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1.
地下水水质评价是进行地下水资源开发、管理的基础,地下水水质预测是对未来的地下水水质变化趋势进行预报,可为地下水污染防治提供科学的依据。在模糊综合评价中,分别采用聚类权法、加权平均算子和级别特征值法,对传统方法的权重确定、算子选择和结果向量分析等关键环节进行改进;在指数平滑预测中,根据拟合结果确定指数平滑的类型,采用试算法选取权系数,并应用于大沽河地下水源地水质评价和预测。评价结果表明,改进的模糊综合评价可解决传统方法的不适性问题,可根据级别特征值比较评价等级相等的水质,更具实用性和合理性;预测结果表明,李戈庄采区和仁兆-朴木采区未来十年水质将持续恶化,且通过卡方检验分析2016-2017年预测的误差,验证了预测方法的有效性。 相似文献
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水环境质量评价是环境质量评价的重要组成部分,本文根据胶州湾2005年水质监测资料,分别采用单因子指数法和模糊综合评价法进行水质现状评价。运用单因子指数法的评价结果表明,胶州湾东北部和西北部无机氮超标严重;粪大肠菌群超标较严重,主要分布在胶州湾东北部和东南部。模糊综合评价结果表明,胶州湾大部分水质类别为Ⅳ级,东部、北部海域污染较为严重。 相似文献
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根据2009年9月岚山港海洋临时倾倒区海域水质监测数据,采用单因子质量指数法对该倾倒区的水质进行了评价;采用多项水质参数综合评价法、营养状态质量指数法及有机污染指数法对该倾倒区2000-2009年水质状况的变化趋势进行了分析.结果表明:2009年9月影响该海域表、底层水质的主要因素为无机氮、铜、铅和锌;海水水质综合评价指数Q表明2000年至2009年该倾倒区海水水质优劣顺序为:2000年＞2006年＞2004年＞2009年＞2008年,2000年至2009年该倾倒区海水营养状态质量指数NQI、有机污染指数A呈上升趋势,但海水水质为贫营养水平,无富营养化现象,水体质量状况良好. 相似文献
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海口市龙昆沟入海排污口邻近海域水质状况与评价 总被引：1，自引：0，他引：1
根据2007-2009年海口市龙昆沟入海口邻近海域的水质监测结果,采用水质单因子污染指数评价法对该海域的水质状况进行分析和评价。结果表明:海口市龙昆沟入海口邻近海域受到无机氮、活性磷酸盐和石油类污染较为严重,化学耗氧量及生化耗氧量也出现轻度污染,排污口邻近海域海水水质环境有恶化的趋势。并且依据分析结果,提出了相应的防治对策。 相似文献
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采用模糊综合评价法,根据2009年5个月份和2010年6个月份的东极大黄鱼(Larimichthys crocea)养殖区海水水样监测数据,对该养殖区海水水质状况进行了综合评价。结果表明,在年均值的评价中,2009年和2010年养殖区海水水质均为一类水,对一类水的隶属度分别为0.53和0.80,说明2010年的水质状况好于2009年。2010年6个监测月份的评价结果显示,各监测月份水质状况均为一类水质,但各月水质状况对一类水的隶属度值差别较大。4月份和5月份的水质状况对一类水的隶属度在0.5以上,6月份的水质状况对一类水的隶属度最低,仅为0.33,其余监测月份海水水质对一类水的隶属度均小于4、5月份。评价结果与东极大黄鱼养殖区水质的实际状况相符,说明模糊综合评价法适用于养殖区海水水质的评价。 相似文献
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The analysis of the structure of the cryolithozone, facies, and thicknesses of the Quaternary sediments and the results of the physicochemical mathematical modeling of the modern shelf of the western part of the Laptev Sea support the influence of the Late Pleistocene glaciations on the heat conditions and the distribution of the permafrost in the area. A ～200-m thick glacier formed under aerial conditions from atmospheric precipitation represented the metamorphosed snow cover. According to the modeling, the long-living (from 60?50 to 10?4 ky) glacier reduced the thickness of the permafrost rocks in the reviewed shelf area for 280–360 m. The Holocene marine transgression additionally decreased the thickness from 50–140 m on the inner shelf to 220–350 m on the outer shelf. The modern submarine cryolithozone 450-0 m thick is wide-spread in the studied region from the coast to the shelf boundary (isobaths of 130–140 m), where it pinches out at a distance of ～380 km from the coast at a depth of ～250 m above the sea level. 相似文献
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We analyze the components of the carbon system of the Sevastopol bay waters and the balance of main sediment-forming substances
using the data of field investigations in 1998–2008. The interannual variations of total inorganic carbon and the equilibrium
partial pressure of carbon dioxide in the bay water are noted. An increase in the flux of carbon dioxide into the bay and
in the content of organic carbon in bottom sediments is revealed, and an explanation of this phenomenon is given. The priority
accumulation of organic carbon in the sediments of the bay is established. We assess the interannual variation in the relative
abundances of organic and inorganic carbon as an index of the carbon cycle stability. 相似文献
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We generalize and analyze the state of investigations of the influence of river waters on the hydrologic structure of the
Black Sea. Specific features of the water, regime and hydrography of rivers flowing into the sea, data on the discharge of
rivers, and intrayear and interyear variability of the discharge are presented. We discuss and analyze works studying the
transformation of river waters, routes of desalinized sea waters, and their influence on the thermohaline structure and dynamic
regime of the sea.
