武汉市湖泊水域利用转变及其碳排放影响

考虑到湖泊水域面积与土地面积的相互变迁进程,以及土地利用变化已成为仅次于化石能源燃烧的第二大温室气体排放源的客观现实,首次尝试分析特定区域湖泊水域的变化以及间接产生的碳源碳汇影响。根据2005、2010和2015年遥感影像获取武汉市湖泊水域利用转变的数据,采用国际通用的土地碳排放测算模型,评估武汉市湖泊水域转变为4类用地产生的碳排放量及碳强度变化情况。研究显示:(1)2005～2015年武汉市湖泊水域面积整体减少超10 km~2,且2010年后呈现加速萎缩趋势, 2010～2015年的减少值约为2005～2010年减少值的2.04倍;(2)虽然部分耕地、林地和草地转化为湖泊导致湖泊水域的增加,但湖泊大面积转变为建设用地导致水域面积的显著较少;(3)从碳排放总量来看,变动面积区域内呈碳源区,后5年碳源值是前5年的1.45倍;前后5年湖泊水域变化的碳排放强度分别为0.03和0.04 t/km~2,碳排放强度明显增加。针对武汉市湖泊水域利用的现实状况,提出把"山水林田湖草"放到统一的管理机制中进行考虑、规范土地资源利用、限制建设用地过度扩张等措施。     

退田还湖对鄱阳湖洪水调控能力的影响

利用实测资料统计了鄱阳湖近50年来湖盆形态和洪水水情的变化,表明由于围垦的作用,1954~1992年鄱阳湖面积共减小1 300 km2,容积共减少81×108 m3,调节系数从17.3%下降到13.7%,调洪能力降低20.8%;20世纪90年代与50年代相比,年最高水位平均值抬高1.80 m。计算了退田还湖对近50年来两次特大洪水（1954年洪水和1998年洪水）最高水位的效应值,表明分别可使1954年洪水和1998年洪水的最高水位降低0.72 m和0.68 m。估算了退田还湖对鄱阳湖洪水位频率的影响,表明50年一遇和100年一遇的洪水位分别可降低0.63 m和0.68 m。计算还表明,高水还湖（单退）降低洪水位的作用与圩区还湖前夕的内涝程度密切相关,说明及时排除圩区的内涝对保障退田还湖的防洪减灾作用至关重要。分析了退田还湖面临的主要问题,分别是高水还湖圩区的内涝问题和平垸行洪（双退）圩区的血防问题;探讨解决这两个问题的具体对策,分别为单退圩堤采用“限高加固,排空待蓄”的运作方式,双退圩堤采用“敞开进洪,兼顾血防”的运用方式。     

Perfluoroalkyl carboxylates and sulfonates and precursors in relation to dietary source tracers in the eggs of four species of gulls (Larids) from breeding sites spanning Atlantic to Pacific Canada

