Bioconcentration of polycyclic aromatic hydrocarbons in roots of three mangrove species in Jiulong River Estuary

The polycyclic aromatic hydrocarbons(PAHs) concentrations were determined in the root of three mangrove species(Kandelia candel, Avicennia marina and Bruguiera gymnorrhiza) and their growing environment(sediment) in mangrove wetlands of Jiulong River Estuary, Fujian, China. The total PAHs(16 parent PAHs) in mangrove sediments ranged from 193.44 to 270.53 ng/g dw, with a mean value of 231.76±31.78 ng/g dw. Compared with other mangrove and coastal marine sediments, the PAHs concentrations of all the sampling areas in this study were at relatively lower level. The total PAHs(13 parent PAHs) values varied from 30.83 to 62.73 ng/g dw in mangrove roots. Benzo[a]pyrene(five-ring), fluoranthene(four-ring) and pyrene(four-ring) dominated in mangrove sediments. Based on ratios of phenathrene/anthracene, fluoranthene/pyrene and fluoranthene/pyrene + fluoranthene, the main possible sources of surface sediment PAHs were identified as grass, wood or coal combustion for mangrove wetlands of Jiulong River Estuary. Naphthalene(two-ring) and phenathrene(three-ring) were the most abundant compounds in mangrove roots. Sediment-to-vegetation bioconcentration factors(BCF SV s) were calculated and their relationships with PAHs' physico-chemical properties were investigated. The average BCF SV s of PAHs for three mangrove species roots were almost all under the level of 1 except for naphthalene. Good linear relationship between BCF SV values for mangrove roots and PAHs water solubility, octanol-water partitioning coefficients was derived in present study. The solubility and the octanol-water partition coefficient were proved to be good predictors for the accumulation of PAHs in mangrove roots, respectively.

Late Quaternary diatom and sea level changes in estuarine plain of the Jiulong River

Four units and twenty-four zones of diatom have been discerned in the Borehole ZK5 in the estuarine plain of the Jiulong River, Fujian Province. Comprehensive analysis of these, together with microbiological assemblages and age determinations in some other boreholes, shows that during the Late Wurm Glacial, sea level of the study area rose and fell frequently, but had principally been in the environments of estuary-bay. This mainly resulted from the tectonic subouction. In this period 3 low sea levels occurred. at 18, 16 and 12 kaBP respectively. During Holocene, sea weter intruded massively and the sea level over the transgnaion maximum had been 5-10 m higher than that of the present.

Distribution and number change of the Littorinidae (Gastropoda) on intertidal hard bed in the Jiulong River Estuary

There are 4 species of Littorinidae on the intertidal hard bed in the Jiulong River Estu-ary. They are Littorina scabra, L. brevicula, Nodilittorina pyramidalis pyramidalis and N.millegrana. Of these species, L. scabra is a dominant species. According to the results of in-vestigation, we find distribution patterns of the Littorinidae on intertidal hard bed in theestuary as follows: (1)There is no Littorinid species at Haicheng Station. (2)There is only Lit-

Qeochemical behaviour of iodine in Jiulong River Estuary

Dissolved iodine species and the relationship between its distribution and salinity in Jiulong River estuarine water have been determined. It has been found that the total iodine, iodate and iodide are positive linear with salinity. This indicates that dissolved iodine species (IO-3 and I- ) in estuarine water .how conservative behaviour. The river water contains 2. 40μg/1 as iodide and less than 1. 0μg/1 as iodate, and iodide is the predominant species. Whereas the sea water contains 39. 4μg/1 as iodate and 4. 00μg/1 as iodide, and iodate is the dominant form. The distribution of dissolved iodine in pore water, as a function of depth, has been studied. Iodine in pore water occurs as iodide. The apparent fluxes of soluble iodine from the sediment to the overlying water in the estuary have been determined. The values are 2. 4 (15℃) and 27μmol/(m2·d) (30℃) respectively.

