10a生连香树人工群落生物量研究

对１０年（ａ）生连香树人工群落生物量的分布与模型及凋落物进行了研究,主要结果为：①建立了连香树各器官与地（胸）径或树高的回归模型６８个．②群落总生物量（Ｗｔ／ｔｈｍ－２）为１２６．３２６,其中,地上和地下部分生物量（Ｗ／ｔｈｍ－２）分别为７６．０６８和４７．８１０,凋落物Ｗ为２．４４８．③群落、根系和吸收根的生产力（Ｐ／ｔｈｍ－２ａ－１）分别是１２．３８８～１５．２４８、４．７８１和０．６１１．④群落光能和有效光能利用率分别为０．７５％和１．８８％．⑤９７．４８％的根集中于０～２０ｃｍ土层,６９．９３％的根分布于距干基４０ｃｍ的水平范围;９２．０７％的叶分布于３～６ｍ的垂直范围,８３．８０％的叶分布于距干基１ｍ的水平范围;８４．０５％的干枝分布于距干基０．５ｍ的水平范围．⑥１０～１２月凋落量占全年的８１．２６％．⑦凋落物对元素生物循环的影响大小顺序为Ｐ＞Ｎ＞Ｋ＞Ｃａ＞Ｍｇ＞Ｆｅ＞Ａｌ＞Ｍｎ．⑧提出了生物循环功能系数、凋落物分解率和保存率的算法及含义     

四川不同海拔豆地生态及大豆生长发育变化研究

对φ（Ｎ）３２°１４′～３２°５６′,λ（Ｅ）１０４°３６′～１０４°５１′范围内海拔（ｈａｌｔ）４００ ～１ ４００ ｍ 豆地小气候观测结果表明：ｈａｌｔ每升高１００ ｍ ,平均气温递减０．７２ ℃;年降雨量递增６３．０ ｍｍ（４００～６００ ｍ） ～１０６．８ ｍｍ（８００ ～１ ４００ ｍ）;相对湿度递增１％ ;日照时数呈抛物线上升变化． ｈａｌｔ４００ ｍ 日均温稳定通过１２．０ ℃的初期为３ 月中旬,ｈａｌｔ每升高１００ ｍ ,该时间延迟５～７ ｄ． 不同ｈａｌｔ＞１２℃的有效积温分别为３６２１．２ ℃（４００ ｍ）;３ ２４５ ．０ ℃（６００ ｍ）;３ １４９．９ ℃（８００ ｍ） ;２ ８０４ ．８ ℃（１ ０００ ｍ） ;２０８２．１ ℃（１２００ ｍ）;１ ９５０．１ ℃（１ ４００ ｍ） ． 在相对较高的海拔,存在明显的逆温和南北坡效应,相应存在大豆局部高产区． 不同海拔豆地生态及大豆生长发育变化研究结果可为四川不同海拔区大豆品种合理布局和应用高产优质栽培技术提供了理论依据．     

不同消毒剂对水中脊髓灰质炎病毒灭活的比较

将脊髓灰质炎病毒（ Ｐｏｌｉｏ Ｖ） 及不同消毒剂投加到模拟水样中,按不同接触时间１ ,３ ,１０ ,３０ ｍｉｎ 取样,空斑定量． 当模拟水有机质含量 Ｃ Ｏ Ｄ 为２０ ｍｇ／ Ｌ,病毒浓度ｎ（ Ｐ Ｆ Ｕ） ≈１ ×１０５ ｍ Ｌ－ １ 时,分别投加氯制剂有效氯ρ（ Ｃｌ）１６ ｍｇ／ Ｌ,接触３０ ｍｉｎ ;ρ（ Ｃｌ Ｏ２） ＝ ８ ．０ ｍｇ／ Ｌ,３０ ｍｉｎ ; Ｃｌ＋ Ｃｌ Ｏ２ 联合消毒剂（５ ．０ ＋ ５ ．０） ｍｇ／ Ｌ,３０ ｍｉｎ ;ρ（ Ｏ３） ＝ １ ．２２ ｍｇ／ Ｌ,１０ ｍｉｎ 时;可使病毒彻底灭活． 它们使 Ｐｏｌｉｏ Ｖ 达到９９ ．９９ ％ 灭活的浓度时间乘积（ ρ×ｔ） 值分别是６６２ ．５ ,１２９ ．５ ,２００ ．０ 和３ ．２ ｍｇ Ｌ－ １ ｍｉｎ ． 消毒效果（ 顺序） 为 Ｏ３ ＞ Ｃｌ Ｏ２ ＞ Ｃｌ＋ Ｃｌ Ｏ２ ＞ Ｃｌ． 联合消毒灭活 Ｐｏｌｉｏ Ｖ 的效果为 Ｃｌ 的３ ．３ 倍,表明将 Ｃｌ 与 Ｃｌ Ｏ２ 联合应用具有协同效应,优于传统的单一加氯消毒方式     

