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1.
《海洋开发与管理》2006,23(5):67-67
大连市海洋与渔业局是大连市海洋与渔业行政管理部门,为市政府组成部门,在市委市政府的正确领导下,紧紧围绕振兴老工业基地和建设“大大连”的战略目标,依法强化海洋管理,发挥优势,开拓创新,促进了海洋经济持续协调健康发展。在诸多海洋产业中,渔业是大连独具特色的优势产业。目前,全市海水增养殖面积21.5万hm2,其中海上养殖面积15.6万hm2、滩涂养殖面积3.7万hm2,陆基养殖面积2.3万hm2;大小渔港212座,其中重点渔港36座,海洋捕捞渔船1.3万艘;水产品加工企业469个,年加工能力125万t。“十五”期间,大连市认真贯彻国家发展渔业的总体方针,发挥…  相似文献   

2.
江苏省银宝盐业有限公司是江苏省盐业集团有限责任公司于1998年投资组建的全资子公司,注册资本1.8亿元.拥有4万hm^2土地资源.5.5万hm^2余标准化养殖池塘,12户水产品加工、塑料加工和机械制造等企业,100余名高中级技术人员,主要从事海盐、水产养殖、塑料加工和机械制造等产品的生产加工、销售和投资;年产盐70万t以上,水产品6万t以上,年销售收入2.8亿元以上,年创利税约4000万元。  相似文献   

3.
苏北浅滩生态状况及分析   总被引:1,自引:0,他引:1       下载免费PDF全文
江苏省盐城市占有苏北浅滩的最大部分,主要由沿海滩涂和辐射沙洲组成,面积46.8万hm2左右,其中:潮上带18万hm2,潮间带16.13万hm2,辐射沙洲12.67万hm2。2004年以来,我们采用社  相似文献   

4.
规范养殖用海管理的实践与思考   总被引:1,自引:0,他引:1  
盐城市位于江苏沿海中部,海域总面积约1.7万km2,其中内水面积约1.1万km2,连陆滩涂及辐射沙洲约45.3万hm2。境内海岸线长582km,占江苏全省的60%。海岸大体分两种类型:一类是射阳河以北为侵蚀性粉砂淤泥质海岸,近几年的人工达标海堤建设,海岸侵蚀得到了遏制;一类是射阳河以南为堆积型粉砂淤泥质海岸,沿岸潮间带浅滩宽10~13km,岸外为巨大的辐射状沙脊群,本岸段是江苏海岸淤积作用最大、潮间带最宽的地带。  相似文献   

5.
南通海岸线长206千米,毗邻海域面积约1万平方千米,-15米以内的浅海滩涂面积55.3万平方公顷,其中-2米以上滩涂面积9.3万平方公顷、0米以上辐射沙洲面积7万余平方公顷、潮间带滩涂的宽度3~11千米。养殖用海是南通海洋开发利用活动中面积最大、涉及面最广的用海类型。2002年《海域法》实施以来,全市累计发放养殖用海  相似文献   

6.
山东乳山县白沙口潮汐发电站是 (原 )国家科委和山东省水利厅共同投资建设的我国较早的一座小型潮汐试验电站 ,1 970年 1 1月动工兴建 ,总装机容量 96 0 k W,6台机组 ,单台机组为 1 6 0 k W。1 978年 8月 1日 1 #2 #机组并网运行 ,1 983年 3 # 4 #机组运行 ,1 987年 5 # 6 #机组运行 ,至此 6台机组全部投入运行发电。共计投资 40 8万元。完成工程量土石方 5 6万 m3,砌石 3万 m3,钢筋砼 0 .5万 m3。截止到目前电站已连续运行长达2 0多年 ,发电 2 1万小时 ,发电量 1 5 2 0万度。直接创产值 85 0万元 ,实现社会效益 85 0 0万元 ,实现纯利润 1 …  相似文献   

7.
一、海洋与渔业是城阳区大农业的重头戏城阳区是1994年青岛市行政区划后成立的新区,地处青岛近郊,胶州湾北岸,是青岛市的城乡结合处,域内交通发达,经济实力雄厚,流亭国际空港、济青、青银、环胶州湾高速公路及胶济铁路纵横交错,加之青岛港、黄岛前湾港等港口,构成了陆海空立体交通网络,地理条件十分优越。全区海岸线长78km,浅海滩涂总面积1.07万hm2,辖5处渔业街道,共有渔民3万余人。2002年,全区水产品总产量达到30.6万t,实现产值16.8亿元,占全区大农业的60%以上,渔业二、三产总产值达45亿元,出口创汇2.8亿元。城阳区已开发养殖面积0.8万hm2…  相似文献   

8.
利用人工培育的亲鱼所获得的受精卵 ,孵化出仔鱼 30 0万尾 ,在水温 18~ 2 0℃、微充气的培育条件下 ,使用海水小球藻、轮虫、卤虫无节幼体和不同规格的微颗粒配合饲料进行饲喂 ,经 58d培育出平均全长 2 .3cm的苗种 132万尾 ,育苗成活率高达 64.1% ,单位水体最高出苗量达 1.33万尾 / m3;另外 ,还有 1.3~ 1.9cm的苗种 68万尾  相似文献   

9.
林承坤 《海岸工程》1989,8(4):51-60
中国最大港上海港是世界十大港口之一。1985年上海港货物吞吐量达11290万吨。目前吞吐能力不足。为解决此困难,必须建造若干新港。根据沉积、河流冲积过程和入海航道水深来选择港址,作者建议选择杭州湾的金山咀和长江口的七丫口为最佳港址。前者码头泊位的规模宜确定为3.5万—5万吨级,后者为1万—2万吨级。  相似文献   

10.
1.自然和社会经济背景日本是一个群岛国。它的专属经济水域占世界第六位,共约451万平方公里,接近陆地国土面积的12倍。水深少于200米的区域有30.7万平方公里,等于日本陆地面积的80%。日本的海岸线总长度约3.3万公里,是少数单位陆地面积占有海岸线长度最大的国家之一(表1、2)。  相似文献   

11.
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   

12.
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   

13.
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   

14.
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   

15.
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   

16.
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   

17.
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   

18.
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   

19.
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   

20.
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   

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