Translated by Peter V. Malyshev and Dmitry V. Malyshev 相似文献
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V. A. Ivanov S. P. Lyubartseva N. Mikhailova N. B. Shapiro 《Physical Oceanography》2001,11(6):509-524
We analyze the results of numerical calculations performed according to the three-dimensional interdisciplinary model of an
ecological system of the Black-Sea shelf zone near the estuary of the Danube. The complete system of equations of hydrothermodynamics
is solved together with transport equations of the advection-diffusion-reaction type used to describe the transformation of
a substance (nitrogen) between the components of the characteristic vectors of the ecosystem: plankton, detritus, and biogenic
elements (nitrates). We describe the distinctive features of the circumcontinental distribution of components obtained as
a result of numerical experiments and present arguments for the conclusion that the ecosystem of the Danube estuary water
area plays the role of a buffer zone between the press of the Danubian biogenic pollutions and the neighbouring areas of the
shelf zone and open sea.
Translated by Peter V. Malyshev and Dmitry V. Malyshev 相似文献
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Ten years of semistationary studies of the interaction of the ice cover and the coastal relief of the Kandalakhsa Gulf in the White Sea allowed us to reveal the peculiarities of these processes in the warm and cold years and the mechanisms of the origination of ice forms, including ice tents, which govern the character of the tidal flats. Three dynamic fast ice zones are distinguished by their geomorphological location, morphology, and ice dynamics. The dependence of the mechanisms and volumes of the enrichment of the fast ice in the sediments on the coastal zone??s relief was established. At the coast of the Kindo Peninsula (Velikaya Salma Strait), the ice mostly contains fine-sandy sediments. Coarser sediments, including boulders, are occasional and frozen into the ice at the contact of the fast ice and the bottom. At the expense of the ice??s spreading by 4?C6 times in the warm years and 2?C4 times in the cold years, several thousand tons of sediments mostly from the tidal flat??s surface (100?C700 m3 from 1 km of coast in the wide tidal flats and <50 m3 on the steep coasts) are delivered to the water area. 相似文献
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Relationship between the path of the Kuroshio in the south of Japan and the path of the Kuroshio Extension in the east 总被引：2，自引：0，他引：2
A relationship between paths of the Kuroshio and Kuroshio Extension (KE) is investigated, using the satellite-derived altimetry
dataset of 1993–2008. When the Kuroshio takes the nearshore nonlarge meander path or typical large meander path and resultantly
goes through the deeper channel (about 2500 m) of the Izu-Ogasawara Ridge, the KE path adopts a relatively stable state with
the two quasi-stationary meanders. On the other hand, when the Kuroshio takes the offshore nonlarge meander path and then
passes over the shallower part of the Ridge (about 1000 m), the KE path tends to be convoluted, i.e., an unstable state. 相似文献
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I. E. Timchenko A. A. Primalenny V. D. Yarin E. F. Vasechkina E. M. Igumnova 《Physical Oceanography》2001,11(4):367-378
We use many-year archival observations of hydrologic and hydrobiologic state of the Sea of Azov for the identification of
the structure of a model of its ecosystem. The ecosystem model, supplemented with expert estimates of bioresource consumption
(fish reserve), contamination level, and possible ecologic fines for violation of the sea natural state, is formalized by
the method of system dynamics. Hereat, the major part of influence functions is found in terms of observational data with
application of self-organization algorithms. We also present the results of simulated experiments with the model of the ecosystem,
which enable us to analyse scenarios of its behaviour under the influence of various external factors (wind, river discharge,
water exchange with the Black Sea, etc.).
Translated by Peter V. Malyshev and Dmitry V. Malyshev 相似文献
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E. L. Vinogradova 《Oceanology》2008,48(4):483-492
The spatiotemporal variability of the hydrochemical composition of the riverine runoff in nearmouth areas is presented using the example of selected rivers of the Arctic Basin. The temporal dynamics of the riverine nutrient runoff are mainly determined by the seasonal and interseasonal variations in the drainage basins. The spatial variations in the chemical composition of riverine waters in the near-mouth areas are mainly caused by the dynamics of the water flow and the river bed relief and, to a lesser degree, by biochemical processes. It is shown that the variations in the nutrient composition of the waters in near-mouth areas are comparable in magnitude to those at the river-sea geochemical barriers. 相似文献
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The methodology and the first results of the computations of the volumes, masses, and growth rates of the sedimentary body of the buried Black Sea basin are presented. Their temporal evolution reflects the regional paleogeodynamics, in particular, the reorientation of the vector of the relative movement of the Arabian and Eurasian lithospheric plates and the related intensification of their collision in the late Miocene-Pliocene. 相似文献
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Izvestiya, Atmospheric and Oceanic Physics - Analysis of the temporal variations of the virtual heights of the sporadic E layer (h?ES) determined from ionograms with increased accuracy (1... 相似文献