转化血型用蕃茄α－D－半乳糖苷酶的分离、纯化及理化性质

成熟蕃茄匀浆后，经硫酸铵盐析，ＤＥＡＥ－ＳｅｐｈａｄｅｘＡ－５０离子交换层析，ＳｅｐａｄｅｘＧ－１００凝胶过滤和Ｍｅｌｉｂｉｏｓｅ－Ａｇａｒｏｓｅ亲和层析，获得了α－Ｄ－半乳糖苷酶（Ｃ．Ｅ．３．２．１．１１）。酶制剂经ＰＡＧＥ检测为一条带；ＳＤＳ－Ｇ－ＰＡＧＥ测得酶Ｍｒ为３４０００；比活力５２．９Ｕ／ｍｇ·；提纯倍数为５２９０１产率为４５％．酶专－催化以α－Ｄ－半乳糖为末端ａ－（１，３）连接的糖苷键，以ＰＮＰＧ（对硝基苯－α－Ｄ－半乳糖昔）为废物，酶催化反应的Ｋｍ＝０．１１ｍｍｏｌ／Ｌ，Ｖｍａｘ为６７μｍｏｌ·ｍｇ１－·ｍｉｎ－１．ｔ稳定范是０～３５℃；ＰＨ稳定范围是４．０～７．０．最适ｐＨ为５．１．半乳糖是酶的竞争性抑制剂；Ｃｕ２＋、Ｚｎ２＋、Ｍｎ２＋、Ｆｅ３＋、Ａｇ＋和ＥＤＴＡ对酶活性无影响．纯酶制剂可作为Ｂ型血向Ｏ型血转化的工具酶液．     

高效液相色谱法分析水中痕量多环芳烃

本文利用高效液相色谱法测定水中痕量多环芳烃（ＰＡＨｓ）。以二氯甲烷作溶剂,超声提取水中痕量ＰＡＨｓ;甲醇、水作流动相,梯度淋洗,用程序可变波长荧光检测器测定。ＰＨＡｓ浓度为０．００７＝０．６μｇ·ｍｌ＾－１范围时,线性相关系数均在０．９９９９以上;峰高、峰面积的相对标准偏差（ｎ＝１０）分别为１．０１－１．８５％,２．００－３．９４％;检测限（Ｓ／Ｎ＝２）为３．１－２３．０ｐｇ;实际水样的加标回收率     

一种海生黄藻的氨基酸和脂肪酸组成

对一种海生超微型藻类,品系ＰＰ９８３,的分类学地位、生长和生化组成进行了研究．形态学观察和色素分析表明,ＰＰ９８３ 是一种黄藻．在２５ ℃和１００ μｍｏｌ ｍ － ２ ｓ－１ 的条件下,ＰＰ９８３ 的生长速率为１．１５ ｄｉｖｄ,其对数生长期的蛋白质、脂肪和糖类质量分数分别为干重的４０ ．２％ 、２５ ．０ ％ 和１１ ．１％ ;共检出了１７ 种氨基酸,其总量为干重的２７．８ ％ ．ＰＰ９８３ 的多不饱和脂肪酸（ＰＵＦＡｓ）占总可提取脂肪酸的２６．４％ ,其中主要是ＥＰＡ,占干重的４．６％ ,而ＤＨＡ未检出．结果显示,ＰＰ９８３ 不仅可作为海生动物的优良饵料,而且是ＥＰＡ的重要潜在资源     