In the present study, we identified and examined the spatial trends, sources and dietary relationships of bioaccumulative perfluorinated sulfonate (PFSA; C(6), C(8), and C(10) chain lengths) and carboxylate (PFCA; C(6) to C(15) chain lengths) contaminants, as well as precursor compounds including several perfluorinated sulfonamides, and fluorotelomer acids and alcohols, in individual eggs (collected in 2008) from four gull species [glaucous-winged (Larus glaucescens), California (Larus californicus), ring-billed (Larus delawarensis) and herring (Larus argentatus) gulls] from 15 marine and freshwater colony sites in provinces across Canada. The pattern of PFSAs was dominated by perfluorooctane sulfonate (PFOS; >89% of ΣPFSA concentration) regardless of egg collection location. The highest ΣPFSA concentrations were found in the eggs collected in the urbanized areas in the Great Lakes and the St. Lawrence River area [Big Chicken Island 308 ng/g ww, Toronto Harbour 486 ng/g ww, and Ile Deslauriers (HG) 299 ng/g ww]. Also, eggs from all freshwater colony sites had higher ΣPFSA concentrations, which were significant (p<0.05) in many cases, compared to the marine sites with the exception of the Sable Island colony in Atlantic Canada off the coast of Nova Scotia. C(6) to C(15) chain length PFCAs were detected in the eggs, although the pattern was variable among the 15 sites, where PFUnA and PFTrA dominated the pattern for most colonies. Like the ΣPFSA, the highest concentrations of ΣPFCA were found in the eggs from Big Chicken Island, Toronto Harbour, Ile Deslauriers (HG), and Sable Island, although not all freshwater sites had higher concentrations compared to marine sites. Dietary tracers [δ(15)N and δ(13)C stable isotopes (SIs)] revealed that PFSA and PFCA exposure is colony dependent. SI signatures suggested that gulls from most marine colony sites were exposed to PFCs via marine prey. The exception was the Mandarte Island colony in Pacific British Columbia, where PFSA and PFCA exposure appeared to be via terrestrial and/or freshwater prey consumption. The same was true for the freshwater sites where egg SIs suggested both aquatic and terrestrial prey consumption as the source for PFC exposure depending on the colony. Both aquatic (marine and freshwater) and terrestrial prey are likely sources of PFC exposure to gulls but exposure scenarios are colony-specific.     

Distributions of heavy metals in the surface sediments of the Gulf of Saros, NE Aegean Sea

The Gulf of Saros in the northeastern Aegean Sea (Turkey) is a relatively unpolluted marine environment. There is almost no industry and only small settlements in the surrounding region. The main sources of fresh water and sediment to the Gulf are the Meric River in the northwest and the Kavak Creek in the east. It has an asymmetric bathymetry with a 10-km-wide shelf to the north and up to 15-km-wide, 700-m-deep trough in the south. Water circulation in the Gulf is characterized by longshore currents and anticyclonic eddies. The Black Sea waters, leaving the Sea of Marmara through the Canakkale Strait, are known to enter the southern Gulf during the summer. The surface sediments on the northern shelf consist mainly of sand, whereas those on the slope and the deep trough are mainly silt and clay. The ranges of Fe, Mn, Cu, Zn, Pb, Ni, and Hg contents of the surface sediments from the Gulf of Saros are 0.25 4.60%, 114 1740 ppm, 6-44 ppm, 23-154 ppm, 2-80 ppm, 14-145 ppm, and 10-130 ppb, respectively. These values are low compared to those from the other neighboring marine environments, indicating the pristine nature of the Gulf in terms of metal pollution. However, most metal and organic carbon (Corg) distributions in the Gulf sediments show the effect of anthropogenic and natural inputs to the northwestern and eastern shelf areas from the Meric River and the Kavak Creek and to the deep trough from the Black Sea waters.     

Attributing changes in land cover using independent disturbance datasets: a case study of the Yucatan Peninsula,Mexico

Detailed observations of natural and anthropogenic disturbance events that impact forest structure and the distribution of carbon are essential to estimate changes in terrestrial carbon pools and the associated emissions and removals of greenhouse gasses. Recent advances in remote sensing approaches have resulted in annual and decadal estimates of land-cover change derived from observations using broad-scale moderate resolution imaging spectroradiometer (MODIS) 250 m–1 km imagery. These land-use change estimates, however, are often not attributed directly to a cause or activity and are not well validated, especially in tropical areas. Knowledge of the type of disturbance that caused the observed land-cover changes is important, however, for the quantification of the associated impacts on ecosystem carbon stocks and fluxes. In this paper, we provide estimates of the amount of forest land-cover change in a Mexican forested region and propose an approach for attributing the cause of the observed changes to the underlying disturbance driver. To do so, we collate geospatial and remote sensing data from a variety of sources to summarize statistics about the major disturbances within the Yucatan Peninsula, an “early action” region for the reduction of emissions from deforestation and degradation, from 2005 to 2010. We combine the datasets to develop rules to estimate the likely disturbances that caused the observed land-cover changes based on their spatially explicit location. Finally, we compare our observed disturbance rates to those detected using classified land-cover data derived from MODIS.     

