段的变化。利用kriging插值法分析了河北平原地下水水位和地下水水质的空间分布情况,认为地下水水位和地下水水质的5个因子存在着空间自相关,地下水水位和水质的变异与人为因素有关。
     (3)以地下水水质评价结果的V类水为响应因子,可开采模数、地下水埋深、含水层净补给模数、含水层岩性的富水性和矿化度五个因素为预测因子,利用实证权重法研究了河北平原地下水的脆弱性。认为河北平原的地下水脆弱性较高区域主要分布在靠近渤海的滨海区,而受地下水埋深和地下水矿化度的影响,在河北平原的东部的唐山和秦皇岛一带的中部条带区域内脆弱性级别较高。
     (4)利用模糊数学法进行了河北平原水资源与社会经济的协调评价,同时,利用灰色系统、时间序列和神经网络的层次组合预测法对河北平原地下水的水资源量和地下水水位进行了中长期预测,认为河北平原水资源与社会经济严重不协调,未来地下水水位和水资源量继续下降。并在此基础上提出了河北省水资源可持续利用的对策。
Water resources belong to basic natural resources. It is one of the controlling factors of ecotope. Since the last stage of 20 centure, the water consumption of many countries rise steeply. And in many areas water crisis take place. The shortage of water resources arouses broad attention, and regards as main agenda in most international conferences. In 21 centure, with the global social economy developing fleetly, the population apace increases, and urbanization is accelerated observably. So the water exploitation deepen gradually, the contradictions among every utilization of water resources intensify increasingly. The shortage of water resources is more and more severe.
     Hebei plain, which is in the north of North China Plain, becomes one of the areas that face the controdations between supplies and demands for water severely. The surface water is lacking in Hebei plain, so the ground water is the main supply resource. Since 70s, towns and countries have become lacking of water along with the demands of water resources by social economy and population increasingly, that leads to cosmically exploration of groundwater. In this plain, the area of surficial overexploration is 33,026 km2, thereinto, the severe overexplorating area is 1,717 km2; the area of deep overexploration is 12,011 km2, thereinto, the severe overexplorating area is 31,216 km2. That causes the drainage of surfacial aquiclude in some piedmont, the rapid drop of water level of deep groundwater in the mideast plain, series of environmental geologic problems such as ground subsidence. The overexploration of groundwater will leads to ecotope damages and geologic disasters such as land subsidence, seawaterinvasion and so on, that will bring huge economic loss. So it is very meaningful that analyzing the circulate mechanics, studying the theories and methods of sustainable utilization of groundwater resources in North China Plain, discussing the countermeasures on sustainable utilizations of groundwater resources.
     Through in-depth analysis of the exporation actuality of groundwater and the environmental responsion in North China Plain, the author dynamic analogised the groundwater of Hebei plain, appraised the vulnerability of the groundwater and the compatibility between water resources and social economy, forecasted the quantity of the groundwater resources and the change of water level in future, bringed frowared countermeasures on sustainable utilizations of water resources in Hebei province, obtained some research productions as follow:
     (1)Investigated the exporation actuality of groundwater and the environmental responsion in North China Plain; analyzed the effect on groundwater environment in Hebei plain from man-made disturbance and global climate change; discussed the change of rainfall, the reserve of groundwater resources, surface flow and the relationship among them.
     (2)Based on GIS, investigated the groundwater level, spatial autocorrelation and variation of groundwater quality in Hebei plain by variation functions of geologic statistical method; analyzed their changes in different time-interval; studied the groundwater level and spatial distribution of groundwater quanlity in Hebei plain.
     (3)Taken the fifth class of groundwater quanlity as response factor, exploiting modulus, burial depth of groundwater, recharge modulus of water-bearing beds, water-reserving capability of water-bearing beds and the mineralizing degree as five pre-estimate factors, studied the vulnerability of groundwater in Hebei plain by positive weight method.