Characteristics of nutrients in the Jiulong River and its impact on Xiamen Water, China

Water samples were collected at 20 sites on 4 occasions in 2009(twice in May,and once in both August and November) along the Jiulong River,South China to examine how nutrient inputs from the Jiulong River could affect the nutrient status of the Xiamen Water.Samples were analyzed for nitrite(NO2-N),nitrate(NO3-N),ammonium(NH4-N),phosphate(PO4-P),silicate(SiO3-Si),salinity,and temperature,to determine the nutrient and trophic status of the river.The results indicate that nutrients are derived mainly from river runoff.NO3-N was the main form of DIN in most parts of the river.In addition,NO3-N,DIN,and SiO3-Si behave conservatively.There is a surplus of DIN and SiO3-Si in the river,and PO4-P is a limitation on phytoplankton growth.The concentration of DIN is typically above 0.60 mg/dm3,and higher than 1.00 mg/dm3in most parts of the river.The concentration of PO4-P is typically above 0.02 mg/dm3,while the concentration of SiO3-Si is higher than 1.00 mg/dm3.Between 2003 and 2008,samples were collected 3 times per year(May,August and November) at 27 sites in the Xiamen Water and analyzed for NO2-N,NO3-N,NH4-N,PO4-P,salinity,and temperature.We discovered that the Jiulong River was the key source of DIN into the Xiamen Water,but not PO4-P,indicating the reason of the N/P molar ratio imbalance in the Xiamen Water.In the future,the effects of high DIN concentrations on the phytoplankton communities and marine ecosystems of the Xiamen Water shall be studied.

Dynamics of phytoplankton communities in the Jiangdong Reservoir of Jiulong River,Fujian,South China

Phytoplankton blooms occurring in the Jiangdong Reservoir of Jiulong River,Fujian Province,South China,are a potential source of contamination of the drinking water of Xiamen(Amoy)City.To understand the main factors governing phytoplankton composition and succession,we sampled phytoplankton and measured environmental parameters in the reservoir,weekly or biweekly from Jan.2010 to Feb.2012.We identifi ed 123 species of phytoplankton from 7 phyla and 74 genera.The major phyla were Chlorophyta,Bacillariophyta,Cryptophyta,Cyanophyta,and Dinophyta.The main trend in the succession of phytoplankton was from prevalence of Cryptophyta-Bacillariophyta communities to those of Chlorophyta-Cyanophyta.High cell concentrations of Cryptophyta,predominantly Komma caudate,Cryptomonas marssonii,and Cryptomonas erosa,were present in winter,associated with low river discharge and cold water.Bacillariophyta,primarily Cyclotella meneghiniana,Aulacoseira granulata,and Aulacoseira granulata var.angustissima,dominated in early spring,coinciding with high turbulence and low irradiance.During early summer and autumn,Chlorophyta,comprising Scenedesmus quadricauda,Dictyosphaerium ehrenbergianum,and Pandorina sp.were prevalent during conditions of warmer water temperatures and low turbulence.Cyanophyta,with dominance of Pseudanabaena mucicola,Merismopedia tenuissima and Raphidiopsis sp.increased throughout the summer,coinciding with higher water temperatures and lower nutrient concentrations.Dinophyta content was occasionally high during winter and summer.Peridiniopsis penardii(Dinophyta)bloomed during winter 2009,with a persistently high biomass recorded into early spring.Canonical correspondence analysis indicated that phytoplankton communities were infl uenced by river discharge,irradiance,water temperature,and nutrient concentrations.

Stable isotope geochemical characteristics of dissolved inorganic carbon in the Jiulong River Estuary, Fujian Province, China

The isotopic composition of dissolved inorganic carbon(DIC) in estuarine environments has been studied for its significant role in determining the isotopic composition of inorganic/organic matter and its applications to the study of various natural processes. In this paper, based on the stable isotope geochemical characteristics of dissolved inorganic carbon in the Jiulong River Estuary, the following conclusions are drawn:(1) δ13CDIC values are mainly controlled by the mixing ratio of fresh water and sea water;(2) δ13Cphytoplankton values are linearly related to the δ13CDIC values;(3) δ13CPOM values for the Jiulong River Estuary are affected by anthropogenic pollution significantly; and(4) the comprehensive analysis of δ13Cphytoplankton, δ13CPOM and δ13CDIC shows that along with increasing salinity, the proportion of POM derived from the degradation of phytoplanktons gradually increases.

