松嫩平原地下水氟、砷的富集規(guī)律及影響因素研究

1、松嫩平原地下水氟、砷的富集規(guī)律及影響因素研究 【摘要】 本論文依托中國(guó)地質(zhì)調(diào)查局“東北地方病嚴(yán)重區(qū)地下水勘查及供水安全示范工程”和吉林省地調(diào)局“吉林省西部高氟、高砷區(qū)生態(tài)環(huán)境地球化學(xué)評(píng)價(jià)”項(xiàng)目。松嫩平原地下水原生水質(zhì)不佳,是我國(guó)地方性氟、砷中毒病區(qū)。長(zhǎng)期以來(lái)由于水質(zhì)問(wèn)題導(dǎo)致該區(qū)地下水資源緊缺,嚴(yán)重制約了社會(huì)經(jīng)濟(jì)的發(fā)展。因此,為保證區(qū)域飲水安全,合理開(kāi)發(fā)利用地下水資源,開(kāi)展地下水中氟、砷中毒的研究十分必要。在資料收集、野外調(diào)查、樣品采集及測(cè)試分析的基礎(chǔ)上,應(yīng)用水文地質(zhì)學(xué)、水文地球化學(xué)的基本理論和方法,借助野外調(diào)查、測(cè)試分析及數(shù)據(jù)分析技術(shù)等,結(jié)合地質(zhì)

2、、地貌特點(diǎn),開(kāi)展了松嫩平原地下水氟、砷的分布特征及相關(guān)的水化學(xué)特征研究。在查閱大量國(guó)內(nèi)外文獻(xiàn)的基礎(chǔ)上,結(jié)合項(xiàng)目組實(shí)測(cè)數(shù)據(jù)及對(duì)比國(guó)內(nèi)氟、砷中毒地區(qū),分析了研究區(qū)地下水氟、砷的來(lái)源,歸納總結(jié)了影響兩者富集的因素,提出了典型區(qū)地下水氟、砷的富集特征進(jìn)行了分析,建立了富集影響因素評(píng)價(jià)指標(biāo)體系。在區(qū)域宏觀分析的基礎(chǔ)上,選取典型地區(qū)進(jìn)行地下水中氟、砷富集特征及影響因素的總結(jié)?！綼bstract】 songnen plain is rich in groundwater resources,but the complexity of the problem of water quality,poor raw

3、 water quality,generally high fluoride area in diving is to the higher incidence of fluorosis in the world.in recent years,also found in the southwestern region of arsenic poisoning,the above-mentioned problems of water resources has fur- -ther exacerbated the contradiction between supply and demand

4、.therefore,for the rati- -onal development of groundwater resources and the prevention of endemic diseases,to carry out ground water fluoride,arsenic enrichment research imperative.in this paper,to participate in china established by the board emphasized the "seri- -ous endemic area northeast o

5、f groundwater exploration and water safety demonstration project" and emphasized the bureau of jilin province,"the western jilin province,high fluoride,high-arsenic geochemical evaluation of ecological environment," based on the completed project.in data collection,field investigation

6、,sample collection and testing based on the analysis,the application of hydro-geology,hydro-geochemistry of basic theories and methods,using analytical techniques of mathematical statistics,3s tech-nology, analysis of the songnen plain groundwater fluoride,arsenic distribution cha-racteristics and c

7、hemical characteristics of water,combined with the project team compared the measured data and is similar to the domestic area,an analysis of the study area ground water fluoride,arsenic sources,summarized the impact of the two enrich-hment factors.finally,select the typical area,extracted three typ

8、ical fluoride,arsenic-rich characteristics and analyzed.the concentration of fluoride and arsenic in the well to explain the phenomenon,in turn,verified the rationality of argumentation in this article.application of kriging interpolation method,combined with geographic inform-ation systems and mapp

9、ing software mapgis6.7 software suefer8.0,rendering the songnen plain groundwater fluorine,arsenic distribution and its characteristics are des-cribed. songnen plain groundwater fluoride content in the distribution of visible ban-ding, that is,from the basin center to the edge of the basin,from the

10、shallow dive into deep water pressure,fluorine concentration by the high prevalence of low rule.arsenic in groundwater exceeded the phenomenon is different from the universality of excessive fluoride,only to have the special characteristics of the geological environment in some areas,and focus on th

11、e 2030m aquifers.combination of geological,geomorphological characteristics,as compared with fluorine,arsenic concentration in different types of water chemistry characteristics, obtained with fluorine,arsenic-related chemical composition of the main water and related to each other.found that corres

12、pond to the high-arsenic groundwater with high concentrations of total iron,re-carbonate,low sulfate concentration,and a greater na /(cl + so4) ratios meq;high fluoride water chemical characteristics of clear water with high concentrations of the tds,fluoride standards for nearly twice as much water

13、;fluoride, arsenic concentration in groundwater at the same time,compared with other types of enrichment,and there are no special features of the hydrochemistry;high f,high-as groundwater,water chemistry types mostly hco3 type,hco3-cl or cl-hco3 type.the study area combined with the geochemical envi

14、ronment and high-fluorine water, the distribution of high-arsenic water location,kind of testing the use of geotechnical data to investigate the groundwater fluoride,arsenic source material is the interpretation of groundwater fluoride,arsenic concentration is the basis of with the key.songnen plain

15、 source of fluoride in groundwater can be divided into primary sources and secondary sources,is the primary source of rock weathering through release of fluoride,fluoride secondary sources refer to the soil and the leaching of sedimentary rocks,and carbonate analysis balance the release of fluoride.

16、mineral rocks of groundwater by arsenic is the primary source of arsenic is also a major source;arsenic in the organism and ferromanganese nodules quality secondary enrichment,constitutes a secondary source of arsenic in groundwater,but alsois a direct source.element fluorine and arsenic geochemical

17、 nature of the different elements to deter-mine the impact of two factors-rich groundwater,there is obviously different.on chec-king a large number of domestic and foreign literature on the basis of the measured data combined with the project team and contrast the domestic fluorine,arsenic poisoning

18、 areas, summarized the impact of groundwater fluoride,arsenic enrichment factor.high fluoride groundwater is in a particular geographical environment of the formation of these elements together for the natural environment,geological environment and the three types of human activities,the formation a

19、nd distribution of contributions from a variety of factors with a superposition of the control.to date,the causes of arsenic contamination of groundwater was not yet fully recognized the same conclusion,but the impact of arsenic-rich have a common understanding of certain factors,including oxidation

20、-reduction environment and role of microbial adsorption - desorption is a key factor.available on groundwater fluoride,arsenic enrichment research literature and found that research is limited to spatial scales over most of the serious areas,only a portion of the article has taken over the region an

21、d non-comparative study of overweight,but it is limited to a simple comparison of the chemical characteristics of water.in this paper,fluorine, arsenic poisoning typical tongyu county region taonan city and its adjacent areas and dry county as an example,in-depth comparative analysis of different regions,different aquifer fluoride and arsenic enrichment,extraction of the three typical features,in source analysis and impact factor analysis on the basis of the study area combined with the specific geological and hydrogeological conditions are analyzed.the conce- -ntration