凡纳滨对虾(Litopenaeus vannamei)继饥饿后恢复生长期间生化组成及能量收支的动态变化   总被引：1，自引：0，他引：1       下载免费PDF全文

于赫男  林小涛  许忠能  周小壮 《海洋与湖沼》2008,39(2):124-130

采用氧弹式热量计和常规的动物生化成分分析方法,测定凡纳滨对虾在恢复生长过程中生化组成和能量分配模式的动态变化。结果表明,饥饿状态下,虾体干重、脂肪含量和能值下降,水分和灰分含量升高,但蛋白质含量没有明显改变。恢复投喂后,能量特定生长率显著提高,而虾体各生化组成在不同时间内均恢复到对照组水平。饥饿使对虾恢复生长过程特别是其前期的能量分配模式发生极显著变化。对虾的摄食能分配于生长的比例增大,而损失于代谢消耗的比例则相应减少;摄食能的增加和消化吸收率提高则仅发生在恢复生长的初期。可以认为,凡纳滨对虾继饥饿后的补偿生长效应主要出现在恢复生长的前期,并随时间延长逐步减弱,其生理机制最主要是得益于代谢耗能比例的减少。  相似文献   

Wave breaking on turbulent energy budget in the ocean surface mixed layer   总被引：2，自引：0，他引：2  

孙群  管长龙  宋金宝 《中国海洋湖沼学报》2008,26(1):9-13

As an important physical process at the air-sea interface, wave movement and breaking have a significant effect on the ocean surface mixed layer （OSML）. When breaking waves occur at the ocean surface, turbulent kinetic energy （TKE） is input downwards, and a sublayer is formed near the surface and turbulence vertical mixing is intensively enhanced. A one-dimensional ocean model including the Mellor-Yamada level 2.5 turbulence closure equations was employed in our research on variations in turbulent energy budget within OSML. The influence of wave breaking could be introduced into the model by modifying an existing surface boundary condition of the TKE equation and specifying its input. The vertical diffusion and dissipation of TKE were effectively enhanced in the sublayer when wave breaking was considered. Turbulent energy dissipated in the sublayer was about 92.0% of the total depth-integrated dissipated TKE, which is twice higher than that of non-wave breaking. The shear production of TKE decreased by 3.5% because the mean flow fields tended to be uniform due to wave-enhanced turbulent mixing. As a result, a new local equilibrium between diffusion and dissipation of TKE was reached in the wave-enhanced layer. Below the sublayer, the local equilibrium between shear production and dissipation of TKE agreed with the conclusion drawn from the classical law-of-the-wall （Craig and Banner, 1994）.  相似文献   

Modelling and mass balance assessments of nutrient retention in a seasonally-flowing estuary (Swan River Estuary,Western Australia)     

Barbara J. Robson  Paul A. Bukaveckas  David P. Hamilton 《Estuarine, Coastal and Shelf Science》2008

An integrated mass balance and modelling approach for analysis of estuarine nutrient fluxes is demonstrated in the Swan River Estuary, a microtidal system with strong hydrological dependence on seasonal river inflows. Mass balance components included estimation of gauged and ungauged inputs to the estuary and losses to the ocean (outflow and tidal exchange). Modelling components included estimation of atmospheric (N fixation, denitrification) and sediment–water column nutrient exchanges. Gross and net denitrification derived using two independent methods were significantly correlated (r² = 0.49, p < 0.01) with net rates averaging 40% of gross. Annual nitrogen (N) and phosphorus (P) loads from major tributaries were linearly correlated with annual freshwater discharge and were 3-fold higher in wet years than in dry years. Urban drains and groundwater contributed, on average, 26% of N inputs and 19% of P inputs, with higher relative contributions in years of low river discharge. Overall, ungauged inputs accounted for almost 35% of total nitrogen loads. For N, elevated loading in wet years was accompanied by large increases in outflow (7x) and tidal flushing (2x) losses and resulted in overall lower retention efficiency (31%) relative to dry years (70%). For P, tidal flushing losses were similar in wet and dry years, while outflow losses (4-fold higher) were comparable in magnitude to increases in loading. As a result, P retention within the estuary was not substantially affected by inter-annual variation in water and P loading (ca. 50% in all years). Sediment nutrient stores increased in most years (remineralisation efficiency ca. 50%), but sediment nutrient releases were significant and in some circumstances were a net source of nutrients to the water column.  相似文献   

