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1.
The stone pagoda of the Bunhwangsa temple in Republic of Korea was made of piling small brick-shaped stones. The majority of stone bricks are andesitic rocks with variable geneses. Rock properties of the pagoda roof suffer partial significant deterioration, such as multiple peel-offs, exfoliation, onion-peel-like decomposition, cracks forming round lines and falling-off stone pieces. The stylobates and tabernacles at the four corners are composed of granitic rocks, which are heavily contaminated by lichens and mosses. Some of these contamination marks show dark black or yellowish brown colors by inorganic secondary hydrates. The four tabernacles and northern face of the pagoda body have been exposed to relatively high humidity, which causes light gray efflorescence as stalactites between the northern and western sides of the body. The efflorescences are composed of calcite, gypsum and clay minerals. The stone lion statues at the southeast and northeast corners are made of alkali granite, while the others are lithic tuff. Total rock properties of the pagoda consist of 9,708 stone bricks. Among them, 11.0% are fractured, 6.7% are fallen off, and 7.0% show considerable surface efflorescence, which shows that the pagoda has been highly deteriorated by physical, chemical and biological weathering. The authors strongly suggest long-term monitoring and comprehensive conservation researches.  相似文献   

2.
魏峰  胡璟珂 《岩矿测试》2014,33(4):578-583
微量注射器越来越多地用于转移微量液体,但是微量注射器中有机化合物的残留可能造成的交叉污染易被忽视。本文系统地研究了微量注射器中有机氯农药类和多氯联苯类化合物的残留和清洗效果。结果表明,三个品牌的微量注射器清洗的难易不同,在选择微量注射器时应根据实验结果选择满足实验要求的类型;正己烷清洗液的体积与稀释倍数成正比,原因在于0.1 mL、0.2 mL、0.5 mL和1 mL第一针清洗液洗出的化合物质量接近,清洗液体积甚至与洗出化合物的量负相关,因此选用体积最小的0.1 mL效果和成本优势最大;相同浓度的有机氯农药类和多氯联苯类化合物清洗效果接近,原因可能是这两类化合物的理化性质相近;不同浓度的标准溶液需要清洗的次数不同,浓度越高的标准溶液需要清洗的次数越多。本文总结出三条清洗规律:①1 mL微量注射器中的残留量约为吸取量的1%左右;②第一针洗出化合物的量超过残留量的90%;③随着清洗次数的增加,呈现清洗效果越来越差、稀释倍数越来越小的趋势。根据这些规律,可以针对不同浓度的不同化合物采取相应的清洗措施,在标准溶液配制和气相色谱仪方法设置过程中更有效地预防污染和节约成本。  相似文献   

3.
The worst environmental pollutants in Anzali International Wetland are oily hydrocarbons especially aromatic and poly aromatic compounds (PAHs). The existence of oily compounds with approximate limit of concentration of 0.1 μg/l in aquatic environment bans the growth of fish larva and causes the generic state manner of animals. Anzali International Wetland, which is situated in the west — southern part of Caspian Sea where has environmental importance in life of living organisms and ecosystems. In this reseach, four sites, Pirbazar, Pasikhan, west and central parts, where are situated in Anzali International Wetland, have been studied in 2002. Waste sedimentation soil Sampling was performed during winter and spring in the above-mentioned regions. In the first stage, the purpose of sampling was to access optimum instrumental conditions and correct and precise procedures. Oily pollutants were extracted from water and it was done by using CC14 solvent after cleaning and concentrating. The extracted samples were identified with gas chromatographic method with using polyaromatic standard solutions. By the powerful GC/MS method; results of qualitative analysis were confirmed. Also by GC/MS using SIM mode quantitative analysis were performed. Quantitative study of polyaromatic compounds has also been done by luminescence spectrophotometry. Some compounds which were identified in the water samples were: olifinic, aromatic and poly — aromatic compounds such as: antracene, fluourine, xylene, methylbenzene, naphthalene and acenaphtylene. Finally, the degree of biodegradation of compounds such as pristan (C19H40) and phytan (C20H42) in water samples was integrated.  相似文献   