     (4)Appraised the compatibility between water resource of Hebei plain and social economy by fuzzing mathematics method; at the same time, made a medium-term and longterm pre-estimation on groundwater reservation and level in Hebei plain via the pre-estimating method that is a hierarchy combination of grey system, time series and neurowet. Based on these,bringed forward countermeasures on sustainable utilizations of water resources in Hebei province.
引文
[1]国家气候变化对策协调小组办公室,中国21世纪议程管理中心.全球气候变化-人类面临的挑战[M].商务印书馆.2004.70-79
    [2]王国庆.气候变化对黄河中上游水量的影响[J].人民黄河,1994,12.
    [3]尤联元等.环境变化对黄河下游来水来沙的影响[J].地理学报,1995,1.
    [4]傅国斌.全球变暖对华北水资源影响的初步分析[J].地理学与国土研究,1991,7.
    [5]刘春蓁等.气候变化对我国水文资源的可能影响[J].水科学进展,1997,3.
    [6]秦伯强,施雅风.青海湖水文特征及水文下降原因分析[J].地理学报,1992,3.
    [7]季子修等.海平面上升对长江三角洲附近沿海潮滩和湿地的影响[J].海洋与湖沼,1994,6.
    [8]刘昌明.今日水世界[M],暨南大学出版社,2000
    [9]范荣生 王大齐.水资源水文学[M],北京:中国水利水电出版社,1996.10
    [10]沈灿燊.水资源导论[M],北京:高等教育出版社,1990.5
    [11]王浩等.西北地区水资源合理配置和承载能力研究[M].黄河水利出版社,2003
    [12]葛新权等.知识经济与可持续发展[M].社会科学文献出版社,1999
    [13]中国21世纪议程.国21世纪人口,环境与发展白皮书[M].中国环境科学出版社,1994
    [14]孙富行.水资源承载力分析与应用[D].河海大学博士学位论文.2005.11:35-36
    [15]John D.Bredeheoft, The Water Budget Myth Revisited:Why Hydrogeologists Model,Ground Water,Jul/Aug 2002; Vol.40, No.4
    [16]王玮.鄂尔多斯白坚系地下水盆地地下水资源可持续性研究[D].博士学位论文.3-5
    [17]张建山,赵尔慧,李俊亭.潜水稳定流含水层最佳井深的实验研究[J].地 下水,1989,(04)
    [18]刘国栋,王安,陈卫东.科学开发配置水资源改善城区供水环境[J].海河水利,2004,(05)
    [19]崔亚莉等.西北地区地下水的地质生态环境调节作用研究[J].地学前缘.Mar 2001;Vol.8,NO.1
    [20]束龙仓,Xunhong Chen.地下水开采对河流流量衰减的影响分析——以美国内布拉斯加州普拉特河谷为例[J].水利学报,2003,(02)
    [21]段永侯,肖国强.河北平原地下水资源与可持续利用[J].水文地质工程地质,2003,(01)
    [22]王琪,史基安,赵兴东,张中宁,孟自芳.石羊河流域地下水地球化学特征演化的计算机模拟研究[J].中国沙漠,2003,(02)
    [23]丁宏伟,王贵玲,黄晓辉.红崖山水库径流量减少与民勤绿洲水资源危机分析[J].中国沙漠,2003,(01)
    [24]William M.Alley. Sustainability of Ground-Water Resources(MJ,USGS Circular 1186,Denver, Colorado,1999
    [25]李蝶娟,张世法,竺士林,武桂梅,雷太荣.太原市供水风险和外区调水水价预测[J].水科学进展,2000,(01)
    [26]朱文彬,樊国瑞.石家庄地区水资源利用与经济发展协调模型研究[J].水科学进展,1994,(04)
    [27]陈守煜,黄宪成,李登峰.大连市水资源利用与宏观经济协调发展规划多目标群决策模型与方法[J].水利学报,2003,(03)
    [28]冯国斌;阮本青.黄河流域节水灌溉的探讨[J].中国水利,1999,(05)
    [29]冯尚友,傅春.我国未来可利用水资源量的估测[J].武汉水利电力大学学报,1999,(06)
    [30]刘昌明.21世纪中国水文科学研究的新问题新技术和新方法[M],北京:科学出版社,2001.9
    [31]张平.国外水资源管理实践及对我国的借鉴[J].治淮,2005,(03)
    [32]陈守煌.复杂水资源系统优化模糊识别理论与应用[M].长春:吉林大学出版社,2002.113-124.