煤加压气化废水加压曝气生物处理研究

加压曝气生物氧化新技术,新组合处理煤加压气化废水,ＣＯＤ负荷１５．６ｋｇ／（ｍ＾３·ｄ）,去除率９２．１％;ＮＨ３－Ｎ负荷０．５７ｋｇ／（ｍ＾３·ｄ）,去除率９１．０％,二项指标出水均达到国家排放标准。     

10a生态香树人工群落生物量研究

对１０年（ａ）生连香树人工群落生物量的分布与模型及凋落物进行了研究,主要结果为（１）建立了连香树各器官与地（胸）径或树高的回归模型６８个（２）群落总生物量为１２６．３２６,其中,地下和地下部分生物量（Ｗ／ｔｈｍ＾－２）分别为７６．０６８和４７．８１０,凋落物Ｗ为２．４４８（３）群落,根系和吸收根的生产力（Ｐ／ｔｈｍ＾－２ａ＾－１）分别是１２．３８８－１５．２４８、４．７８１和０．６１１（４）群落光     

硝化菌群在不同条件下的增殖速率和硝化活性

研究了不同环境因子变化对硝化菌群的增殖能力及其对硝化作用活性的影响,确定了硝化菌群的最佳生长条件．研究发现,温度（θ／℃）、ｐＨ、供氧状况、无机碳源浓度等对于硝化细菌菌群的增殖能力及硝化作用活性具有较重要的影响,而含盐量高低几乎无影响．最适（θ、ｐＨ、［ρ（Ｏ２）］、［ρ（ＮａＨＣＯ３）］分别为３０℃、ｐＨ８．５、３．５ｍｇＬ－１、１ｇＬ－１,此时最大比生长速μｍ可达５．１８ｄ－１,最大比降解速υｍ可达４８．４３ｈ－１．在含氧量较低时,氨氮浓度的升高使硝化菌群的μ值下降,υ值上升．考察有机碳对该菌群的影响发现,ｍ（Ｃｏｒｇ）ｍ－１（Ｎ）在０～０．５之间时,菌群有较大的比生长速率,并且硝化作用活性增强     

胡椒养分含量状况的研究

胡椒大、中量元素的含量在不同树龄中有所不同，幼龄期以氮最高，其Ｎ：Ｐ２Ｏ３：Ｋ２Ｏ：Ｃａ：Ｍｇ为１：０．１５：０．５３－０．９：０．２２－０．３８：０．１５－０．３０；成年龄则以Ｋ２Ｏ最高，Ｎ：Ｐ２Ｏ３：Ｋ２Ｏ：Ｃａ：Ｍｇ为１：０．１３：１．３２：０．４４：０．１６．在不施微肥的情况下，胡椒叶片缺Ｂ、Ｍｏ、Ｚｎ．成年龄胡椒各养分含量都是从萌芽期（收获后）开始，随生育期的进展而增加，到果实成熟期下降．一株中产胡椒Ｎ、Ｐ２Ｏ５、Ｋ２Ｏ总吸收量为２８２．４ｇ，其比例为１：０．１９：０．９．     

Benthic algal production across lake size gradients: interactions among morphometry, nutrients, and light

Attached algae play a minor role in conceptual and empirical models of lake ecosystem function but paradoxically form the energetic base of food webs that support a wide variety of fishes. To explore the apparent mismatch between perceived limits on contributions of periphyton to whole-lake primary production and its importance to consumers, we modeled the contribution of periphyton to whole-ecosystem primary production across lake size, shape, and nutrient gradients. The distribution of available benthic habitat for periphyton is influenced by the ratio of mean depth to maximum depth (DR = z/ z(max)). We modeled total phytoplankton production from water-column nutrient availability, z, and light. Periphyton production was a function of light-saturated photosynthesis (BPmax) and light availability at depth. The model demonstrated that depth ratio (DR) and light attenuation strongly determined the maximum possible contribution of benthic algae to lake production, and the benthic proportion of whole-lake primary production (BPf) declined with increasing nutrients. Shallow lakes (z < or =5 m) were insensitive to DR and were dominated by either benthic or pelagic primary productivity depending on trophic status. Moderately deep oligotrophic lakes had substantial contributions by benthic primary productivity at low depth ratios and when maximum benthic photosynthesis was moderate or high. Extremely large, deep lakes always had low fractional contributions of benthic primary production. An analysis of the world's largest lakes showed that the shapes of natural lakes shift increasingly toward lower depth ratios with increasing depth, maximizing the potential importance of littoral primary production in large-lake food webs. The repeatedly demonstrated importance of periphyton to lake food webs may reflect the combination of low depth ratios and high light penetration characteristic of large, oligotrophic lakes that in turn lead to substantial contributions of periphyton to autochthonous production.     