Enhancement of jellyfish (Aurelia aurita) populations by extensive aquaculture rafts in a coastal lagoon in Taiwan   总被引：1，自引：0，他引：1  

Lo  Wen-Tseng; Purcell  Jennifer E.; Hung  Jia-Jang; Su  Huei-Meei; Hsu  Pei-Kai 《ICES Journal of Marine Science》2008,65(3):453-461

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日粮水平对周期性变温模式下刺参生长和能量收支的影响   总被引：2，自引：2，他引：0  

安振华  董云伟  董双林 《中国海洋大学学报(自然科学版)》2008,38(5)

变温对不同水生生物生长的影响有所不同,对部分种类具有明显的促进作用,而由于种类或温度设置等差异,研究结果各有差异.刺参(Apostichopus japonicus)在生长和生理水平上对一定程度上的符合自然水域温度波动曲线的周期性变温具有积极响应,作者研究在2个变温平均温度(均温15,18 ℃),5个日粮水平(饥饿;0.3%初始体重;0.6%初始体重;0.9%初始体重;1.4%初始体重)下刺参幼参的生长、摄食和能量收支.结果表明,在饱食条件下,刺参在变温条件下生长率高于相应的恒温对照,(15±3) ℃下差异达到显著水平.在各日粮条件下,(15±3) ℃下刺参的生长率均高于(18±3) ℃下对应日粮组.随日粮水平的升高,食物吸收率(FI)和食物转化率(FCE)显著升高.食物转化率变温组均大于恒温处理组,且在均温15 ℃下变温组显著高于恒温组(P<0.05).在能量分配模式中呼吸能占比例最大,且随变温均温升高而显著增加,是造成不同温度下刺参生长率变化的主要因素之一.在(15±3) ℃和(18±3) ℃下,刺参以能量表示的维持日粮值分别为0.39%和0.51%,与相关资料报道的恒温状态下维持日粮相比,一定程度上的变温并不会提高刺参的维持代谢.  相似文献   

Historic changes in flux of matter and nutrient budgets in the Bohai Sea   总被引：1，自引：0，他引：1  

LIU Sumei  ZHANG Jing  GAO Huiwang  LIU Zhe 《海洋学报(英文版)》2008,27(5):81-97

Over the past four periods （ 1959--1960, 1982--1983, 1992--1993, and 1998--1999）, the ecosystem of the Bohai Sea changed due to both a significant decrease of river water discharge from the Huanghe River and a reduction of precipitation. The shifts in nutrient chemistry could result in changes in the phytoplankton composition with an increased potential for non-diatom algal blooms. Simple box model was used to estimate the water - mass balance and nutrient budgets for the Bohai Sea. Water budgets indicate that the residual flow changed from out of the Bohai Sea before 1993, but became inflow to the Bohai Sea after then. The nutrient budgets developed indicate that the Bohai Sea was a sink for nutrients except for phosphate in 1959--1960 and 1982-- 1983 and for silicate in 1982--1983. Net water flow transports nutrients out of the Bohai Sea in 1959--1960, 1982--1983 and 1992--1993, but into the sea in 1998--1999 due to climate changes, such as precipitation and subsequent freshwater discharge. The residual fluxes of nutrients are minor relative to atmospheric deposition and riverine inputs. Conversions of phosphate values to carbon by stoichiometric ratios were used to predict that the system was net heterotrophic before 1982--1983 and net autotrophic after then. Nutrient budgets can explain the change of nutrient concentrations in the Bohai Sea except nitrates, which should include the surface runoff.  相似文献   

热带气旋登陆维持和迅速消亡的诊断研究   总被引：19，自引：6，他引：13  

李英  陈联寿  王继志 《大气科学》2005,29(3):482-490

采用动态合成方法, 对登陆后长久维持热带气旋(LTC)和迅速衰亡热带气旋(STC)的涡度、动能、热量和水汽的收支平衡进行计算和对比分析.结果表明: (1)LTC在陆上长久维持过程中, 其低层正涡度衰减缓慢并保持一定强度.STC登陆后正涡度减弱较快.(2)热带气旋登陆后涡度的收支主要取决于水平散度项、平流项和剩余项.散度项使LTC低层正涡度增加, 高层减少, 平流项和剩余项则使其低层涡度减弱, 高层涡度增加.总体而言, LTC自高层获得正涡度的补充, STC则没有获得环境正涡度.(3)低层, 摩擦耗散使LTC动能减少, 但动能通量辐合可补充部分动能而减缓衰减.中高层, LTC登陆后36～60 h动能收大于支, 动能的增加一部分来自于斜压动能制造, 一部分来自于次网格尺度.STC有类似的动能耗散, 却无动能补充.(4)LTC登陆后保持一定强度, 并从外界获得热量和水汽补充来支持积云对流发展, 而积云对流对LTC的维持具有正反馈作用.STC登陆后没有这一过程.  相似文献   