Fast acclimation of phytoplankton assemblies to acute salinity stress in the Jiulong River Estuary

Mixing of freshwater and seawater creates the well-known salinity gradients along the estuaries. In order to investigate how phytoplankton respond to the acute salinity changes, we exposed natural phytoplankton assemblies from the Jiulong River Estuary to differential saline field water while continuously monitoring their photosynthetic performances under both indoor-and outdoor-growth conditions. When the natural cell assemblies from salinity 30 field water were exposed to series low saline field water(salinity 25, 17, 13 and 7.5), the effective Photosystem II quantum yield(ΔF/Fm′) decreased sharply, e.g., to one-fifth of its initials after 5 min exposure to salinity 7.5 field water, and then increased fast during the following 40 min and almost completely recovered after 320 min. During such an exposure process, non-photochemical quenching(NPQ) sharply increased from 0 to 0.85 within 5 min, and then decreased to nearly 0 within the following 70 min. When these cells re-acclimated to salinity 7.5 field water were exposed to series high saline field water(salinity 13, 17, 25 and 30), a similar response pattern was observed, with the decreased ΔF/Fm′ accompanied with increased NPQ, and followed by the recovery-induced increase in ΔF/Fm′ and decrease in NPQ. A similar response pattern as ΔF/Fm′to the acute osmotic stress was also observed in the photosynthetic carbon fixation capacity according to radiocarbon(14C) incorporation. Our results indicate that estuarine phytoplankton assemblies could rapidly recover from the acute osmotic stress, implying a potential cause for their frequent blooms in coastal-estuarine waters where despite drastically varying salinity, available nutrients are abundant due to the land-derived runoffs or mixing-caused relaxations from sediments.

Characteristics of Heavy Minerals Composition and Distribution in Jiulong River Estuary Sediment

The bottom sediment samples were gathered during island investigation in 1994 and in the period of carrying out the natural science fund project of Fujian in 1999. The composition, distribution and assemblage characteristics of heavy minerals which granularity distributes from 0.063 to 0.125 mm in the sediment from Jiulong River estuary are studied in the paper. The results show that there are 49 kinds of heavy minerals and the average content of them is 9.38 %. The dominant and characteristic minerals are magnetite, hematite, epidote, ilmenite, limonite, hornblende, zircon, andalusite, biotite and so on. 4 mineral assemblage ⅠⅡzones (.The watercourse gateway of Jiulong River mineral zone, . The northern estuary ⅢⅣof Jiulong River mineral zone, . The southern estuary mineral zone, . The eastern estuary of Jiulong River mineral zone ), can be divided based on the heavy mineral contents and the distribution characteristics, which not only relates to the matter sources but also is controlled by hydrodynamic condition and the sedimentary environment in the Jiulong River estuary.

Distribution,fluxes and decadal changes of nutrients in the Jiulong River Estuary,Southwest Taiwan Strait

The Jiulong River Estuary (JRE) is a typical subtropical macro-tide estuary on the southwest coast of the Taiwan Strait (TWS),which has been greatly impacted by human activities over the past 30 years.To understand nutrient dynamics and fluxes under such a heavy background of anthropogenic perturbation,eight cruises were conducted from April 2008 to April 2011,covering both wet (May to September) and dry (October to April next year) seasons.Nutrient concentrations were very high for the freshwater end-member in the upper reach of the JRE (nitrate (NO 3-N):120-230 mol L-1 ;nitrite (NO 2-N):5-15 mol L-1 ;ammonium (NH 4-N):15-170 mol L-1 ;soluble reactive phosphorus (SRP):1.2-3.5 mol L-1 ;dissolved silicate (DSi):200-340 mol L-1).In dry seasons,concentrations of these nutrients were higher than in wet seasons.Nitrate was the dominant chemical species of dissolved inorganic nitrogen (DIN),with percentages of 67%-96% in wet seasons and 55%-72% in dry seasons.Distributions of NO 3-N and DSi against salinity were nearly constant during all cruises,and showed generally conservative mixing behaviors in the estuary (1<Salinity<32).The concentrations of SRP varied within a narrow range of 1.0-2.0 mol L-1 in low/middle salinity areas,and they were quickly diluted by relatively oligotrophic near-shore seawater in the high salinity region.Based on a temporally high-resolution water discharge dataset,riverine fluxes of DIN,SRP and DSi into the JRE were calculated at 34.3 10 3 t N a 1,0.63 10 3 t P a-1 and 72.7 10 3 t Si a-1,respectively.In comparison,estuarine export fluxes of DIN,SRP and DSi from the JRE to the TWS were estimated at 34.8 10 3 t N a-1,0.82 10 3 t P a-1 and 71.6 10 3 t Si a-1.The estuarine addition flux of SRP was independently estimated at 0.16 10 3 t P a-1.In comparison with major world rivers,the Jiulong River shows a very high areal yield rate of NO 3-N.In comparison with historical datasets from 1980s-1990s,concentrations of NO 3-N and SRP increased 2-3 times in upper/middle areas of the JRE,while DSi remained at the same level.The latter is much different from decadal nutrient changes in the Mississippi River and the Yangtze River/Estuary.Such nutrient changes may fundamentally contribute to recent red tide events in the JRE and adjacent Xiamen Bay.