江汉平原湖域拆围监测及其生态环境效益估算研究 ——以洪湖为例

围网及网箱养殖是江汉平原湖泊水体环境污染的重要原因。湖北省湖库拆围大行动实施之后,湖泊围网拆除的成效及其生态环境效益值得关注和探讨。故以湖北省第一大湖洪湖为为例,首先基于改进的归一化差异水体指数（MNDWIn）、纹理分析等方法实现对湖泊拆围效果的快速监测;在提取拆围信息的基础上,根据洪湖水产养殖类型分担率及产排污系数法,对拆围的环境效益进行估算。结果表明：（1）洪湖拆围行动使湖内围网全部被拆除,共拆除湖内围网养殖区面积117.81 km2,自然水面面积增加110.49 km2;洪湖沿岸景观得到了明显改观,其中西部和北部地区拆围效果最为显著,而洪湖南部和北部的湖泊沿岸还存在部分待清理的非水体异质物。（2）洪湖拆围行动使排放到湖泊水体中的污染物减少1 265 284.38 kg,其中植物营养物总氮和总磷的浓度分别减少0.848、0.185 mg/L,这两项指标将由拆围前的Ⅲ类水质提升为Ⅱ类水质,湖泊水体富营养化问题得到较大改善;研究可为区域湖泊管理及流域生态环境保护提供快速监测技术支持和应用参考。     

Nitrogen and phosphorus inputs to the Black Sea in 1970–2050

Increased nitrogen (N) and phosphorus (P) inputs are major causes of eutrophication in the coastal waters of the Black Sea. The objective of this study is to analyze the past and future trends in river export of nitrogen and phosphorus to the coastal waters of the Black Sea and to assess the associated potential for coastal eutrophication. The Global NEWS-2 (Nutrient Export from WaterSheds) model was used for this purpose. Currently, most eutrophication occurs in the North Black Sea and the Azov Sea. In the future, however, this may change. We analyzed trends up to 2050 on the basis of the Millennium Ecosystem Assessment (MEA) scenarios. The results indicate that nutrient loads in rivers draining into the North Black Sea and the Azov Sea may decrease in the coming decades as a result of agricultural trends and environmental policy. However, in these scenarios, the targets of the Black Sea Convention are not met. In the South Black Sea, there is currently little eutrophication. But this may change because of increases in nutrient inputs from sewage in the future.     

Variation of nutrient and metal concentrations in aquatic macrophytes along the Rio Cachoeira in Bahia (Brazil)

The use of cuprous fungicides in cocoa production in the southern part of the state of Bahia (Brazil) for decades has caused an accumulation of copper in various components of the cocoa plantations, and a contamination of regional freshwater ecosystems is suspected. Urban and industrial sources are supposed to contribute to water pollution and eutrophication of the Rio Cachoeira, the main river in this region. In order to study the metal contamination and nutritional status of this freshwater ecosystem, samples of the aquatic macrophytes Eichhornia crassipes and Pistia stratiotes were collected at seven sites along the river course. The samples were analysed for their copper, aluminium, chromium, nitrogen and phosphorus concentrations. The levels of heavy metals increased in the downstream direction, particularly in the roots of water hyacinth. A dramatic increase of nitrogen and phosphorus concentrations in water as well as in plant tissues was found in samples collected downstream from the city of Itabuna. Metal input and eutrophication were attributed to agricultural, industrial and urban sources in the region. Biomonitoring of the water quality using aquatic macrophytes as accumulative indicator plants is recommended in addition to chemical water analyses.     