亚洲通量观测网建立的回顾与展望     

山本晋  三枝信子  蒲生稔  FUJINUMA Y  INOUE G  HIRANO T 《地理学报(英文版)》2005,15(2):142-148

1IntroductionTheelucidationofthebudgetsofcarbon,waterandothermassesatvariouslandecosystemshasbecomeanimportantsubjectintheglobalwarmingissue.Forthisstudy,thedatafrompreciseandlong-termobservationsofcarbondioxide,watervapor,andheatfluxtakeninvariouslandsur…  相似文献   

基于主体功能区的京津冀城市群碳收支时空分异与碳补偿分区   总被引：2，自引：0，他引：2  

夏四友  杨宇 《地理学报》2022,77(3):679-696

从主体功能区划视角研究碳收支和碳补偿分区,对于制定适应各主体功能区低碳发展策略,推动区域生态环境协同治理,实现高质量发展具有重要意义,也是地理学思想对于实现“双碳”目标的重要贡献。本文首先构建主体功能区视角下碳收支与碳补偿的理论框架,然后以京津冀城市群157个县级单元为研究区,引入集中化指数、标准显性比较优势指数、SOM-K-means聚类等方法研究功能区视角下京津冀城市群碳收支时空分异与碳补偿分区,并提出以低碳发展为导向的碳减排空间优化方案。结果表明：① 2000—2017年京津冀城市群碳收支量呈现波动上升态势,其集中化指数均高于0.4的“警戒线”,碳收支地区差异整体偏大。② 碳收支时空分异显著,碳排放高值区呈现以京津唐为中心,向外逐步降低的“核心—外围”空间格局;而碳吸收空间格局趋于稳定,总体呈现东、北、西部高,而中、南部低的倒“U”型格局。③ 京津冀城市群碳收支与主体功能区战略定位较为吻合,优化开发区和重点开发区是碳排放的主要承压区,而重点生态功能区是碳吸收的优势主导区,各功能区碳吸收集中化指数差别较碳排放集中化指数小。④ 京津冀城市群共有53个支付区、64个平衡区和40个获补区,结合主体功能区规划战略目标,最终形成9类碳补偿空间优化区,并提出每一类型区低碳发展方向及策略。⑤ 未来要加强更微观尺度的碳收支及碳补偿研究,丰富和完善碳补偿理论框架,将碳补偿融入到碳交易市场,探索实现“双碳”目标的多元化路径。  相似文献   

青藏高原大气水汽收支特征及影响     

柏晶瑜  徐祥德 《地理学报(英文版)》2004,14(1)

Based on 1961-2000 NCEP/NCAR monthly mean reanalysis datasets, vapor transfer and hydrological budget over the Tibetan Plateau are investigated. The Plateau is a vapor sink all the year round. In summer, vapor is convergent in lower levels (from surface to 500 hPa) and divergent in upper levels (from 400 to 300 hPa), with 450 hPa referred to as level of non-divergence. Two levels have different hydrologic budget signatures: the budget is negative at the upper levels from February to November, i.e., vapor transfers from the upper levels over the plateau; as to the lower, the negative (positive) budget occurs during the winter (summer) half year. Evidence also indicates that Tibetan Plateau is a "vapor transition belt", vapor from the south and the west is transferred from lower to upper levels there in summer, which will affect surrounding regions, including eastern China, especially, the middle and lower reaches of the Yangtze. Vapor transfer exerts significant influence on precipitation in summertime months. Vapor transferred from the upper layers helps humidify eastern China, with coefficient -0.3 of the upper budget to the precipitation over the middle and lower reaches of the Yangtze (MLRY); also, vapor transferred from east side (27.5°-32.5°N) of the upper level has remarkable relationship with precipitation, the coefficient being 0.41. The convergence of the lower level vapor has great effects on the local precipitation over the plateau, with coefficient reaching 0.44, and the vapor passage affects the advance and retreat of the rainbelt. In general, atmospheric hydrologic budget and vapor transfer over the plateau have noticeable effects on precipitation of the target region as well as the ambient areas.  相似文献