九龙江口表层沉积物碘含量分析

于2021年5—6月对九龙江红树林保护区与非红树林保护区进行布点采样,测定其表层沉积物碘含量和有机碳含量。结果表明:13个采样点中,碘含量范围为3.7~24.8 mg·kg^(-1),差值最高可达7倍,平均值为12.3 mg·kg^(-1);有机碳含量范围为16~45 g·kg^(-1),平均值为30 g·kg^(-1)。不同类型样品碘含量大小依次为:长林龄林下沉积物>河道清淤沉积物>非林下沉积物>短林龄林下沉积物,其中长林龄林下沉积物碘含量范围为15.7~24.8 mg·kg^(-1),平均值为19.2 mg·kg^(-1);短林龄林下沉积物含量为5.5~6.9 mg·kg^(-1),平均值为6.2 mg·kg^(-1);二者相差3倍以上。有机碳含量最高的为长林龄林下沉积物和河道清淤沉积物,平均值均为32 g·kg^(-1);最低值为短林龄沉积物,含量为22 g·kg^(-1)。不同类型沉积物有机碳含量与碘含量基本呈正相关关系,但相关性不显著;同等有机碳含量的样品,长林龄林下沉积物碘含量显著高于其它样品。

九龙江流域丰枯水期表层水体氮污染特征及其来源解析

为探明九龙江流域表层水体氮污染分布特征及其污染来源,于2020年7月(丰水期)和2021年1月(枯水期)开展九龙江全流域表层水体多点多断面原位观测,利用正定矩阵因子分析模型(positive matrix factorization,PMF)对不同水期全流域表层水体氮污染来源及贡献率进行解析,耦合相关性统计分析方法研究不同水期流域表层水体氮污染的关键驱动因子。结果表明,九龙江流域表层水体氮污染存在明显的水期分异特征,ρ(TN)为0.72~13.14 mg·L^(-1),丰水期ρ(TN)为1.39~10.95 mg·L^(-1),枯水期为0.72~13.14 mg·L^(-1)。硝态氮(NO_(3)^(-)-N)、氨氮(NH_(4)^(+)-N)、亚硝态氮(NO_(2)^(-)-N)和溶解性有机氮(DON)浓度均表现为丰水期大于枯水期,但颗粒态氮(PN)浓度则表现为枯水期大于丰水期。丰水期氮污染以NO_(3)^(-)-N、NH_(4)^(+)-N和DON形态为主,枯水期则以NO_(3)^(-)-N、DON和PN形态为主。应用PMF模型对流域表层水体氮污染来源进行解析,结果表明,丰水期流域农业化肥施用引起的农业面源污染、生活污水及河流内动植物残体、微生物、矿物颗粒是流域水体氮污染的主要来源,而枯水期流域农业化肥污染、城市工业污水排放及河流中动植物残体等悬浮颗粒则是流域水体氮污染的主要来源。该结果强化了丰枯水期九龙江流域表层水体氮污染受流域农业生产活动和径流变化共同影响的认识,建议将流域农业、工业生产氮污染源头控制和氮污染的水期分异有效纳入流域水体氮污染综合管理。

基于时序InSAR的九龙江河口地区地面沉降时空演变规律及成因分析

为探明九龙江河口地区地面沉降情况,本研究采用小基线集合成孔径雷达干涉测量(small baseline subset interferometric synthetic aperture radar, SBAS-InSAR)和永久散射体合成孔径雷达干涉测量(persistent scatterer interferometric synthetic aperture rader, PS-InSAR)技术获取了2017年1月至2022年3月地面沉降的时空分布信息和演变规律,并结合实地调查数据和水文地质调查监测资料对地面沉降成因进行了系统分析。研究结果表明:SBAS-InSAR和PS-InSAR两种方法均发现在研究期间九龙河口地区地面整体呈现出沉降趋势,SBAS-InSAR监测结果发现研究区沉降速率为6.2 mm/a;研究期间该区域的沉降中心持续扩大且沉降量呈增加趋势,最大累积沉降量达到250 mm以上,主要分布在浮宫镇中南部地区、海澄镇、东园镇中南部地区、角美镇和榜山镇东南部地区;该区域由于大量抽取地下水用于养殖,地下水位下降,引起淤泥层发生固结排水、压密,从而导致地面沉降。

