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贻贝(Mytilus edulis L.)是一种冷水性双壳类软体动物，它在我国沿岸分布的南限是胶州湾，但仅见于港内码头及船底上，且数量不多。
1958年青岛市水产局、原青岛市海水养殖场和中国科学院海洋研究所等单位曾一起自大连和烟台移贻贝苗至青岛试养，次年养殖架上也曾有少量幼苗附着，但未能大量繁殖起来。1971年后胶南县海水养殖试验场及青岛市第二海水养殖场等先后进行数十亩乃至数百亩移苗养殖，附苗量虽有所增长，但直至1974年仍缺乏生产意义。这种情况引起我们的思考:胶州湾贻贝苗源能否大量发展？它的限制因素是什么？
1972年至1973年，我们与烟台地区海水养殖试验场等单位曾对烟台沿岸贻贝苗源进行调查研究，确认当时烟台苗种产量不高的主要原因是附着基不足，其次是亲贝不足，据此试验成功了“废旧草绠采苗法”。之后，随着采苗器材的增加及养殖面积的不断扩大，烟台芝罘湾已发展成为一个较好的苗场，通常可供万亩以上生产用苗。这个经验对我们开发胶州湾的苗源很有启发。
1975年胶南县在胶州湾大力推广“废旧草绠采苗法”，收割海带后保留废旧海带架两万台采贻贝苗， 1976年进一步扩大贻贝养殖面积，继续留绠采苗。我们在青岛市水产局及胶南县水产局等单位的协助下，于1975年9月及1976年8-9月，对胶州湾内及湾口(青岛前海)留绠采苗的情况进行了调查，这些调查资料即为本文的主要依据。 相似文献
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东山湾翡翠贻贝海区半人工采苗技术研究 总被引：1，自引：0，他引：1
本文研究了东山湾翡翠贻贝的繁殖期，附苗期及海区半人工采苗技术。结果表明：东山湾翡翠贻贝的繁殖期在５－１０月，其５－６月为繁殖盛期。贻贝附苗季节在６－１１月，主要附苗季节在６月上中旬至７月初。通过对东山湾７片采苗区海水理化因子的测定和采苗效果的比较试验，确定了东山湾合适的采苗区为２＾＃－６＾＃区，其中３＾＃，４＾３，５＾＃区采苗效果最好，同时筛选出了木麻黄，胶皮合股绳和泡沫编织袋等３种附苗效果较好的 相似文献
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《海洋科学集刊》1976,(11):201-210
像其他海洋生物的生长一样,贻贝(Mytilus edulis L.)也是因海区或生境不同,养殖方法不同,季节不同,生长状况也不同。研究殆贝的生长规律,无疑对判断养殖效果、确立养殖程序等是十分重要的;同时在生态学研究中,对分析种群结构及推断某些生物学特点等,也是不可缺少的。
关于贻贝的生长过去虽有一些记载,但是较系统的材料,现在还不多见。随着生产发展及调查研究的需要,对这个问题我们必须做到胸中有数。为此,我们于1972-1973年结合人工育苗工作,对烟台沿岸的贻贝,自受精卵开始至成贝收获的全部生长过程,进行了较系统的调查研究。除贝壳生长的材料外,还测定了养成时期的肉质部生长的材料。对自然苗的生长情况也作了一些记录。关于春苗的幼虫期及幼苗期的生长情况,我们过去已较详细地报告过[1],此处不再赘述;仅对生产意义更大的人工秋苗的生长状沉予以论述。 相似文献
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1974—1985年在烟台市、荣成和长岛县进行了自然海区采苗的试验研究。研究结果表明,采苗袋(笼)是较好的扇贝自然海区采苗器。 自然海区采苗技术的关键是:采苗袋网目在1.5毫米左右,内放少量网片作为稚贝附着基;海区透明度大;适时预报投放采苗器时间;掌握适宜的采苗水层。 该项技术经济效益显著。 相似文献
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１９８８～１９８９年，作者在山东省海阳县进行树脂涂料器材的采苗和养成筛选试验，取得了一定的效果。１９９０年，将海区试验移到了浙江省乐清湾进行，经过棚架式采苗和浮筏式养殖，附苗密度、生长速度，都能达到生产要求。１９９０年９月４日，对采苗情况进行验收，得到了专家及同行的好评。１９９１年扩大试验到１０００片，与橡皮条交叉分挂在同一棚架上采苗，然后移到同一浮筏上养成。养成期间，几次抽样检测，分别测量其密度和大小。１９９２年４月９日，委托专家和同行再次验收，以检测的结果，推算出一台筏架树脂纸板和一台筏架橡… 相似文献
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贻贝养殖,在我国沿海地区已经广泛开展。贻贝人工育苗是解决贻贝养殖苗种的途径之一,尤其在自然苗缺乏的地区,或是为了选择优良品种出发,更有其重要意义。我们在过去工作的基础上,于1972—1974年期间,在胶南县海水养殖场进行了贻贝生产性人工育苗试验。以后又在青岛进行了一些培养条件的研究。通过几年的工作,对于育苗的一些重要环节,尤其对于提高室内水池培养到附着阶段的成活率,和探索下海后掉苗的原因,已取得了一定的成果,使人工育苗生产初具规模。现将主要结果报告于下。 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
15.
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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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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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