长江流域国家级保护地空间分布特征及其国家公园廊道空间策略研究

长江流域国家级保护地数量庞大、保护类型多样,为了实现对长江流域自然资源的整体保护和管理的目的,从全域尺度分析其空间分布特征是梳理长江国家公园廊道构建的重要基础。通过数理统计与ArcGIS空间分析,结合中国自然地理表征和人文地理表征,对长江流域现有8类共计996处国家级保护地空间的分布特征进行了研究,结果表明：（1）长江流域国家级保护地总体呈集聚分布,并形成三江源区域、三江并流区域、川西高山高原区域、秦岭中段区域、渝西盆地区域、环洞庭湖区域、环鄱阳湖区域、黄山区域、环太湖区域9个集聚区;（2）长江流域国家级保护地主要集中在中切割高山区和中下游低山丘陵平原区,覆盖了河网密布、水资源丰富、植物种类繁多、土壤肥沃、可达性较高、人口密度适中及经济发展水平较高的东部和中部区域。基于其国家保护地空间分布特征,提出构建“长江源头—入海口”重要保护节点、“洞庭湖—鄱阳湖—巢湖—太湖”重要保护片区、“武当山—华釜山—大凉山、巫山—武陵山—药山”重要保护带的“三重要”模式与“国家公园先行区—国家级保护地聚集区—自然、社会、经济优势区—原生动植物本底”的“四层次”体系相结合的长江国家公园廊道空间策略     

The boundary between European and Asian freshwater ichthyofaunas in the Arctic part of the Polar Urals

The spatial distribution of ichthyofauna in water bodies of the northern Polar Urals is reviewed. Four lake types are distinguished according to the species composition of fishes. The faunistic ranking of water bodies has been performed. The zoogeographic boundary between the ranges of the European and Siberian ichthyofaunas in the freshwater part of the Arctic has been determined.     

Does human activity impact the natural antibiotic resistance background? Abundance of antibiotic resistance genes in 21 Swiss lakes

Antibiotic resistance genes (ARGs) are emerging environmental contaminants, known to be continuously discharged into the aquatic environment via human and animal waste. Freshwater aquatic environments represent potential reservoirs for ARG and potentially allow sewage-derived ARG to persist and spread in the environment. This may create increased opportunities for an eventual contact with, and gene transfer to, human and animal pathogens via the food chain or drinking water. However, assessment of this risk requires a better understanding of the level and variability of the natural resistance background and the extent of the human impact. We have analyzed water samples from 21 Swiss lakes, taken at sampling points that were not under the direct influence of local contamination sources and analyzed the relative abundance of ARG using quantitative real-time PCR. Copy numbers of genes mediating resistance to three different broad-spectrum antibiotic classes (sulfonamides: sul1, sul2, tetracyclines: tet(B), tet(M), tet(W) and fluoroquinolones: qnrA) were normalized to copy numbers of bacterial 16S rRNA genes. We used multiple linear regression to assess if ARG abundance is related to human activities in the catchment, microbial community composition and the eutrophication status of the lakes. Sul genes were detected in all sampled lakes, whereas only four lakes contained quantifiable numbers of tet genes, and qnrA remained below detection in all lakes. Our data indicate higher abundance of sul1 in lakes with increasing number and capacity of wastewater treatment plants (WWTPs) in the catchment. sul2 abundance was rather related to long water residence times and eutrophication status. Our study demonstrates the potential of freshwater lakes to preserve antibiotic resistance genes, and provides a reference for ARG abundance from lake systems with low human impact as a baseline for assessing ARG contamination in lake water.     