水体微塑料的垂向分布及采样方法比较研究——以九龙江河口为例

由于受到潮汐过程的影响,河口区微塑料的调查和研究存在着方法不统一、数据误差较大的问题.2019年夏季使用泵采法在九龙江河口开展原位全水层微塑料采样,对不同水层、不同站位间的微塑料丰度及其赋存特征进行分析,并与其他在该河口的相关调查研究结果进行对比.结果表明:九龙江河口表、中、底层水体中的微塑料赋存量存在明显差异,河流入海口及靠近污染源处表层水中微塑料丰度明显高于中、底层中,在潮汐作用剧烈的河口区,中、底层中微塑料丰度高于表层水中,存在明显分层现象;使用不同采样方法获取的微塑料数量浓度值存在较大差异,泵采法相比拖网法能更有效地截留塑料纤维;使用泵采法过滤水样体积、滤经筛网孔径大小都对收集到的微塑料丰度、尺寸有显著影响.采样方法的不同将导致微塑料丰度结果的显著差异,在潮汐河口进行微塑料监测有必要将潮汐作用考虑在内.因此,建议建立潮汐河口的微塑料业务化监测和通量观测,并采用洪、枯季,大、小潮的全潮时段的观测采样方法.

九龙江流域生态需水量时空变化趋势分析

为了维持和保护流域生态系统健康,避免流域生态环境退化,进行流域生态需水量的确定和研究是有必要的。根据九龙江2000—2018年2个水文站实测数据,结合Tennant法确定河道内生态基流,选择面积定额法,利用流域内土壤质地分布状况,以及基于遥感开发的MCD12Q1土地利用产品和MOD16A2蒸散发产品估算植被生态需水量,并对区域生态环境需水量进行时间变化趋势分析和空间分布分析。结果表明:(1)在2000—2018年,九龙江流域有林地、草地面积整体呈现增加趋势,农田、疏林地面积呈现下降趋势;(2)九龙江流域内北溪、西溪河道内多年平均生态需水量分别为22.68亿m3,10.67亿m3,植被多年平均生态需水量为105.27亿m3;(3)有林地、草地的生态需水量呈显著上升趋势,疏林地、农田生态需水量呈下降趋势,前者显著,后者不显著。受人类活动影响,九龙江流域土地覆盖/利用类型年际变化剧烈,因此在区域生态需水量变化中其作用不可忽略,随着遥感/GIS技术的发展,对土地覆盖/利用类型以及植被蒸发量的高时空分辨率观测变得可能,有助于准确预测区域生态需水量。

九龙江口潮下带春季小型底栖动物分布及优势类群海洋线虫的群落结构分析

小型底栖动物世代周期短,对环境的变化较为敏感,是海洋环境质量评估中重要的指示生物,其多样性指数和群落分布格局可以作为环境监测的有效工具.为了解福建省九龙江口小型底栖动物分布及多样性,于2018年4月(春季)在九龙江口潮下带沿着盐度梯度设置11个站位,进行小型底栖动物类群、密度以及自由生活海洋线虫(简称海洋线虫)多样性及群落结构分析,结果共鉴定出9个小型底栖动物类群,分别是海洋线虫、桡足类、多毛类、寡毛类、动吻类、端足类、介形类、双壳类、纽虫,以及其他类.小型底栖动物和海洋线虫的平均密度分别为(323±404)ind/(10 cm^(2))和(292±414)ind/(10 cm^(2)).此外共鉴定出海洋线虫58属,主要优势属有Daptonema、Desmodora、Sabatieria、Parodontophora、Spilophorella和Neochromadora.海洋线虫主要摄食类型为非选择性沉积食性者和刮食者.地理位置接近的站位,海洋线虫群落结构也较相似,部分站位平行样间呈现较高的群落结构空间异质性.根据海洋线虫的各项生物变量进行九龙江口生态质量状况评价,结果表明近河口和远河口的环境受到污染或扰动较大.盐度低的站位其生物多样性指数也低,盐度可能是影响海洋线虫群落结构的重要环境因子.

