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941.
In this paper, the vertical variations of heavy metal elements (including Cd, Cr, Cu, Hg, Mn, Ni, Pb, and Zn) in the sediments of Songhua Lake are analyzed using sediment cores. A 70‐year evolutionary history of these heavy metal elements in Songhua Lake is described and the sources of the heavy metals in the sediments are investigated by evaluating the pollution characteristics of the metals in terms of their enrichment coefficients and geoaccumulation indexes. The results indicate that Cr, Cu, Mn, Ni, Pb, and Zn in the sediments originated mainly from basin erosion and were transported to the lake by rivers. Cd and Hg in the sediments also originated from basin erosion that occurred prior to the mid‐1990s, and these sediments have since been overlaid by artificial pollution. The distribution of heavy metals in the sediments of Songhua Lake is influenced by many factors, including sediment composition, the relative importance of fluvial input, and artificial pollution.  相似文献   
942.
Human‐induced and natural interruptions with continuous streams of observational data necessitate the development of gap‐filling and prediction strategies towards better understanding, monitoring and management of aquatic systems. This study quantified the efficacy of multiple non‐linear regression (MNLR) versus artificial neural network (ANN) models as well as the temporal partitioning of diurnal versus nocturnal data for the predictions of chlorophyll‐a (chl‐a) and dissolved oxygen (DO) dynamics. The temporal partitioning increased the predictive performances of the best MNLR models of diurnal DO by 45% and nocturnal DO by 4%, relative to the best diel MNLR model of diel DO ($r_{{\rm adj}}^{2} = 68.8\%$ ). The ANN‐based predictions had a higher predictive power than the MNLR‐based predictions for both chl‐a and DO except for diurnal DO dynamics. The best ANNs based on independent validations were multilayer perceptron (MLP) for diel chl‐a, generalized feedforward (GFF) for diurnal and nocturnal chl‐a, MLP for diel DO, GFF for diurnal DO, and MLP for nocturnal DO.  相似文献   
943.
944.
通过对罗布泊古湖盆区域("大耳朵")湖相沉积物含水量与含盐量、介电性质、地表微地貌等理化参量的分析,本文提出了罗布泊古湖盆区域的散射过程与次地表散射结构;利用全极化测量技术(PolSAR, Polarimetric Synthetic Aperture Radar),本文对不同纹理区域进行了物理散射机制的定量化剖析,同极化相关分析与极化度推算结果表明整个"大耳朵"区域后向散射强烈,亮条带比暗条带的散射机制更为复杂,地表微地貌状态是造成"大耳朵"特征的表观原因.在此基础上,本文利用极化分解技术进一步分离不同散射机制分量,通过定量比较各部分贡献对于"大耳朵"特征的表征能力,提出次地表介质性质(如含盐量)是"大耳朵"特征的根本性成因,相关性可达0.784,同时分析了次地表高含水含盐湖相沉积物在SAR响应中的重要性及其与地表形态之间的动力学形成机制.最后,本文论证了合成孔径雷达(SAR, Synthetic Aperture Radar)在罗布泊地区的穿透能力,预示着SAR遥感技术在干旱区环境研究中的应用潜力.  相似文献   
945.
Here we present datasets from a hydroacoustic survey in July 2011 at Lake Torneträsk, northern Sweden. Our hydroacoustic data exhibit lake floor morphologies formed by glacial erosion and accumulation processes, insights into lacustrine sediment accumulation since the beginning of deglaciation, and information on seismic activity along the Pärvie Fault. Features of glacial scouring with a high‐energy relief, steep slopes, and relative reliefs of more than 50 m are observed in the large W‐basin. The remainder of the lacustrine subsurface appears to host a broad variety of well preserved formations from glacial accumulation related to the last retreat of the Fennoscandian ice sheet. Deposition of glaciolacustrine and lacustrine sediments is focused in areas situated in proximity to major inlets. Sediment accumulation in distal areas of the lake seldom exceeds 2 m or is not observable. We assume that lack of sediment deposition in the lake is a result of different factors, including low rates of erosion in the catchment, a previously high lake level leading to deposition of sediments in higher elevated paleodeltas, tributaries carrying low suspension loads as a result of sedimentation in upstream lakes, and an overall low productivity in the lake. A clear off‐shore trace of the Pärvie Fault could not be detected from our hydroacoustic data. However, an absence of sediment disturbance in close proximity to the presumed fault trace implies minimal seismic activity since deposition of the glaciolacustrine and lacustrine sediments.  相似文献   
946.