Derivation of ecotoxicity thresholds for uranium

Assessment of the risk of impact from most radionuclides is based on the total radiological dose rate to the organism of concern. However, for uranium (U) there can be greater risk from chemical toxicity than radiological toxicity (depending on the isotopic composition). Chemical ecotoxicity of U is dependent on several environmental parameters. The most important are carbonate content, because of the formation of soluble carbonate complexes, and divalent cation content (Ca++ and Mg++), because of their competitive interaction with the uranyl ion (UO2++). This study summarizes the literature available to set PNECs (predicted no-effect concentrations) for chemical toxicity of U to non-human biota. The corresponding radiological doses were estimated, and as expected chemical toxicity proved to be the greater concern. There were limited data from some types of biota; however, PNECs for the types of biota of interest were as follows: terrestrial plants--250 mg U kg(-1) dry soil; other soil biota--100 mg U kg(-1) dry soil; freshwater plants--0.005 mg U L(-1) water; freshwater invertebrates--0.005 mg U L(-1) water; freshwater benthos--100 mg U kg(-1) dry sediment; freshwater fish at water hardnesses of: <10 mg CaCO3 L(-1) (very soft water)--0.4 mg U L(-1) water; 10-100 mg CaCO3 L(-1) (soft water)--2.8 mg U L(-1) water; and >100 mg CaCO3 L(-1) (hard water)--23 mg U L(-1) water; or as a function of hardness--0.26 (hardness as mg CaCO3 L(-1); mammals--0.1 mg U kg(-1) body weight d(-1).     

Evidence for a warm and humid Mid-Holocene episode in the Aegean and northern Levantine Seas (Greece,NE Mediterranean)

Marine and terrestrial biological and biogeochemical proxies in three sediment cores from North and SE Aegean and northern Levantine Seas record continuous warm and humid conditions between 5.5 and 4.0 ka BP related to the establishment of relatively stratified conditions in the upper water column. These conditions may have resulted from the concordant albeit weak Mid-Holocene South Asian monsoon forcing, combined with lighter Etesian winds. During this interval, sea surface temperatures fluctuate in the Aegean Sea, although exhibiting a strong positive shift at ~4.8 ka BP. The warm and humid climatic conditions triggered upper water column stratification and enhancement of the deep chlorophyll maximum (DCM), leading to dysoxic conditions and the deposition of a sapropel-like layer, but only in the SE Aegean site. In contrast to the shallow water SE Aegean, the deeper North Aegean and the northern Levantine sites, although experiencing stratification in the upper parts of the water column, did not achieve bottom-water dysoxia. Thus, a top–bottom mechanism of stratification–DCM development accompanied by fast transport and burial of organic matter is a likely explanation for the preservation of productivity signal in the shallow sites of the SE Aegean and establishment of sapropelic conditions during the warm and humid Mid-Holocene. The termination of the Mid-Holocene warm and humid phase coincides with the “4.2 ka” climate event. Our data exhibit an N–S time transgressive aridification gradient around the Aegean Sea, most probably associated with the reorganization of the general atmospheric circulation during the Mid-Holocene.     

Organochlorine levels in edible fish from the Marmara Sea, Turkey

Samples of 12 edible fish species from the Marmara Sea were analyzed for organochlorines (PCBs, DDTs, HCB, HCHs, toxaphene, etc.). The results showed that the total concentrations ranged from 329.41 ng/g fat to 1453.87 ng/g fat. DDT group components made up almost half or more of organochlorine contamination. Levels in red mullet were compared with those from neighbor seas. The sum of DDTs as well as HCHs concentrations were markedly lower than in the Black Sea but higher in the Aegean Sea and Mediterranean. Thus, inflow from the Black Sea might be considered as a contamination source for DDT and HCH contamination. On the other hand, total PCB concentration (sum of congeners 28, 52, 101, 118, 138, 153 and 180) detected in this study was comparable or lower than those from the Aegean Sea and Mediterranean. Toxaphene was a minor contaminant. Measured values were below maximum residue levels for human consumption.     

Evaluation of the usefulness of bird feathers as a non-destructive biomonitoring tool for organic pollutants: a comparative and meta-analytical approach

