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1.
廖永岩  赵丽梅 《台湾海峡》2001,20(3):363-370
分别添加孔雀石绿,亚甲基蓝,制霉菌素,达克宁,里劳素等抗真菌药,进行远海梭子蟹离体卵孵化,并对孵化出的蟹幼体进行人工培育至幼蟹,结果发现,孔雀石绿孵化率最高。里劳素SaoI 24h存活率最高,0.2mg/dm^3浓度孔雀石绿孵化率达16%。0.1mg/dm^3里劳素Sao I24h存活率达7.2%,在24.5-27.5度下,从Sao状幼体至大眼幼体为12d,存活率为51.3%,从大眼幼体至第一期幼蟹需4d,存活率为17.3%。  相似文献   

2.
研究ZnSO4、CuSO4、KMnO4对南京丰年虫96小时的急性毒性,结果表明ZnSO4、CuSO4 浓度越高,南京丰年虫暴露其中时间越长,死亡率越高.ZnSO4、CuSO4 对南京丰年虫24h、48h、72h和96h 的LC50分别为1.55×10-6、1.40×10-6、1.28×10-6、0.55×10-6和0.49×10-6、0.46×10-6、0.41×10-6、0.05×10-6,安全浓度为0.05×10-6和0.005×10-6;KMnO4在6.4×10-6以上使南京丰年虫在1~2h内全部死亡,而在6.4×10-6以下毒性不甚明显.  相似文献   

3.
亚甲基蓝对南美白对虾(Pemaeus vannamei Boon)幼体的毒性研究   总被引:6,自引:0,他引:6  
研究了亚甲基蓝对南美白对虾蚤状幼体、糠虾幼体及仔虾的急性毒性。结果表明,不同发育期的幼体,仔虾对此种消毒剂的耐受力不同。亚甲基蓝对南美白对虾蚤状幼体(Z)的24hLC50、48hLC50和安全浓度分别为:2.88×10-6,0.89×10-6,0.025×10-6;对糠虾幼体(M)的24hLC50、48hLC50和安全浓度分别为:3.39×10-6,1.04×10-6,0.029×10-6;对仔虾(P)的24hLC50、48hLC50和安全浓度分别为:6.76×10-6,2.24×10-6,0.073×10-6。  相似文献   

4.
用不同药物治疗凡纳对虾状幼体黏脏病 ,结果表明 :用浓度为 3× 10 - 6 养虾丹、混合施用 0 .15× 10 - 6 次氯酸钠 + 1.5mg/L土霉素或 0 .0 1× 10 - 6 的亚甲基蓝 + 1.5mg/L土霉素可治疗凡纳对虾幼体黏脏病  相似文献   

5.
从东海陆架区采集几组不受扰动的岩芯柱样,研究了有机氯杀虫剂BHC、DDT在东海陆架区的污染历史,表明BHC、DDT在本区的污染水平呈波动变化,约8-10年左右出现一个污染高峰.文中同时介绍了在不同时间尺度上估算水-沉积物界面上BHC、DDT沉积输入通量的两种较为简便的估算模式,并估算得1980-1981年间它们的沉积通量分别为1.3×10-5-19×10-5g/(m2·a)和8.4×10-5-74×10-5g/(m2·a)之间;而自BHC、DDT大量使用以来近40年间,在本陆架区的年均输入通量分别为5.18×10-5-7.70×10-5g/(m2·a)和11.5×10-5-21.0×10-5g/(m2·a)之间.  相似文献   