Benthic-planktonic coupling, regime shifts, and whole-lake primary production in shallow lakes

Alternative stable states in shallow lakes are typically characterized by submerged macrophyte (clear-water state) or phytoplankton (turbid state) dominance. However, a clear-water state may occur in eutrophic lakes even when macrophytes are absent. To test whether sediment algae could cause a regime shift in the absence of macrophytes, we developed a model of benthic (periphyton) and planktonic (phytoplankton) primary production using parameters derived from a shallow macrophyte-free lake that shifted from a turbid to a clear-water state following fish removal (biomanipulation). The model includes a negative feedback effect of periphyton on phosphorus (P) release from sediments. This in turn induces a positive feedback between phytoplankton production and P release. Scenarios incorporating a gradient of external P loading rates revealed that (1) periphyton and phytoplankton both contributed substantially to whole-lake production over a broad range of external P loading in a clear-water state; (2) during the clear-water state, the loss of benthic production was gradually replaced by phytoplankton production, leaving whole-lake production largely unchanged; (3) the responses of lakes to biomanipulation and increased external P loading were both dependent on lake morphometry; and (4) the capacity of periphyton to buffer the effects of increased external P loading and maintain a clear-water state was highly sensitive to relationships between light availability at the sediment surface and the of P release. Our model suggests a mechanism for the persistence of alternative states in shallow macrophyte-free lakes and demonstrates that regime shifts may trigger profound changes in ecosystem structure and function.     

Small-scale gradients of phytoplankton productivity in the littoral fringe

Inshore-offshore transects and time-series sampling programs were carried out on the South shore of the St. Lawrence Estuary on several occasions during the summer season of 1978, 1979 and 1986. In 1981, a time-series sampling program was also conducted on three occasions during the summer. The sampling program was carried out to test the hypothesis that higher phytoplankton biomass and productivity occurs in the littoral zone than in the offshore zone. Our results showed consistently higher nutrient concentrations and lower seasonal variability in the littoral zone than offshore. However, biomass indicators (chlorophyll concentrations and phytoplankton cell counts) showed lower values nearshore than offshore, in contrast to primary production and photosynthetic capacity which were higher nearshore than offshore. These differences are interpreted with reference to the grazing activity of benthic filter-feeders, which probably helped to reduce the phytoplankton biomass in the littoral zone, while at the same time, they contributed to the rapid recycling of nutrients, thereby allowing much higher phytoplankton productivity nearshore than offshore. These results are in keeping with the ecological concept suggesting that exploitation can have a rejuvenating effect on an ecosystem which often is translated into enhanced productivity.     

Nutrient cycling by fish supports relatively more primary production as lake productivity increases