    [33]陈守煜.工程模糊集理论与应用[M].北京:国防工业出版社,1998,13-23,40-104.
    [34]陈守煜.系统模糊决策理论与应用[M].大连:大连理工大学出版社,1994.3-38,87-98.
    [35]陈守煜.模糊水文学与水资源系统模糊优化原理[M].大连:大连理工大学出版社.1990.
    [36]张文国.区域底地下水资源可持续利用的模糊集分析理论与应用研究[D].大连:大连理工大学博士论文,1999,1-4.
    [37]贾崃.区域水资源承载力研究[J].西安理工大学学报,1998,14(4):382-387.
    [38]张道军.复杂水环境资源系统智能管理、预测和决策研究田[D].大连理工大学博士学位论文.2002.10
    [39]陈守煜,李亚伟.基于模糊人工神经网络识别的水质评价模型[[J].水科学进展,2005,16(1):88-91.
    [40]薛建军,姚桂基.人工神经网络在水质评价中的应用[[J].水文,1997,3:37-39.
    [41]玛规龙,杨庆学.应用神经网络评价于桥水库水质[[J].海河水利,1999,5:39-46.
    [42]李亚伟.水资源系统模糊决策、评价与预测方法及应用[D].大连理工大学博士学位论文.2005.12:17-18
    [43]王本德.水文中长期预报模糊数学方法[M].大连理工大学出版社,1993.
    [44]王本德.水库防洪预报调度方法及应用[M].北京:中国水利水电出版社,1996.
    [45]丁晶,邓育仁.随机水文学[M].成都科技大学出版社,1988.
    [46]易丹辉.统计预测[M].中国人民大学出版社,1990.
    [47]陈守煜,中长期水文预报综合分析理论模式与方法[J].水利学报,1997(8):15-21.
    [48]聂相田.水资源管理系统模糊与随机分析方法及应用研究[D].大连理工大学博士学位论文.1999.4:13-15
    [49]徐军祥,邢立亭,佟光玉,范立芹.济南泉域地下水环境演化与保护[J].水文地质工程地质.2004.6:69-73
    [50]杨志双.河北平原区域地壳稳定性分析与评价[D].吉林大学博士学位论文.2003.11:7-12
    [51]张石春,张建平.河北省平原区近30年来地下水动态变化及可持续利用对 策[J].海河水利.2005.2:15-20
    [52]王欣宝,尚琳群,李玉龙.环渤海河北地区地下水环境演化研究[J].地质调查与研究.2004.27(3):149-156
    [53]郭永海,张作辰,沈照理,钟佐桑.河北平原地下水动力环境演化影响因素的关联度分析[J].工程地质学报.1995.3(3):62-66
    [54]张宗祜,施德鸿,沈照理,钟佐桑,薛禹群.人类活动影响下华北平原地下水环境的演化与发展[J].地球学报.1997.18(4):337-344
    [55]王焰新,马腾,郭清海,马瑞.地下水与环境变化研究[J].地学前缘.2005.12(特刊):14-21
    [56]CHEN Z, GRASBY S E, OSADETZK G. Relation between climate variability and groundwater levels in the upper carbonate aquifer, southern Manitoba, Canada[J]. Journal of Hydrology,2004,290(1):43-62.