4.
The Bulkugsa Dabotap pagoda was built in AD 761, and designated as World Cultural Heritage by UNESCO in 1995. The ca. 270 blocks used in the construction of the pagoda consist mainly of white grey alkali granite with medium-grained equi-granular texture and small mialolitic cavities. Small quantities of biotite granite, granodiorite, gabbroic and tuffaceous rocks were also used. Some overlapping blocks are very damp. The pagoda body is inclined toward the northeast owing to differential loading. Fractures and artificial deterioration of the pagoda are not serious, but the surfaces of blocks show exfoliations that indicate granular decomposition of minerals. The supporting rocks and the round handrail of the octagonal second floor are too weathered to be treated and are being replaced. The roof stones on the first and second floor are seriously damaged because there is no drainage route for rainwater. The joints between blocks have fractures that cross each other; they have been further damaged by inserting concrete, cement mortar, rock fragments and iron plates. This has accelerated discoloration and fractures. Widespread colonization by algae, fungi, lichens and bryophytes has occurred on the margins and surfaces roof stones of the pagoda. Chemical treatment will be necessary to remove the vegetation cover.  相似文献   

5.
Comprehensive understanding of chemical and mineralogical changes induced by weathering is valuable information when considering the supply of nutrients and toxic elements from rocks. Here minerals that release and fix major elements during progressive weathering of a bed of Devonian New Albany Shale in eastern Kentucky are documented. Samples were collected from unweathered core (parent shale) and across an outcrop excavated into a hillside 40 year prior to sampling. Quantitative X-ray diffraction mineralogical data record progressive shale alteration across the outcrop. Mineral compositional changes reflect subtle alteration processes such as incongruent dissolution and cation exchange. Altered primary minerals include K-feldspars, plagioclase, calcite, pyrite, and chlorite. Secondary minerals include jarosite, gypsum, goethite, amorphous Fe(III) oxides and Fe(II)-Al sulfate salt (efflorescence). The mineralogy in weathered shale defines four weathered intervals on the outcrop—Zones A–C and soil. Alteration of the weakly weathered shale (Zone A) is attributed to the 40-a exposure of the shale. In this zone, pyrite oxidization produces acid that dissolves calcite and attacks chlorite, forming gypsum, jarosite, and minor efflorescent salt. The pre-excavation, active weathering front (Zone B) is where complete pyrite oxidation and alteration of feldspar and organic matter result in increased permeability. Acidic weathering solutions seep through the permeable shale and evaporate on the surface forming abundant efflorescent salt, jarosite and minor goethite. Intensely weathered shale (Zone C) is depleted in feldspars, chlorite, gypsum, jarosite and efflorescent salts, but has retained much of its primary quartz, illite and illite–smectite. Goethite and amorphous FE(III) oxides increase due to hydrolysis of jarosite. Enhanced permeability in this zone is due to a 14% loss of the original mass in parent shale. Denudation rates suggest that characteristics of Zone C were acquired over 1 Ma. Compositional differences between soil and Zone C are largely attributed to illuvial processes, formation of additional Fe(III) oxides and incorporation of modern organic matter.  相似文献   

6.
冯家江是北海市区重要的生态廊道。研究冯家江流域水体中氮的空间分布特征、污染来源、影响因素,对掌握冯家江流域氮污染现状及污染防控等具有重要的现实意义。本研究应用地统计学方法分析了冯家江流域地表水及沿岸地下水中氮污染物的空间分布特征。结果表明,地表水中氮污染物呈现出“高氨氮、低硝氮”的特征,NH3-N质量浓度平均值高达5.42 mg/L,NO3-N在孔隙潜水中明显富集,其质量浓度最高达32.63 mg/L。城镇生活污染物、人畜粪便及农业生产中化肥的施用是地表水、地下水中氮污染物的主要来源。pH值、氧化还原条件及包气带岩性结构和厚度是影响冯家江流域水体中氮污染物迁移转化的重要因素。  相似文献   

7.
洪范池铁矿体赋存于太古宙泰山岩群山草峪组,矿体周围泉水众多,论证矿床开采疏排水能否对泉水产生影响具有重要意义。研究分析表明,朱砂洞组含水层及山草峪组风氧化带裂隙水是矿床充水的直接充水水源,矿床充水水文地质条件属简单类型。泉水出露于寒武纪张夏组含水层中,并且与山草峪组含水层间无水力联系。若张夏组含水层不与采区沟通,矿山生产疏排水不会对泉水产生明显的影响。  相似文献   