In this study, we investigated whether bird feathers can be used as a non-destructive biomonitor for organic pollutants. We analysed the outermost tail feathers of 8 terrestrial and aquatic bird species from Belgium (8 species, n=108) for polychlorinated biphenyls (PCBs), polybrominated diphenyl ethers (PBDEs) and organochlorine pesticides (OCPs). Every compound class could be quantified in one single tail feather of the birds under study (sum PCBs ranging from 5.5 to 510 ng/g feather, sum PBDEs from 0.33 to 53 ng/g feather, sum DDTs from 1.5 to 730 ng/g feather), except for PBDEs in feathers of the common moorhen (Gallinula chloropus). Further, we calculated Pearson correlations between concentrations of organic pollutants in feathers and concentrations in corresponding muscle or liver tissue from the birds. Correlations were found significant in half of the cases of the terrestrial species, but were found not significant for the aquatic species, with the exception of a significant correlation of sum PCBs in the common moorhen. Only for the common buzzard (Buteo buteo) (n=43) all correlations were found significant (0.32相似文献   

The ecological effects of trichloroacetic acid in the environment

Trichloroacetic acid (TCAA) is a member of the family of compounds known as chloroacetic acids, which includes mono-, di- and trichloroacetic acid. The significant property these compounds share is that they are all phytotoxic. TCAA once was widely used as a potent herbicide. However, long after TCAA's use as a herbicide was discontinued, its presence is still detected in the environment in various compartments. Methods for quantifying TCAA in aqueous and solid samples are summarized. Concentrations in various environmental compartments are presented, with a discussion of the possible formation of TCAA through natural processes. Concentrations of TCAA found to be toxic to aquatic and terrestrial organisms in laboratory and field studies were compiled and used to estimate risk quotients for soil and surface waters. TCAA levels in most water bodies not directly affected by point sources appear to be well below toxicity levels for the most sensitive aquatic organisms. Given the phytotoxicity of TCAA, aquatic plants and phytoplankton would be the aquatic species to monitor for potential effects. Given the concentrations of TCAA measured in various soils, there appears to be a risk to terrestrial organisms. Soil uptake of TCAA by plants has been shown to be rapid. Also, combined uptake of TCAA from soil and directly from the atmosphere has been shown. Therefore, risk quotients derived from soil exposure may underestimate the risk TCAA poses to plants. Moreover, TCE and TCA have been shown to be taken up by plants and converted to TCAA, thus leading to an additional exposure route. Mono- and di-chloroacetic acids can co-occur with TCAA in the atmosphere and soil and are more phytotoxic than TCAA. The cumulative effects of TCAA and compounds with similar toxic effects found in air and soil must be considered in subsequent terrestrial ecosystem risk assessments.     

A review of research on China’s carbon emission peak and its forcing mechanism

In order to make further steps in dealing with climate change, China proposed to peak carbon dioxide emissions by about 2030 and to make best efforts for the peaking early. The carbon emission peak target (CEPT) must result in a forcing mechanism on China’s economic transition. This paper, by following the logical order from “research on carbon emission history” to “carbon emission trend prediction,” from “research on paths of realizing peak” to “peak restraint research,” provides a general review of current status and development trend of researches on China’s carbon emission and its peak value. Furthermore, this paper also reviews the basic theories and specific cases of the forcing mechanism. Based on the existing achievements and development trends in this field, the following research directions that can be further expanded are put forward. First, from the perspective of long-term strategy of sustainable development, we should analyze and construct the forcing mechanism of CEPT in a reverse thinking way. Second, economic transition paths under the forcing mechanism should be systematically studied. Third, by constructing a large-scale policy evaluation model, the emission reduction performance and economic impact of a series of policy measures adopted during the transition process should be quantitatively evaluated.     

近十年鄱阳湖区极端干旱事件频发现象成因初析

近10 a来鄱阳湖区极端干旱事件频发,引起国内外媒体舆论的广泛关注。针对这一情况,运用流域降水、地表蒸散和出湖径流等数据,从流域水量收支平衡的角度,较为系统地分析了导致鄱阳湖区极端干旱事件频发的原因。结果表明,近10 a来鄱阳湖水文干旱起始日期提前,枯水期拉长。虽然干旱持续时间的长短呈现2~3 a的波动,但在总体上呈现逐渐加长的趋势。从流域水分收支的角度来看,近10 a来以水分亏缺为主,流域降水亏缺是基本的致旱因素,流域蒸散量增加则起到一定的增强作用,而出湖径流所起的作用比较复杂,在多数情况下其致旱的影响程度弱于流域降水作用。长江顶托作用强弱变化可以调节流域的水分收支平衡,强化或者减轻湖泊的干旱程度。2003、2004、2007、2008和2009年发生的极端干旱事件主要由流域水分收入项的大幅度减少所造成的,而长江水情变化在多数情况下加剧了流域水分收支的不平衡。这些研究结果明晰了鄱阳湖流域气象干旱与湖泊水文干旱之间的关系以及长江水情变化所扮演的重要角色,为应对未来的干旱变化和制定合理的抗旱防旱对策与措施提供了科学的依据     