    [57](河北省水利厅).2001水资源公报[2006.3]. http://www.hbsw.net
    [58](河北省水利厅).2002水资源公报[2006.3]. http://www.hbsw.net
    [59](河北省水利厅).2003水资源公报[2006.3]. http://www.hbsw.net
    [60](河北省水利厅).2004水资源公报[2006.3]. http://www.hbsw.net
    [61]郭迎春,张广录,阮新,et al. Influences of chronological variations of air temperature and precipitation on water resources and desertization in Hebei Province[J].地理学与国土研究,2001,17(2):67-70.
    [62]李生志,李国东,王顺兵,et al.河北省水资源环境[J].河北师范大学学报(自然科学版),1996,20(1):98-105.
    [63]李艳芳.河北省水资源危机和可持续利用[J].石家庄师范专科学校学报,2002,4(2):31-33.
    [64]李国正,苏晓虹,简明凯.河北省“非常规水资源”现状、潜力分析及对策[J].水资源保护,2005,21(5):58-60.
    [65]刘苏峡,莫兴国,朱永华,et al. A new method and for ecological water consumption calculation application in Haihe River Basin[J].自然资源学报,2004,19(5):662-671.
    [66]许月卿,蔡运龙.基于GIS的河北平原地下水位时空变化动态分析[J].北京大学学报自然科学版.2005.41(2):265-272.
    [67]王政权.地统计学及其在生态学中的应用[M].北京:科学出版 社,1999.162-192
    [68]候景儒,等.实用地质统计学[M].北京:地质出版社,1998.
    [69]李哈滨,王政权,王庆成.空间异质性定量研究理论与方法[J].应用生态学报,1998,9(6):651-657
    [70]Li HB., Reynolds JF. On definition and quantification of heterogeneity[J]. Oikos,1995,73:280-284
    [71]Goovaerts P. Geostatistics in soil science:state-of -the -art and perspectives[J]. Geoderma,1999.89:1-45
    [72]Chaosheng Zhanga, David McGrath. Geostatistical and GIS analyses on soil organic carbon concentrations in grassland of southeastern Ireland from two different periods[J]. Geoderma,2004,119:261-275
    [73]Nancy F. Glenna, James R. Carr. The use of geostatistics in relating soil moisture to RADARSAT-1 SAR data obtained over the Great Basin, Nevada, USA[J]. Computers & Geosciences,2003,29:577-586
    [74]Trangmar BB., RS. Yost. Application of geostatistics to spatial studies of soil properties [J]. Advances Agronomy,1985,38:44-94
    [75]Cynthia S.A. Wallacea, Joseph M. Wattsb, Stephen R. Yoola. Characterizing the spatial structure of vegetation communities in the Mojave Desert using geostatistical techniques[J]. Computers & Geosciences,2000,26:397-410
    [76]Nikos Nanos, Santiago C. Studying within-stand structure and dynamics with geostatistical and molecular marker tools[J]. Forest Ecology and Management,2004,189:223-240
    [77]Rossi Re, Mulla DJ, et al. Geostatistical tools for modeling and interpreting ecological spatial dependence[J]. Ecological Monographs,1992,62(2): 277-314
    [78]王军,傅伯杰.黄土丘陵小流域土地利用与土壤水分的时空分布[J].地理学报,2000,55(1):84-91
    [79]郭旭东,傅伯杰,陈利顶,等。河北省遵化平原土壤养分的时空变异特征-变异函数与Kriging插值分析[J].地理学报,2000,55(5):555-566
    [80]李小玉,宋冬梅,肖笃宁.石羊河下游民勤绿洲地下水矿化度的时空变异[J].地理学报.2005.60(2):319-327.
    [81]马黎春,盛建东,蒋平安,汤庆峰.克拉玛依干旱生态农业区土壤质地的空间异质性研究[J].干旱区地理.2006.29(1):109-114.
