我国淡水水域光合产物的气候生产力探讨

根据太阳辐射在水体中的有效分布、生长季水温和浮游植物光合生态特性等因子,模拟计算了我国大陆东部淡水水域的光合生产力、气候生产力及其季节变化的地理规律。从中得知,这些水域初级产物的年气候生产力主要呈纬向分布,由南向北递减,各地范围在 1.6-24.4gC/m²·a之间,长江以南是>15.0gC/m²·a的高值区,长城以北和四川盆地为<10.0gC/m²·a的低值区,因此,在气候生产力高值区有可能充分利用气候资源优势,开发低成本的自然淡水水域渔业;而在低生产力区,受自然资源的局限其自然捕鱼量需适量控制,因地制宜。     

在磁场中活性炭吸附有机物的研究

将磁化技术引入吸附过程中，考察了磁场处理对活性炭吸附苯、硝基苯、苯甲酸、氯苯和苯酚的影响．结果表明，预磁处理能使非极性物质苯和极性较小的氯苯、苯酚在活性炭上的吸附容量减小，而使极性较大的苯甲酸和有NO2基团的硝基苯的吸附容量增大．增大磁场强度能加强苯和苯甲酸的磁处理效果。     

Exploration of relationships between phytoplankton biomass and related environmental variables using multivariate statistic analysis in a eutrophic shallow lake:A 5-year study

Understanding the process of the changing phytoplankton patterns can be particularly useful in water quality improvement and management decisions.However,it is generally not easy to illustrate the interactions between phytoplankton biomass and related environmental variables given their high spatial and temporal heterogeneity.To elucidate relationships between them,in a eutrophic shallow lake,Taihu Lake,relative long-term data set of biotic and abiotic parameters of water quality in the lake were conducted using multivariate statistical analysis within seasonal periodicity.The results indicate that water temperature and total phosphorus(TP)played governing roles in phytoplankton dynamics in most seasons(i.e.temperature in winter,spring and summer; TP in spring,summer and autumn); COD(chemical oxygen demand)and BOD(biological oxygen demand)presented significant positive relationships with phytoplankton biomass in spring,summer and autumn.However,a complex interplay was found between phytoplankton biomass and nitrogen considering significant positive relationships occurring between them in spring and autumn,and conversely negative ones in summer.As the predatory factor,zooplankton presented significant grazing-pressure on phytoplankton biomass during summer in view of negative relationship between them in the season.Significant feedback effects of phytoplankton development were identified in summer and autumn in view that significant relationships were observed between phytoplankton biomass and pH,Trans(transparency of water)and DO.The results indicate that interactions between phytoplankton biomass and related environmental variables are highly sensitive to seasonal periodicity,which improves understanding of different roles of biotic and abiotic variables upon phytoplankton variability,and hence,advances management methods for eutrophic lakes.     

秦山核电站邻近水域海水光的穿透性能变化研究

本文运用水体可见光的传输机理，讨论了光的传输特性与水中悬浮泥沙，色素和黄色物质的定量关系。同时简述了在秦山核电站邻近海域１９９５年１０月￣１９９６年７月间４个航次的有关水光学特征现场测量过程和实验室分析方法。最后，通过水体中太阳光透透深度和真空层，研究了该邻近海域的光穿透性能的季节性变化。研究表明，核电站运行以来，秦山核电站邻近海域水的光穿透性能变化很小。     

土壤中钼的形态分析方法研究

本文对土壤中有效钼的浸取条件进行最佳化，并利用提高灰化温度达到消除浸取剂对石墨炉原子吸收测定钼的影响，方法用于国标样品和武汉市区土壤样品中钼的形态分析，获得满意的分析结果。     

石墨炉原子吸收法直接测定水中钼

用石墨炉原子吸收法测定水中钼.用不带平台的热涂层石墨管,将灰化温度提高到1850℃,原子化温度定为2380℃,取得较好效果.对6个样品测定,相对标准差<10%,加标回收率在96.6～101%之间,精密度和准确度较好.     

Florisil柱层析与GC-ECD测定海洋环境样品中OCPs

建立了ＧＣ－ＥＣＤ测定海洋环境样品中ＯＣＰs的分析方法。通过Ｆｌｏｒｉｓｉｌ柱层 析的分类分析和毛细管ＧＣ－ＥＣＤ的测定，得出了ＯＣＰs柱层析的分离点（所需正己烷 的最小淋洗体积为１５０ｍｌ）和ＯＣＰs的回收率（其范围为２１．８％～１０８．７％），给出了海洋环境样品中ＯＣＰs的含量。结果表明，本方法是可行的。     

Release of bioactive active iodine in kelp

The release process and influencing factors of bioactive iodine of kelp are systemically studied by leaching experiment. The results showed that the bioactive iodine of kelp can be released rapidly and the principal form of iodine in lixivium is I^- . There is a dynamic process between the release and absorption of iodine. With the increase of leaching water, the gross amounts of released iodine rise.There also exists a transforming process among I^- , IO3^- and organic iodine in lixivium.     

珠江口浮游藻类生态及与关键水质因子分析

从宏观上和特殊性两方面对其进行浮游藻类生态发生与关键水质因子 (盐度、DO、PO4 P、NO3 N)关联的研究与总结。得出二者间确有关联 ,在 12个测点站位中 ,C12 站位具有水域特殊性 ,即在C12 测点具有溶解氧超饱和现象 ,溶氧饱和率为 115 % ,中肋骨条藻高达 8.6 9× 10 5L 1,个体百分组成高达 87.4 % ,藻类优势度为92 .3% ,该测点水域处于赤潮状态 ,并导致C12 测点活性磷浓度为最低测值。由于硝酸盐含量很高 ,藻类生长和硝酸盐的特殊对应关系不明显。相关分析显示 ,在整个水域盐度与藻类生长为正相关 ,藻类丰度与最高溶氧也为正相关 ,藻类生长与活性磷和硝酸盐之间乃为负相关     

探讨影响赤潮的物理因子及其预报

通过多年对广东沿海港湾赤潮发生机理的探讨 ,归纳出引发赤潮的主要物理因子 ,并深入研究潮汐变化与赤潮形成的关系。作者认为在沿海一些半封闭的海湾 ,在月赤纬偏小期间发生大潮易引发赤潮。大亚湾澳头水域 4～ 5月份大潮后多呈现不正规全日潮 ,易出现赤潮生物高峰期 ,较明显的赤潮从发生至消退的全过程往往跨越一个潮水期。根据实践经验总结 ,作者提出利用潮汐变化规律对大亚湾澳头水域 2 0 0 1年 5月份可能出现的赤潮初始阶段作尝试性预测 ,并在赤潮初始阶段通过对水域的浮游生物优势种和当地天气的变化趋势加强观测、研究 ,希望能对赤潮暴发作出较准确的预报。