Animals can be important in nutrient cycling in particular ecosystems, but few studies have examined how this importance varies along environmental gradients. In this study we quantified the nutrient cycling role of an abundant detritivorous fish species, the gizzard shad (Dorosoma cepedianum), in reservoir ecosystems along a gradient of ecosystem productivity. Gizzard shad feed mostly on sediment detritus and excrete sediment-derived nutrients into the water column, thereby mediating a cross-habitat translocation of nutrients to phytoplankton. We quantified nitrogen and phosphorus cycling (excretion) rates of gizzard shad, as well as nutrient demand by phytoplankton, in seven lakes over a four-year period (16 lake-years). The lakes span a gradient of watershed land use (the relative amounts of land used for agriculture vs. forest) and productivity. As the watersheds of these lakes became increasingly dominated by agricultural land, primary production rates, lake trophic state indicators (total phosphorus and chlorophyll concentrations), and nutrient flux through gizzard shad populations all increased. Nutrient cycling by gizzard shad supported a substantial proportion of primary production in these ecosystems, and this proportion increased as watershed agriculture (and ecosystem productivity) increased. In the four productive lakes with agricultural watersheds (>78% agricultural land), gizzard shad supported on average 51% of phytoplankton primary production (range 27-67%). In contrast, in the three relatively unproductive lakes in forested or mixed-land-use watersheds (>47% forest, <52% agricultural land), gizzard shad supported 18% of primary production (range 14-23%). Thus, along a gradient of forested to agricultural landscapes, both watershed nutrient inputs and nutrient translocation by gizzard shad increase, but our data indicate that the importance of nutrient translocation by gizzard shad increases more rapidly. Our results therefore support the hypothesis that watersheds and gizzard shad jointly regulate primary production in reservoir ecosystems.     

惠州西湖浮游植物磷脂脂肪酸特征研究

对富营养化水体常见浮游植物进行了分离和培养,测定了其磷脂脂肪酸（PLFA）。同时,检测了惠州西湖浮游植物的磷脂脂肪酸;结合惠州西湖浮游植物群落组成数据,分析了浮游植物磷脂脂肪酸特征及其与浮游植物群落结构的关系。结果表明：结合PLFA与细胞丰度和生物量的分析,α-亚麻酸（18：3ω3）的质量浓度与蓝藻（除湖丝藻外）呈正相关;二十碳四烯酸ARA（20：4ω6）和二十二碳六烯酸DHA（22：6ω3）的质量浓度与硅藻呈正相关;二十碳五烯酸EPA（20：5ω3）和16：3ω3的质量浓度与绿藻呈正相关等,其中16：3ω3为绿藻门独有的脂肪酸。这些均与室内实验得到的结果相符合。本研究表明,磷脂脂肪酸可以作为生物标志物来分析浮游植物组成,它将是一种可行的研究浮游植物群落结构的新方法。     

In situ net primary productivity and photosynthesis of Antarctic sea ice algal, phytoplankton and benthic algal communities

Primary production at Antarctic coastal sites is contributed from sea ice algae, phytoplankton and benthic algae. Oxygen microelectrodes were used to estimate sea ice and benthic primary production at several sites around Casey, a coastal area in eastern Antarctica. Maximum oxygen export from sea ice was 0.95 mmol O₂ m⁻² h⁻¹ (~11.7 mg C m⁻² h⁻¹) while from the sediment it was 6.08 mmol O₂ m⁻² h⁻¹ (~70.8 mg C m⁻² h⁻¹). When the ice was present O₂ export from the benthos was either low or negative. Sea ice algae assimilation rates were up to 3.77 mg C (mg Chl-a)⁻¹ h⁻¹ while those from the benthos were up to 1.53 mg C (mg Chl-a)⁻¹ h⁻¹. The contribution of the major components of primary productivity was assessed using fluorometric techniques. When the ice was present approximately 55–65% of total daily primary production occurred in the sea ice with the remainder unequally partitioned between the sediment and the water column. When the ice was absent, the benthos contributed nearly 90% of the primary production.     

Quantitative relationships among phytoplankton body size classes and production processes in the North Adriatic frontal region