8.
Monitoring of mine waste on sulphide deposits through hyperspectral remote sensing data contributes to predicting surface water quality, quantitatively estimating acid drainage and metal contamination on a yearly basis. The mineralogy of surface crusts loaded with highly soluble salts is a record of available humidity and temperature along the year. A temporal monitoring of salt efflorescence on mine wastes at a mine site in the Iberian Pyrite Belt (Spain) has been mapped in this work using hyperspectral airborne Hymap data. Climate change estimations are made based on oxidation stages derived from well-known sequences of minerals tracing sulphides oxidation intensity, using archive spectral libraries. Therefore, mine-waste weathering products of sulphide mapped from airborne hyperspectral remote sensing data can be used as a short-term record of climate change, providing a useful tool for assessing environmental geoindicators in semi-arid areas.  相似文献   

9.
【研究目的】查明防城港地区浅层偏酸性地下水时空分布、成因及环境影响。【研究方法】于2013—2015年间进行了浅层地下水pH值现场测试,枯水期214组,丰水期168组;讨论了其时空分布特征、成因和生态影响。【研究结果】结果表明,丰水期和枯水期偏酸性（pH <6.5）地下水样分别占79.3%和64.3%,pH值总体上丰水期低于枯水期。地下水pH值在低山区（均在5≤pH＜5.5范围,平均值5.18,n=4）＜丘陵区（大多数5≤pH＜6.5,平均值5.18,n=202）＜平原区（大多数6.5≤pH＜8.5,平均值6.77,n=8）。【结论】偏酸性地下水成因主要与偏酸性大气降水有关,其次与酸性的包气带介质及硫化物矿物的氧化有关。偏酸性大气降水入渗补给是丰水期pH值低于枯水期的主要原因。相比较而言,潮汐作用使得江平地区地下水pH值升高。偏酸性地下水影响饮水安全（研究区枯水期仅20.6%的样品pH值符合生活饮用水标准）,促进某些有害组分的释放,腐蚀地下管网和建筑桩基等设施。偏酸性地下水向地表水排泄亦可对地表水环境和地表生态系统产生影响。本研究有助于研究区水资源管理。创新点：本研究利用地质调查项目数据优势,系统阐述了防城港地区浅层偏酸性地下水时空分布特征;偏酸性地下水的成因与偏酸性大气降水、酸性包气带介质和硫化物矿物氧化有关;偏酸性地下水对人类健康、地下设施和生态环境具有潜在影响。  相似文献   

10.
水中有机污染物的超声处理技术发展研究   总被引：1，自引：0，他引：1  
王德慈 《地下水》2011,33(5):67-69
超声技术在处理水中有机污染物的应用近年来受到越来越多的关注。与常规处理方法相比,超声处理技术高效省时,对众多难处理有机污染物具有良好的降解作用。结合近年来超声技术处理水中有机污染物的研究进展,通过介绍超声降解有机污染物的原理、方法及其应用,最后对水中有机物的超声处理技术的发展趋势进行了展望,指出高效、省时的超生空化技术...  相似文献   

11.
The facing masonry of the Gothic Charles Bridge in Prague (Czech Republic) has been largely altered during nineteenth and twentieth century repairs, due to extensive replacements of weathered sandstone ashlar blocks. Natural stone varieties used during these replacements show different responses to a variety of weathering processes which lead to their rapid decay. The decay of the newer stone has been accelerated by use of Portland cement paste as the binding and fill material, instead of the original hydraulic lime-based and cocciopesto-type mortars. The hardened Portland cement paste makes an almost impermeable barrier, with permeability three to four orders of magnitude lower, compared to the original mortars and natural stone. The low permeability of this new alien material results in the accumulation of water-soluble salts (specifically nitrates, but also sulphates and chlorides) in the facing masonry ashlars, with their crystallisation coming in the form of both sub- and efflorescence, as well as the development of various decay forms (blistering, granular disintegration and/or scaling and flaking). The source of the water-soluble salts can be traced back to previous restoration attempts. These included chemical cleaning (black crust removal) by nitric acid, ammonium hydroxide (‘ammonium water’), or ammonium hydrogen carbonate, all which can be linked to high nitrate content in the efflorescence.  相似文献   

12.
对强渗透性地层旋挖钻进成孔混凝土灌注桩质量通病进行了分析,总结此类地层必须重视泥浆护壁质量对混凝土灌注桩施工质量的重大影响,必须重视钻斗的活塞抽吸对孔壁的破坏性,建议其验收标准中增加泥浆护壁质量验收,重视清孔后的孔径验收,不可完全沿用与旋挖钻孔泥浆护壁效果有着天壤区别的回转钻、潜水钻成孔混凝土灌注桩的质量验收标准。  相似文献   