福建九龙江流域历史旱涝急转的识别与情势分析

为完善九龙江流域应对极端水文事件和旱涝急转的调度预案,根据九龙江流域历史观测资料,利用短周期降雨旱涝急转指数SDFAI与标准差法对九龙江流域旱涝急转的历史典型年进行识别并分析。研究结果表明:①1952—2021年,九龙江流域的旱涝急转典型年共计11 a,年份分布较均匀,近十年的旱涝急转典型年为2016、2020年;②九龙江流域四季旱涝转移的概率特征为在干旱情况下,由旱转涝的概率小于连旱的概率,在洪涝情况下,由涝转旱的概率大于连涝的概率;③对九龙江流域旱涝急转历史典型年1987、1995、2016年的水文情势进行了分析,将典型年的降雨量、蒸发量与常年量作对比,得到了其逐月变幅情况,为制定旱涝急转应急调度方案提供数据支撑。

九龙江河口水体粪类有机质污染时空变化特征研究

河口是陆源污染物入海的主要通道,在全球气候快速变化和人类活动加剧的背景下,河流入海污染物通量急剧增加,导致河口、海湾及其周边海域水体污染、生态受损等严峻的环境问题发生。本文选取了受极端事件和人类活动影响显著的我国东南强潮型的九龙江河口,利用粪甾醇有机标志物手段开展河口环境粪类污染示踪研究,探讨九龙江河口区粪类污染物(“源”)进入河流后的入海行为(“到”),揭示粪类有机质在近河口海域时空分布特征及受控因素(“汇”)。研究发现,不同季节的河口径流过程和潮汐作用影响粪类有机污染物的时空分布,潮汐过程对中上游河口区水体环境中粪甾醇的赋存影响较大,呈现高潮低浓度而低潮高浓度的潮周期变化特征;河口区粪甾醇在陆−海输运过程的赋存特征还受控于最大浑浊带复杂的水体和沉积动力过程,对粪类有机污染物有一定的净化作用;研究还通过对比人为源贡献主导的氨氮等河流输入的营养盐说明粪甾醇在河口区的时空分布特征与人类活动密切相关。

九龙江河口咸淡水混合过程中汞的额外增加与消除

河口是海陆界面能量和物质交换的重要场所,研究汞在河口的迁移特征及影响因素,对认识汞的生物地球化学行为具有重要意义.本研究测定了九龙江河口区沉积物孔隙水的总汞(total mercury,THg)浓度与汞同位素特征,结合笔者所在课题组已发表的相关研究数据,比较不同季节、不同潮位、降水与否的表层水THg浓度、汞同位素组成与盐度之间的关系,探究影响表层水中汞额外增加/消除的因素及机制.结果表明:(1)孔隙水THg浓度[(38.28±28.80)ng/L,n=28]显著高于表层水[(8.53±6.85)ng/L,n=35](P<0.01);孔隙水THg浓度受季节或径流量变化的影响不明显.孔隙水δ^(202)Hg平均值(-1.24‰±0.36‰,n=28)处于表层水(-0.32‰±0.38‰,n=29)和沉积物(-1.99‰±0.69‰,n=18)之间;Δ^(199)Hg平均值(-0.13‰±0.03‰,n=28)低于表层水(-0.04‰±0.10‰,n=29)和沉积物(-0.04‰±0.16‰,n=18),表明汞在孔隙水与沉积物间的双向传递与吸附及非光致氧化过程有关.(2)枯水期河口区表层水中的汞以额外消除为主,呈现汞“汇”特征;丰水期则呈现汞“源”特征.当咸淡水在河道较浅处交汇时,表层水中汞的额外增加更大.无论是增加或消除,表层水中汞的δ^(202)Hg与Δ^(199)Hg值均升高.汞在咸淡水交汇界面的迁移受径流量、潮位、河道特征及降水事件等多因素影响.(3)枯水期中降水事件发生时表层水THg浓度和汞同位素组成随盐度的变化特征与非降水期不同,表明降水可影响表层水中汞的行为.研究显示,汞在咸淡水交汇界面的迁移受径流量、潮位、河道特征及降水事件等多因素影响,河口是汞“源”也是汞“汇”.