The variation patterns of phytoplankton standing crop and productivity in the North Adriatic frontal region and the relative importance of pico-, nano-, micro-phytoplankton are shown. Data of standing crop (chlorophyll a - Chl a ) and productivity ( 14 C assimilation) and PAR radiation ( w Em m 2 r s m 1 ) were collected during the four oceanographic cruises of the PRISMA II project. Average standing crop and productivity in the study area were 1.41 - 0.42 r mg r m m 3 Chl a and 1.23 - 0.37 r mg r C r m m 3 r h m 1 ; average assimilation number (P/B) was 0.872 - 0.589 r mg r C (mg-Chl a ) m 1 h m 1 and average photosynthetic efficiency (PE) was 0.020 - 0.054 (mg r C(mg-Chl a ) m 1 r h m 1 ) [ w Em m 2 r s m 1 ] m 1 . Phytoplankton biomass and productivity showed significant patterns of variation with the distance from the coast, with increasing depth and decreasing light intensity. The same patterns were shown by the three phytoplankton size classes. The spatio-temporal variations were significantly larger within the microplankton than within the pico- and nano-plankton size classes. Planktonic guilds were dominated by picoplankton, both as standing crop and productivity, in the northern stations (0.539 - 0.21 r mg r m m 3 Chl a and 0.572 - 0.25 r mg r C r m m 3 r h m 1 ) and in those more offshore, while microplankton was more important in the coastal and southern stations (0.727 - 0.58 r mg r m m 3 Chl a and 0.63 - 0.28 r mg r C r m m 3 r h m 1 ). In relative terms, picoplankton accounts for the 53% and 46% of biomass and primary production, while the microplankton account for the 43.6% and 48%. Assimilation number and photosynthetic efficiency did not show spatio-temporal variations but PE was inversely related with PAR radiation for all the size classes. Data suggest that the spatio-temporal patterns observed in this study are affected by the competitive relationships among body size classes in the phytoplankton guilds.     

Microphytobenthos of the Dogger Bank: a comparison between shallow and deep areas using phytopigment composition of the sediment

The surface sediment characteristics related to benthic microalgae primary production were studied at the Dogger Bank, North Sea, in order to evaluate the potential role of microphytobenthos as a food source for the macrobenthic fauna. Twenty-one stations were sampled in July 2001 and May 2002, with water depth ranging from 16.3 to 68.5 m. High-performance liquid chromatography pigment analyses revealed that concentrations of chlorophyll a, chlorophyll c and fucoxanthin are mainly associated with benthic diatom flora at most parts of the Dogger Bank. High percentage of phytopigments (>50%) was firmly attached to sand grains at the stations shallower than 40 m water depth. The deeper stations were characterized by a phytopigment composition originating from pelagic phytoplankton settled on the sea floor. Qualitative microscopy showed that the benthic microflora on top of the Bank mainly consists of small diatoms (5–10 μm), such as e.g., Diploneis spp., living attached to the sand grains. The results are discussed concerning possible implications for ecology and biogeochemistry of the Dogger Bank area.     

Study of the nutrient and plankton dynamics in Lake Tanganyika using a reduced-gravity model

An eco-hydrodynamic (ECOH) model is proposed for Lake Tanganyika to study the plankton productivity. The hydrodynamic sub-model solves the non-linear, reduced-gravity equations in which wind is the dominant forcing. The ecological sub-model for the epilimnion comprises nutrients, primary production, phytoplankton biomass and zooplankton biomass. In the absence of significant terrestrial input of nutrients, the nutrient loss is compensated for by seasonal, wind-driven, turbulent entrainment of nutrient-rich hypolimnion water into the epilimnion, which gives rise to high plankton productivity twice in the year, during the transition between two seasons. Model simulations predict well the seasonal contrasts of the measured physical and ecological parameters. Numerical tests indicate that the half saturation constant for grazing by zooplankton and the fish predation rate on zooplankton affect the zooplankton biomass measurably more than that of phytoplankton biomass. This work has implications for the application of this model to predict the climatological biological productivity of Lake Tanganyika.     

Significance of nanoplankton in the Chesapeake Bay estuary and problems associated with the measurement of nanoplankton productivity

Over a 2-year program of monthly cruises covering the entire Chesapeake Bay (USA), the phytoplankters which passed 35 μm mesh were responsible for 89.6% of the phytoplankton productivity. On a single summer cruise, the <35 μm phytoplankton fraction was responsible for 93.4% of the chlorophyll a and 100% of the primary productivity. The <10 μm fraction was responsible for 81.3% of the chlorophyll a and 94% of the productivity. The difference in biomass in the <35 μm and the <10 μm fractions was significant (P=0.025), but no significant difference in the productivity could be demonstrated. Laboratory experiments demonstrated that recently assimilated carbon can be lost with gravity screening. Considering both this and the effect of herbivorous zooplankters enclosed in productivity incubations, a prescreening rather than postscreening technique is recommended for studying nanoplankton productivity.