The objective of this research study is to assess the capability of time-series of MODIS imagery to provide information suitable for enhancing the understanding of the temporal cycles shown by the abnormal growth of the floating macrophytes in order to support monitoring and management action of Lake Victoria water resources.The proliferation of invasive plants and aquatic weeds is of growing concern. Starting from 1989, Lake Victoria has been interested by the high infestation of water hyacinth with significant socio-economic impact on riparian populations.In this paper, we describe an approach based on the time-series of MODIS to derive the temporal behaviour, the abundance and distribution of the floating macrophytes in the Winam Gulf (Kenyan portion of the Lake Victoria) and its possible links to the concentrations of the main water constituencies.To this end, we consider the NDVI values computed from the MODIS imagery time-series from 2000 to 2009 to identify the floating macrophytes cover and an appropriate bio-optical model to retrieve, by means of an inverse procedure, the concentrations of chlorophyll a, coloured dissolved organic matter and total suspended solid.The maps of the floating vegetation based on the NDVI values allow us to assess the spatial and temporal dynamics of the weeds with high time resolution.A floating vegetation index (FVI) has been introduced for describing the weeds pollution level.The results of the analysis show a consistent temporal relation between the water constituent concentrations within the Winam Gulf and the FVI, especially in the proximity of the greatest proliferation of floating vegetation in the last 10 years that occurred between the second half of 2006 and the first half of 2007.The adopted approach will be useful to implement an automatic system for monitoring and predicting the floating macrophytes proliferation in Lake Victoria.  相似文献   
947.
The opening of the Bonnet Carré spillway to prevent flood threat to New Orleans in April 2008 created a sediment plume in the Lake Pontchartrain. The nutrient rich plume triggered a massive algal bloom in the lake. In this article, we have quantified the spatio-temporal distribution of the plume (suspended solids) and the bloom (chlorophyll-a (chl-a)) in the lake using remotely-sensed data. We processed the Moderate-resolution Imaging Spectroradiometer satellite data for mapping the total suspended solids (TSS) and chl-a concentrations. An existing algorithm was used for estimating TSS whereas a novel slope model was developed to predict the per-pixel chl-a concentration. Both algorithms were successful in capturing the spatio-temporal trend of TSS and chl-a concentrations, respectively. Algal growth was found to be inversely related to TSS concentrations and a time lag of ~45 days existed between the spillway opening and the appearance of the first algal bloom at an observation location.  相似文献   
948.
鄱阳湖自然保护区湿地植被群落与水文情势关系   总被引:7,自引:0,他引:7  
以鄱阳湖自然保护区为研究对象,通过构建植被群落-水文参数直方图和计算敏感性指数,分析植被群落对水文条件变化的耐受性和敏感性,研究湿地植被群落与水文情势的关系。结果表明,在鄱阳湖自然保护区内,不同的植被群落对水文情势变化的耐受性和敏感性不同,苔草群落、假俭草群落对水文条件变化敏感性较低;苔草-廖子草群落、苔草-虉草群落和虉草-苔草群落对水文条件变化的敏感性较高,喜欢相对湿润的环境;南荻群落所能承受的水文条件变化范围较窄,喜欢相对干旱的环境。  相似文献   
949.
白干湖矿田东北部出露钾长花岗岩和二长花岗岩,具有相近的成岩年龄和相似的地球化学特征,表明为同源演化的复式岩体。利用SIMS方法获得二者锆石U-Pb谐和年龄是422±3Ma和421±3.7Ma,为晚志留世。岩石主量元素地球化学特征二者表现为弱过铝质(A/CNK为0.99~1.02)或准铝质(A/CNK为0.92~0.94)、高钾(K2O/Na2O分别为1.08~1.31和1.03~1.22)、高碱((Na2O+K2O)分别为8.59%~9.38%和9.54%~9.69%)、钙碱性或弱碱性(δ分别为2.39~3.17和4.02~4.22)、Fe#(TFeO/MgO分别为9.58~12.26和8.94~9.96)高。稀土元素总体含量(分别为228×10-6~448×10-6和271×10-6~392×10-6)较高,微量元素亏损Ba、Nb、Sr、Ti、P和富集La、Ce、Zr、Sm,总体显示A型花岗岩的特征。R1-R2图解显示岩体构造背景落入晚造山区域。Sr-Yb图解显示岩体落入低Sr高Yb的区域,暗示拉伸的地壳减薄的环境。Pearce图解显示构造环境为板内为主。综合区域背景资料,认为该岩体形成于加里东造山旋回的后碰撞阶段。  相似文献   
950.
鄱阳湖流域抚河径流特征及变化趋势分析   总被引:2,自引:0,他引:2  
罗蔚  张翔  邹大胜  黄燕平 《水文》2012,32(3):75-82
抚河是鄱阳湖流域第二大河流,其径流变化研究对揭示鄱阳湖水文情势演变规律和鄱阳湖生态环境保护具有重要的科学意义。本文采用鄱阳湖流域抚河上、中、下游8个主要水文站的实测资料,分析了抚河径流年内分配特征及变化规律;应用Mann-Kendall非参数检验与回归分析等方法,研究了近几十年内抚河年、月径流变化规律及与降雨的关系。结果表明:(1)抚河径流年内分配不均,但不均匀性在流域内空间差异较小;(2)受水利工程调蓄影响,径流年内分配越来越均匀;(3)不同年代年径流特性存在差异,20世纪70年代至90年代初,径流相对稳定,90年代中期到2002年,呈较明显上升趋势,2002年后,表现为下降趋势;(4)月径流变化有增有减,基本规律为枯水期(11月~次年3月)月径流量基本呈上升趋势,洪水期(4~6月)月径流基本呈下降趋势;(5)抚河的年降水量在2002年附近发生突变减少,与年径流量突变时间基本吻合,说明气候变化降雨量减少对近10年鄱阳湖流域抚河入湖径流的减少影响显著。  相似文献   
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