13.
Conway Castle is an immense historical structure, dating back to 1289 AC. It was built on highly dipping thickbeds of indurated shale (argillite) and sandstone. It is surrounded by Conway Bay, railway lines, and tall dense forests indicating high relative humidity and rainfall in this coastal area. The castle suffers from weathering noted as honeycomb, black crust, exfoliation, and discoloration with white salt efflorescence at some parts; these are diagnostic features for salt weathering as confirmed by the laboratory investigations using scanning electron microscopy, X-ray diffraction (XRD), point XRD, and hydrochemical analysis. The salt is found to be from three sources, namely, water spray from Conway Bay that is part of the Irish Sea, chemical alteration of the mortars carbonate content into sulfate salts by acid rain, and wet deposition of air pollutants on the surface of the stone. The cracks noted in the southwestern tower of this castle are a result of landslides in this area that resulted from three factors: (a) high dip angle of the indurated sandstone and shale thickbeds (about 60–65° to the south) under this castle, (b) undercutting of these beds in the dip direction by the surface water of Conway Bay, and (c) seismic waves generated by the trains passing close to this castle. All these factors result in land sliding even at a low rate; however, the net result is cracks in the tower close to these factors.  相似文献   

14.
人们在开采使用矿产资源的同时,堆弃大量含有硫化物的废弃矿石和废渣于周围环境中。矿山环境中因硫化矿物氧化,导致采矿产生大量的酸性矿坑排水。这种水体具有低pH值,高电导率,高硫酸根和高重金属含量的特征。酸性矿坑排水对下游水生生物及植物等具有很强的毒性,大量排放引起的环境问题受到广泛关注。为了了解酸性矿山排水对流域水体和土壤的影响,本文选择位于贵州省西南部兴仁的一个典型废弃煤矿区进行研究,通过测定矿坑排水、水库水、河水的pH值和EC,以及土壤的pH值,分析矿坑排水、地表水以及土壤pH值的空间变化情况,在此基础上对矿坑排水对流域酸化的影响进行了综合评价。调查结果表明,酸性矿坑排水和受其影响的水库水体的电导率很高,且pH值均小于3。研究区域地表水（水库水、河水）本底水化学类型为Ca2+-HCO3-型,其pH值在7左右,反映了流域内有碳酸盐岩广泛分布的自然环境特征。当受到酸性矿坑排水影响后,水化学类型转变为Ca2+-SO42-型,pH值则低于4.0。通常,酸性矿坑排水在流动过程中与河床的碳酸盐岩发生中和反应,促使水体的pH升高。野外考察发现,研究区河道中碳酸盐岩中空易碎,其CaCO3成分因长期与酸性矿山排水发生反应而被耗尽。同时,在氧化条件下,酸性矿坑排水中的铁在流动过程中生成大量的氢氧化物覆盖了沿程的河床。这种覆盖作用抑制了酸性矿山排水进一步与碳酸盐岩发生中和反应。因此,在研究区分布有广泛的碳酸盐岩情况下,受酸性矿坑排水影响的河水到下游5 km处仍保持较低的pH值。研究区的主要农作物是水稻,其灌溉水源主要是水库水。为了了解酸性矿坑排水对土壤的影响,对水库下游流域土壤pH值的空间分布进行普查,统计其出现的频率。结果表明,以受酸性矿坑排水影响的水库水作为灌溉水源的土壤,其表土的pH值较低,平均值在5.0左右。反之,土壤表土的pH值平均值在6.5左右。此外,通过对受到酸性矿坑排水影响显著的土壤进行剖面调查,发现从地表到深度90 cm的土壤的pH值均小于4.0。结合受酸性矿坑排水影响的河水pH值普遍偏低的情况可以推测流域酸化与酸性矿坑排水有密切关系。   相似文献   

