Ⅱ类水体光学特性的剖面测量方法

剖面测量方法是国际上推荐测量水体表观光学参数的首选方法，文章在简要介绍剖面测量原理的基础上，根据Ⅱ类水体特点对应用算法进行改进，并给出其应用效果。     

288.15 K-323.15 K下四硼酸锂溶液的体积性质（英文）

用振荡管密度计测定了常压下288.15 K～323.15 K范围内不同浓度的Li_2B_4O_7溶液的密度,计算了其在不同温度下的表观摩尔体积。用Pitzer离子相互作用模型拟合了Li_2B_4O_7在不同温度下的Pitzer单电解质体积参数,模型的计算值与实验值相吻合良好。     

大深度声遥测触底指示仪测高计换能器的研制

本文介绍利用表观弹性法,设计纵向振动与径向振动相耦合的朗芝万型换能器,该换能器用于大深度声遥测触底指示仪上,实验表明,理论计算值与实验值相符合,计算方法简单、方便。     

EST-derived microsatellites in Pseudosciaena crocea and their applicability to related species

Simple sequence repeat (SSR) markers were obtained for the large yellow croaker Pseudosciaena crocea using 1 205 expressed sequences tags (ESTs) from the NCBI database. Primers for 48 ESTSSR loci were designed and screened with 30 P.crocea specimens captured from Guanjingyang sea area in Fujian Province of China. Sixteen of the loci were polymorphic, which were amplified with 3 to 11 alleles per locus and the mean of 6.13. The observed and expected heterozygosity per locus ranged from 0.091 to 0.844 (mean 0.544) and from 0.118 to 0.892 (mean 0.644), respectively. Polymorphic information content (PIC) ranged from 0.115 to 0.866 (mean 0.593). The results for cross-species amplification of the 16 large yellow croaker EST-SSRs on P. polyactis, C. niveatus, C. lucidus, A. argentatus and J. belengeri revealed that 14, 12, 11, 7 and 6 loci were successfully amplified with 1 to 10 alleles with an average of 4.5 per locus, respectively, which are suitable for population genetics studies of these species and useful for phylogenetic relationship analysis among these species. Overall, this study provides a set of type I markers for population genetics studies and genome mapping for large yellow croaker and its closely related species.     

The Effect of Temperature on Growth and Energy Budget of the Polychaete,Neanthesjaponica Izuka

Growth and energy budget of the polychaete, Neanthesjaponica, at various temperatures （17, 20, 23, 26 and 29℃） were investigated in this study. The growth, as indicated by final dry weight and specific growth rate （SGR）, increased with increasing temperature, with the maximum level at 26℃, and then decreased significantly at 29℃. A similar trend was observed in feeding rate, food conversion efficiency （FCE） and apparent digestive rate （ADR）. However, no significant differences were detected in ADR among all the temperature treatments. In the pattern of energy allocation, faeces energy was only a small component of energy budget and had little influence on the proportion of food energy allocated to growth. The metabolic energy accounted for a large portion of energy intake for each temperature treatment. The nitrogen excretion was appreciable with changing temperature. The two expenditure terms （respiration energy and excretion energy） in energy budget were the major factors influencing the proportion of food energy allocated to growth. These results revealed that temperature affected the growth of N. japonica mainly by influencing feeding rate and FCE. In addition, regression equations describing the relationship between feeding rate, faecal production, SGR, FCE and temperature were obtained. The optimum temperatures for feeding rate, FCE and SGR were estimated at 25.01 ℃, 24.24℃ and 24.73 ℃, respectively, from the regression equations.     

长江口邻近海域溶解氧分布特征及主要影响因素

根据2002年11月5~10日对东海长江口邻近海域(29.0°N~32.0°N,122.0°E~124°E)的现场调查数据,初步分析了调查海域秋季溶解氧分布特征及主要影响因素。结果显示:调查海域秋季溶解氧平面分布整体上呈近岸高、外海低,表层高、底层低的分布趋势,在约20m深度存在溶解氧跃层。调查海域溶解氧饱和度均<100%,表观耗氧量最高达4.0mg/L,氧不饱和状态由表层至底层逐渐加剧,在123°E附近底层仍然存在明显的溶解氧低值区,但其溶解氧含量已较夏季有所回升,含量范围在3.31~8.47mg/L之间,平均为(6.73±1.09)mg/L。该海域秋季溶解氧分布主要受物理过程控制,生物活动仅在底层溶解氧低值区有较大的影响。     

海洋植物谱系地理模式与遗传连通性研究进展

海洋植物谱系地理学虽然在国内受到的关注比较有限,但近年来的研究进展对了解环境变动如何影响物种的多样性结构、生态适应和进化潜力等亦提供了重要信息.本文首先对刊发海洋植物谱系地理研究最具代表性的两本国际期刊《Molecular Ecology》和《Journal of Biogeography》进行搜索和筛选,从研究团队的...     

亚高山湖泊天才湖周边土壤腐殖酸的光降解研究

溶解性有机质(DOM)是湖泊生态系统的物质循环和能量流动的基础.典型亚高山湖泊DOM的主要来源为流域土壤腐殖酸(外源DOM),其具有较强的光吸收特性,光降解是其重要的转化过程,从而改变碳、氮、磷等物质的存在形式.在气候变暖的背景下,亚高山湖泊中DOM的浓度、pH、溶解氧及太阳辐射都可能发生变化;但这些环境变化对亚高山湖...     

山东半岛东部近海海水溶解氧时空变化

山东半岛沿岸海域陆海相互作用强烈,有着复杂水动力环境的同时也是我国重要的渔业资源区和水产养殖区,针对其DO时空变化特征及影响机制的研究具有重要意义.本文基于2015—2017年期间的监测数据,研究了山东半岛东部近海海水溶解氧的时空变化特征,并结合实测的温度、盐度、pH数据探究其影响机制.结果表明:表、底层溶解氧的空间分...     

长江口邻近海域溶解氧的时空分布及影响因素研究

基于2018年早春和夏季长江口邻近海域的调查数据,分析溶解氧(DO)的时空分布,并讨论其影响因素.结果表明,夏季DO浓度变化范围为1.58～9.37 mg/L,浮游生物光合作用产生的DO是夏季表层水体过饱和的主要因素;夏季调查海域受台湾暖流北上引起海水层化加强,同时水体富营养化导致表层生物大量繁殖所引起有机碎屑的沉降和耗氧分解作用是底层低氧区存在的主要因素.夏季在台湾暖流影响下底层水体表观耗氧量(AOU)与营养盐成正相关关系,底层有机物耗氧降解过程与营养盐的再生密切相关.早春DO浓度变化范围为7.90～10.1 mg/L,长江口外北部海域和浙江近岸海域海水混合均匀,DO浓度主要受温度控制,而台湾暖流影响区海水出现层化现象,其低DO含量也为低氧区的形成奠定了基础.