Abundance and diversity of aquatic macroinvertebrate communities in lakes exposed to Chernobyl-derived ionising radiation

Littoral (lake shore) macroinvertebrate communities were studied in eight natural lakes affected by fallout from the Chernobyl accident. The lakes spanned a range in ¹³⁷Cs contamination from 100 to 15500 kBq m⁻² and estimated external dose rates ranged from 0.13 to 30.7 μGy h⁻¹. General linear models were used to assess whether abundance of individuals, taxon richness, Berger-Parker dominance and Shannon-Wiener diversity varied across the lakes. Step-wise multiple regressions were used to relate variation in total abundance, taxon richness, Berger-Parker dominance, Shannon-Wiener diversity, taxon richness within major groups of macroinvertebrates and abundance of the more common individual taxa to the measured environmental characteristics (conductivity, pH, total hardness and phosphate; lake area, lake maximum depth and total external dose) of the lakes. No evidence was found in this study that the ecological status of lake communities has been influenced by radioactive contamination from the Chernobyl accident. Indeed, the most contaminated lake, Glubokoye, contained the highest richness of aquatic invertebrates. Taxon richness in the eight study lakes varied from 22 (Svyatskoe #7) to 42 (Glubokoye) which spans a range typical for uncontaminated lakes in the region. Since ⁹⁰Sr is readily-absorbed by Mollusca, estimated dose rates to this group exceeded those for other invertebrate groups in two lakes (Perstok and Glubokoye). However this study found no association between mollusc diversity or abundance of individual snail species and variation between lakes in the external radiation dose. Indeed Glubokoye, the lake most contaminated by ⁹⁰Sr, had the highest richness of freshwater snails per sample (an average of 8.9 taxa per sample).     

基于环境同位素的鄱阳湖与长江关系变化解析

在气候变化和三峡工程调节的双重影响下,长江中下游通江湖泊江湖关系发生显著改变,而最大的通江湖泊—鄱阳湖—水情的变化及其引发的一系列生态和环境问题受到了高度重视和关注。为了揭示不同时期鄱阳湖与长江间的江湖关系,并初步分析三峡运行对鄱阳湖水情的影响,通过对鄱阳湖北部通江水道湖水、降水和九江段长江干流水同位素特征进行调查并探讨长江水与湖水同位素联系。结果表明:湖水、降水和长江水中δ~(18)O和δ~2H值存在明显的季节和空间变化,可用于揭示湖泊与长江间的关系。在三峡调洪削峰期(7月)湖水δ~(18)O和δ~2H值明显要高于长江水,且湖水主要以外排形式补给长江为主,其比例达75%;在三峡蓄水期(10月)长江水位高于湖口水位,从鄱阳湖出口到老爷庙湖水与长江水同位素值具有较高的相似性,表明了此水域受长江水倒灌影响;而在三峡蓄水期(11和12月)湖水同位素值偏大说明了其受到一定较强的蒸发富集影响。三峡水库运行明显改变了长江水位和流量,进而影响了鄱阳湖与长江的补排关系,调洪削峰调度阶段,较高的长江水位对鄱阳湖存在一定的顶托作用,导致湖水难以排泄。因此,三峡水库的调度需要考虑到鄱阳湖流域水情,以免加重该流域丰水期的洪涝灾害和枯水期的水资源短缺。