15.
New and more complete compositional data are presented for a large number of water samples from the Lake Magadi area, Kenya. These water samples range from dilute inflow (<0.1 g/kg dissolved solids) to very concentrated brines (>300 g/kg dissolved solids). Five distinct hydrologic stages can be recognized in the evolution of the water compositions: dilute streamflow, dilute ground water, saline ground water (or hot spring reservoir), saturated brines, and residual brines. Based on the assumption that chloride is conserved in the waters during evaporative concentration, these stages are related to each other by the concentration factors of about 1:28:870:7600:16,800.Dilute streamflow is represented by perennial streams entering the Rift Valley from the west. All but one (Ewaso Ngiro) of these streams disappear in the alluvium and do not reach the valley floor. Dilute ground water was collected from shallow pits and wells dug into lake sediments and alluvial channels. Saline ground water is roughly equivalent to the hot springs reservoir postulated by Eugster (1970) and is represented by the hottest of the major springs. Saturated brines represent surficial lake brines just at the point of saturation with respect to trona (Na2CO3.NaHCO3.2H2O), while residual brines are essentially interstitial to the evaporite deposit and have been subjected to a complex history of precipitation and re-solution.The new data confirm the basic hydrologic model presented by Eugster (1970) which has now been refined, particularly with respect to the early stages of evaporative concentration. Budget calculations show that only bromide is conserved as completely as chloride. Sodium follows chloride closely until trona precipitation, whereas silica and sulfate are largely lost during the very first concentration' step (dilute streamflow-dilute ground water). A large fraction of potassium and all calcium plus magnesium are removed during the first two concentration steps (dilute streamflow-dilute ground water-saline ground water). Carbonate and bicarbonate are the dominant anions, and mechanisms by which they are extracted from the solution include precipitation of alkali and alkaline-earth carbonates, and degassing, as well as precipitation and re-solution of efflorescent crusts. Much sulfate is apparently lost from solution by sorption as well as subsurface reduction.Seasonal runoff, principally from the valley floor north of Lake Magadi, is considered to be the principal recharge to the Magadi ground water system. Evaporative concentration is the overall process responsible for the chemical evolution of the brines. This includes not only simple evaporation, but also mineral precipitation as films and cements in the unsaturated zone, re-solution, and reprecipitation of efflorescent crusts, with consequent recycling of salts. In fact, a large fraction of the solutes are acquired through dissolution of efflorescent crusts.Data were obtained for borehole brines from as deep as 297 m. They show the existence of two distinct brine bodies below the present lake, one shallow, coexistent with bedded salts, and highly concentrated (260 g/kg average dissolved solids), and the other deeper in lacustrine sediments or fractured lavas, and only half as concentrated.  相似文献   

16.
The treatment of landfill leachate by reverse osmosis (RO) generates huge volumes of heavily polluted concentrate that has to be properly treated before its discharge into the environment. The aim of this work was to assess the solidification/stabilization (S/S) treatment of the leachate concentrate (LC) for chemical/physical immobilization of contaminants and for obtaining durable monolithic matrix suitable for storage, landfilling, or use. In addition, the possible use of brick waste as a partial replacement of natural aggregates used for S/S process was investigated. Concrete mixtures were prepared using local PC, sand, gravel, and tap water/LC. The substitution of coarse aggregate material by brick waste was examined for the replacement ratios 25, 50, and 75%. Hardened concrete specimens were subject to compressive test as well as flexural strength test at 7 and 28 days. Besides, a leaching test was performed, and the collected eluates were analyzed for pH, total dissolved solids, chemical oxygen demand, chlorides, sulfates, phosphorus, and heavy metals. The aggregate replacement with brick waste showed various trends according to the substituted fraction size and ratio. A 28-day compressive strength of more than 25 MPa was obtained even at 50% simultaneous substitution of PC, gravel, and sand. Leaching test analysis confirmed that S/S could be a successful treatment for RO LC decreasing most of the pollutants to comply with landfilling criteria, except for chromium known to be mobile at high pH. Furthermore, the substitution of natural aggregates with brick waste revealed the possibility to cast valuable masonry units. However, a long-term assessment is still needed to ensure the mechanical and chemical stability/durability of concrete.  相似文献   

17.
《Organic Geochemistry》1999,30(8):947-952
Three soil samples polluted by PAH were assessed for both acute (Vibrio fischeri [Microtox® test], Daphnia magna, Thamnocephalus platyurus) and chronic (Pseudokirchneriella subcapitata) toxicity, as well as for genotoxicity (Vibrio fischeri M169, [Mutatox® test]). Bioassays were performed on soil water leachates and on soil solvent extracts to characterise not only the fraction of water soluble pollutants but also to evaluate less soluble and soil-bound pollutants. The toxicity of the water leachates was low to moderate (from 0 to 30 toxic units) whereas the toxicity of the methanol extracts was about 100 to 10,000 toxic units. Although only slightly toxic, the genotoxicity of water leachates was clearly demonstrated. This finding shows that acute and chronic toxicity assays alone may not be sufficient to characterize soil hazards. A step procedure to characterise soil ecotoxicity is therefore proposed which allows one to study the pollutant mobility, toxicity and genotoxicity. It can be used to identify the hazard, to classify soil hazards and thus map contaminated sites, to assess the success of treatment and finally to monitor rehabilitated sites.  相似文献   