    [82]Goovaerts P. Geostatistics in soil science:State of the art and perspectives[J]. Geodema.1999.89:1-45
    [83]王学军,李本纲,陶澍.土壤微量金属含的空间分析[M].科学出版社2005.5:2-10
    [84]Calon C, Critto A, Marcomini A.2001.Risk based characterizeation of contaminated Industrial site using multivariate and geostatistical tools[J]. Envitonmental Pollution,111:417-427.
    [85]Colin P, Froidevaus R, Garcia M.1996. Integrating geophysical data for mapping the contamation of Industrial sites by polycyclic aromatic hydeocabons:a geostatistical approach[J]. ASTM Special Technical Publication,1270:69-87
    [86]Tao S.1995. Spatial structure of Copper, Lead, and Mercury Contents in Surface Soil in Shenzhen area[J]. Water, Air and Soil Pollution,82:583-591
    [87]Tao S.1995. Kringing and mapping of Copper, Lead, and Mercury Contents in Surface Soil in Shenzhen area. Water, Air and Soil Pollution,83:161-172
    [88]Luc Feyen, Jef Caers. Quantifying geological uncertainty for flow and transport modeling in multi-modal heterogeneous formations[J]. Advances in Water Resources.2006.29:912-929
    [89]Fethi B J. Muitivarial geostatistical design of groundwater monitoring networks[J]. J. Water Resource Planing and Management,1994,120(4):505.
    [90]William L. Wingle,Eileen P. Poeter I, Sean A. Mckenna. UNCERT: geostatistics, uncertainty analysis and visualizeation software applied to groundwater flow and contaminant transport modeling[J]. Computer & Geosciences,25(1999)365-376
    [91]Y.Wang, T.Ma, Z.Luo. Geostatistical and geochemical analysis of surface water leakage into groundwater on a regional scale:a case study in the Liulin karst system, northwestern China[J]. Journal of Hydrology.2001. 246:223-234.
    [92]Sergio Cinnirellaa, Gabriele Buttafuocob, Nicola pirrone. Stochastic analysis to assess the apatial distributeon of groundwater nitrate concentrations in the Po catchment (Italy) [J]. Environmental pollution,133(2005) 569-580
    [93]跨世纪的地学态势-调查与科技·中国地质矿产信息研究院,1998
    [94]N.Doerfliger, PY.Jeannin, RZwahlen·Water vulnerability assessment in karst environments a new method of defining protection areas using a mufti-attribute and GIS tools[J]. Environmental Geology,1999,39 (2): 165-176
    [95]郭永海,沈照理,钟佐.河北平原地下水有机氯污染及其与防污性能的关系[J].水文地质工程地质,1996,23(1):40-42
    [96]Z.Hrkal, J.M.Trouillard·Use of GIS for optimalization human activity in a catchment area:A example of the Beauce region (France) [J]. Environmental Geology,1994,24:22-27
    [97]林山杉.地下水脆弱性的概念及评价[J].长春地质学院学报,1997,27(supI):45-J47
    [98]A.J.Tesoriero, FD.Voss·predicting the probability of elevated nitrate concentrations in the Puget Sound Basin:Implications for aquifer susceptibility and vulnerability[J]. Ground Water.1997,35(6):1029-1039.