6.
敌百虫对虾池生物的毒性   总被引:9,自引:0,他引:9  
研究了敌百虫对青岛大扁藻、三角褐指藻、球等鞭金藻和海洋原甲藻等4种海洋微藻及天津厚蟹、脊尾白虾和克氏纺锤水蚤等3种野生甲壳类 ,以及中国对虾、缢蛏和台湾红罗非鱼等3种养殖生物的毒性。研究结果表明 :敌百虫在低浓度下对海洋微藻的生长没有明显影响 ,在一定浓度范围内甚至有促进作用 ,但超过一定浓度范围能完全抑制海洋微藻的生长。各种海洋微藻对敌百虫的敏感性不同。对3种野生甲壳类的半致死浓度分别为 :天津厚蟹LTD50(96h)为1.25×10-6;脊尾白虾LTD50(12h)为0.05×10-6;克氏纺锤水蚤LTD50 (48h)为0.063×10-6。敌百虫对3种养殖生物的半致死浓度分别为 :中国对虾LTD50(48h)为0.060×10-6;缢蛏LTD50(72h)为18.79×10-6;台湾红罗非鱼LTD50(72h)为36.35×10-6。文中还对敌百虫作为对虾病毒病预防药物的价值进行了探讨。  相似文献   

7.
镉对石莼光合作用和呼吸作用及叶绿素含量的影响   总被引:1,自引:0,他引:1  
实验表明 ,用含不同浓度镉 (0、5、10、15、2 0、2 5、30× 10 -6)的海水培养石莼 1~ 8d,石莼的光合作用、呼吸作用、叶绿素含量受到了明显的影响。 5× 10 -6的镉培养 3d,光合速率和叶绿素含量明显下降 ;培养时间越长 ,下降幅度越大。低浓度的镉 (5~ 10× 10 -6)对呼吸有促进作用 ,出现了“伤呼吸”;高浓度的镉 (>10× 10 -6)对呼吸有明显抑制作用 ,培养 5d后石莼开始死亡。  相似文献   

8.
对山东半岛南海岸3个地点虾池内的蟹类组成、分布和携带病毒的情况进行了调查,并用敌百虫和次氯酸钠对天津厚蟹(Helicana fridens)进行了杀灭试验。发现虾池内的蟹类组成相对简单,蟹洞分布 85%集中在水位线以上 100 cm至水位线下 30 cm区域内;敌百虫对天津厚蟹的 96 h半致死浓度 LTD_(50)(96 h)=1.25×10~(-6),96 h全部将天津厚蟹杀死的浓度为 2.75×10~(-6);次氯酸钠(以有效氯计)对天津厚蟹的 72 h半致死浓度为 LTD_(50)(72 h)=63.8×10~(-6),72 h内将天津厚蟹全部杀死的浓度为 111.1×10~(-6)。  相似文献   

9.
铁对自然群落浮游植物生长的影响   总被引:8,自引:0,他引:8  
利用室内加铁实验,研究了铁对胶州湾自然群落浮游植物生长的影响。实验结果显示,加入铁的浓度在5×10-8mol时,实验第7天的总细胞数量和叶绿素a含量分别比不加铁的对照组增加了5.9倍和3.7倍。加入铁的浓度增加10倍,达5×10-7mol时,浮游植物的生长速度更快,实验第5天的细胞数量和叶绿素a含量是对照组的34.9倍和16.1倍。浮游植物优势种中肋骨条藻(Skeletonemacostatum)在加铁浓度为5×10-7mol时,第5天达最高峰,而在加铁浓度为5×10-8mol和对照实验组,细胞数量达到高峰的时间推后了2d,新月菱形藻(Nitzschiaclosterium)在中肋骨条藻衰败后成为优势种。  相似文献   

10.
增加贝类染色体分裂相的方法初探   总被引:1,自引:0,他引:1  
研究以太平洋牡蛎为材料 ,用低温同步化法和 8μg/m L的植物血球凝集素 (PHA- M)、50μg/m L 伴刀豆蛋白 A(Con A)两种外源凝集素分别处理其鳃 ,后用鳃做染色体滴片 ,10 % Giemsa染色后镜检 ,统计分裂相数。发现三种方法都能使分裂相比例增加 ,其中低温同步化法效果最好 ,可使分裂相比例由对照的 0 .7× 10 -4 升高到 6 .5× 10 -4 ,提高 8.3倍。PHA- M法使分裂相比例由对照的 0 .7× 10 -4升高到 5.5× 10 -4 ,提高 6 .8倍 ,Con A法使分裂相比例由对照的 0 .7× 10 -4升高到3.6× 10 -4 ,提高 4 .1倍。  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.
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   

20.
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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