18.
Osheepcheon Creek running through the Dogyae area is being polluted by the influx of the abandoned coal mine drainage. Generally, the more polluted water has lower pH and Eh and higher conductivity values. The concentrations of Mg, Ca, Fe, SO4, and some trace elements, such as Cd, Co, Cr, Mo, Ni, Pb, Rb, Sr, U and Zn, are tens to hundreds of times more concentrated in the abandoned coal mine drainage than in the unpolluted streamwater. However, most immobile toxic pollutants from the mine drainage are quickly removed from the streamwater by the precipitation of amorphous Fe hydroxide and sorption on the precipitated Fe hydroxide. The fast removal of the pollutants from the streamwater maintains the water quality of the creek as acceptable at most places along the stream path, except where the abandoned coal mine drainage flows in. However, the creek has the potential of deteriorating quickly if the mine drainage is allowed to be continuously combined with the streams. A function of pH, Eh, and conductivity has been developed with discriminant function analysis for the purpose of easy, fast, and inexpensive measurement of the degrees of pollution of the streams. The estimated pollution of the streams with the discriminant function are consistent with what the chemical compositions of the water samples indicate. The pollution map of the study area was constructed from the calculated scores with the discriminant function. The pollution map suggests that the pollutants mainly come from the west side of Osheepcheon Creek. Thus, the abandoned coal mine drainage from the west side has to be appropriately treated as soon as possible to prevent Osheepcheon Creek from being further polluted. Considering the topography, climate, and the amount of the mine drainage, an active treatment method is recommended.  相似文献   

19.
Hyblean limestone of Oligo-Miocene age was widely used as a construction material in the architectural heritage of Eastern Sicily (Italy). Among them, the so-called Pietra Bianca di Melilli (Melilli limestone) and Calcare di Siracusa (Syracuse limestone) were prized for their attractive appearance, ease of quarrying, and workability. Syracuse limestone shows general weathering, whereas Melilli limestone is better preserved, and only differential erosion or superficial exfoliation can be detected in monuments. The cause of the different behavior of these two limestones was investigated from the petrographic and petrophysical points of view. The saturation coefficient is higher in Melilli limestone, and ultrasound measurements indicate that it is less compact than Syracuse limestone, so that Melilli limestone could deteriorate more easily than Syracuse limestone. However, pore interconnections and the size of very small pores play the main role in the durability of both materials. The “irregularity” of the Syracuse pore system and its greater number of micropores hinder water flow through the exterior, promote stress in pore structure, and favor the development of scaling, as confirmed by salt crystallization tests. In Melilli limestone, the low concentration of micropores and fast water evaporation allow solutions to reach the surface more easily, resulting in less damaging efflorescence.  相似文献   

20.
《Applied Geochemistry》1999,14(1):53-65
Owens Lake in SE California became essentially dry by the 1920s after the Los Angeles Aqueduct was constructed and diversion of water from the Owens River began. Frequent dust storms at Owens Lake produce clouds of efflorescent salts which present human health hazards as a result of their small particle size and elevated concentrations of As and SO4. This study was conducted to characterize the evolution of major elements in ground water in eastern Owens Lake and to examine the factors controlling the concentrations of dissolved As and F. Evapoconcentration of shallow ground waters at the lakebed surface produces high pH, high alkalinity brines with major ion compositions that are consistent with those predicted by the Hardie–Eugster Model. Evaporite minerals identified in the surface salts using XRD were halite (NaCl), thenardite (Na2SO4), trona (Na3H(CO3)2·2H2O), pirssonite (Na2Ca(CO3)2·2H2O), and nesquehonite (MgCO3·3H2O). Significant correlations between both As and F with Li in shallow ground waters indicate that As and F are not partitioned into surface salts until very high salinities are reached (>9.0 m). Leaching experiments show that As and F can be readily released from lakebed salts when exposed to natural precipitation. Conservative behavior of As and F results from the high pH values and low Ca activities of shallow ground waters that contribute to: (1) redox stability of As(V) even at moderately reducing conditions, (2) a decrease in the adsorption affinities of As and F to mineral surfaces, (3) undersaturation with respect to fluorite (CaF2(s)).  相似文献   

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