    [99]林山杉,武健强,张勃夫·地下水环境脆弱程度图编图方法研究[J].水文地质工程地质,2000 27(3):6-8
    [100]付素蓉,王焰新,蔡鹤生等.城市地下水污染敏感性分析[J].地球科学一中国地质大学学报,2000,25(5):482-486
    [101]孙才志,潘俊.地下水脆弱性的概念、评价方法与研究前景[J].水科学进展,2000 10(4)444-449
    [102]B.T.Nolan·Relating nitrogen sources and aquifer susceptibility to nitrate in shallow groundwater of the Unite States[J]. Ground water,2001, 39(2):290-299
    [103]Iain R.Lake, Andrew A.Lovett, Kevin M.Hiscock et al. Evaluating factors influencing groundwater vulnerability to nitrate pollution:developing the potential of GIS[J]. Journal of Enviromental Management.2003.68:315-328
    [104]P.A.Finke, D.J.Brus, M.F.P.Bierkens et al. Mapping groundwater dynamics using multiple sources of exhaustive high resolution data[J]. Geoderma. 2004.123:23-39
    [105]姜桂华.关中盆地地下水脆弱性研究[D].长安大学硕士学位论文.2002.11:23-30
    [106]雷静.地下水环境脆弱性的研究[D].清华大学工学硕士学位论文.2002.11:13-25
    [107]吴夏懿.基于GIS的济宁市地下水水质脆弱性评价[D].河海大学硕士学位论文.2006.3:1-9
    [108]王国利,周惠成,杨庆.基于DRASTIC的地下水易污染性多目标模糊模式识别模型[J].水科学讲展,2000.11(2):173-179
    [109]DONG LIANG, ZHU YINMEI and N.OGURA. A Modified DRASTIC Approach to Shallow Groundwater Vulnerability in the West Lake Watershed in Hangzhou, China[J]. SCIENCE PRESS, BEIJING.2002.12(1)73-80.
    [110]Alberti L, De Amicis M, Masetti M, et al. Bayes'rule and GIS for evaluating sensitivity of groundwater to contamination In IAVG. [J]. Annual Conference 2001
    [111]Bonham-Carter G F, Agterberg F P, Wright D F. Weights of evidence modeling a new approach to mapping mineral potential[J]. Geological Survey of Canada, Paper89/9,1989,171-183
    [112]Agterberg F P, Bonham-Carter G F, Wright D F. Statistical pattern integration for mineral exploration In Gaal, Gabor and Merriam Daniel F, eds. Computer application in resources estimation prediction and assessment for metal and petroleum[M]. Pergamon Press. Oxford.1990
    [113]Harris J R, Wilkinson L, Heather K, et al. Application of GIS processing techniques for producing mineral prospectivity maps- a case study: Mesothermal Au in the Swayze Greenstone Belt, Ontario Canada[J]. Natural Resources Research.2001,10(2):92-124
    [114]刘晓东,李著信.基于灰色组合模型的管道腐蚀速率预测[J]. CPVT.2007. 24(32):15-19
    [115]邓聚龙,灰色系统[M].北京:国防工业出版社,1985.
    [116]邓聚龙,灰色控制系统[M].武汉:华中工学院出版社,1985.
    [117]陈意平,曲谦隆.灰色系统理论在水利工程中的应用[M].太原:山西科学技 术出版社,1992.
    [118]贺北方,刘正才.灰色系统理论方法与应用[M].气象出版社,1995.
    [119]聂相田,邱林等.水资源可持续利用管理不确定性分析方法及应用[M],河南:黄河水利出版社,1999.9
    [120]蒋燕.ARIMA模型在广西全社会固定资产投资预测中的应用[J].数理统计与管理.2006.25(5):588-592
    [121]黄杰,钱瑾,殷浩文.ARIMA模型在苏州河总磷预测中的应用[J].环境工程学报.2007.1(1):131-135
    [122]胡守仁,余少波,戴葵.神经网络导论[M].北京:国防科技大学出版社,1997.
    [123]徐献铮,张百灵,韦岗等.神经网络理论与应用[M].华南理工大学出版社,1994
    [124]陈守余,周梅春.人工神经网络模拟实现与应用[M].武汉:中国地质大学出版社,2000.
    [125]飞思科技产品研发中心.MATLAB6.5辅助神经网络分析与设计[M].北京:电子工业出版社,2003.
    [126]杨维,王恩德,边大忠.沈阳市规划中心区地下水利用优化管理模型[J].东北大学学报(自然科学版).2004.25(9):907-910
    [127]阮本清,梁瑞驹,王浩等.流域水资源管理[M].北京:科学出版社.2001.11:1-90
    [128]姜文来.水资源价值论[M].科学出版社:北京.1998:40-70

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