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1.
太湖不同生态类型湖区浮游甲壳动物群落结构季节变化比较 总被引：1，自引：0，他引：1
水体富营养化会对整个水生态系统产生重要影响.为了解太湖富营养化对浮游甲壳动物群落结构的影响,于2012年3月至2013年2月对太湖3个典型湖区——藻型湖区(梅梁湾)、草型湖区(胥口湾)和强扰动湖区(湖心区)开展浮游甲壳动物群落结构季节变化比较研究.3个湖区中,湖心区营养水平最高,胥口湾最低.梅梁湾浮游甲壳动物密度和生物量最高,其次是湖心区,胥口湾最低.梅梁湾、湖心区和胥口湾的浮游甲壳动物年平均密度分别为199、150和91 ind./L,年平均生物量分别为1.950、1.557和0.743 mg/L.在整个研究期间,梅梁湾、胥口湾和湖心区的浮游甲壳动物种类数分别为13、11和11;3个湖区的浮游甲壳动物优势种均为中华窄腹剑水蚤和简弧象鼻溞,其中中华窄腹剑水蚤在梅梁湾、胥口湾和湖心区的年平均密度分别为57、25和36 ind./L,简弧象鼻溞在3个湖区的年平均密度分别为40、22和32 ind./L.胥口湾浮游甲壳动物生物多样性指数显著低于梅梁湾和湖心区.相关分析表明,浮游甲壳动物密度与叶绿素a浓度呈极显著正相关.研究表明,同一湖泊不同生态类型湖区浮游甲壳动物会对水体富营养化产生不同的生态响应. 相似文献
2.
太湖悬浮颗粒物细菌碱性磷酸酶编码基因的分布特征 总被引：1，自引：0，他引：1
颗粒态有机磷的碱性磷酸酶矿化是水生态系统磷循环的重要环节,对细菌碱性磷酸酶编码基因的解析有利于揭示浅水富营养化湖泊有机磷矿化的微生物驱动机制.本文以太湖不同生态类型湖区悬浮颗粒物为研究对象,运用荧光定量PCR技术,探究太湖水体中悬浮颗粒物细菌碱性磷酸酶phoX和phoD基因的时空分布特征,以及影响两类基因丰度的主要环境因子.结果表明：太湖不同生态类型湖区中phoD基因丰度是phoX基因的6~42倍,且二者均存在显著的时空分布差异.6月,河口区phoX（9.18×104 copies/L）和phoD（1.88×106 copies/L）基因丰度均最高,其次分别为草型区、湖心区和藻型区.与6月相比,9月各湖区phoD基因丰度显著降低,而phoX基因丰度在藻型区和草型区则有所升高.9月,草型区phoX基因丰度最高（5.70×104 copies/L）,河口区最低（1.49×104 copies/L）.水生植物对phoX和phoD基因丰度具有重要贡献.悬浮颗粒物细菌phoX基因丰度可能被低估.溶解氧、总氮和总磷是影响太湖phoX和phoD基因丰度的主要环境因子. 相似文献
3.
太湖浮游细菌种群基因多样性及其季节变化规律 总被引：8，自引：3，他引：5
为认识湖泊中浮游细菌的多样性及其变化规律,本研究采用聚合酶链式反应-变性梯度凝胶电泳(PCR-DGGE)的方法,研究了太湖梅梁湾和湖心区浮游细菌种群16S rRNA基因多样性以及种群基因组成的季节变化特征.研究结果表明,太湖浮游细菌种群具有丰富的基因多样性.浮游细菌的丰度、DGGE条带数、种群的Shannon-Wiener指数、Simpson 指数和Pielou指数均呈现显著的季节变化规律:夏季及秋季浮游细菌的丰度、基因多样性及种群的均匀度较高,而冬季和春季则较低.浮游细菌种群的基因组成随时间变化.梅梁湾浮游细菌的丰度显著高于湖心.梅梁湾与湖心浮游细菌主要建群种的基因型存在显著差异. 相似文献
4.
针对近年来太湖水体中长孢藻（Dolichospermum,曾用名鱼腥藻Anabaena）比例增加的趋势,本文研究了2005—2019年太湖春季不同湖区长孢藻生物量的长期变化趋势和空间差异,探究了冬、春季气象条件（气温、日照时长、风速、降雨量）和营养盐（总氮、总磷）水平对其的影响.结果表明,2005—2019年太湖监测数据显示春季长孢藻生物量有比较明显的升高现象,主要发生在竺山湖富营养程度较高的区域,其次是湖心区、梅梁湾和南部湖区.偏最小二乘路径建模（PLS-PM）结果表明,不同湖区长孢藻生物量变化的主要驱动因素存在差异.在湖心区,春季长孢藻的生物量主要受冬季气候条件（气温、风速、日照时长）的影响,其次受春季营养盐和春季气候条件的影响.在梅梁湾、竺山湖和南部湖区,春季长孢藻的生物量主要受春季气候条件的影响.在梅梁湾和竺山湖,春季风速、日照时长是春季长孢藻生物量的显著影响因子;在南部湖区,春季长孢藻生物量的主要驱动因素是春季的日照时长和春季气温.本研究从长时间序列角度,对太湖固氮蓝藻的时空分布特征和影响因素开展了研究,为太湖不同湖区开展针对性的藻类水华防控和富营养化治理提供理论基础. 相似文献
5.
太湖流域水污染控制与生态修复的研究与战略思考 总被引：16，自引：2，他引：14
为了探明太湖水体中胶体磷含量,更深入认识营养盐在大型浅水湖泊中的循环过程和机理,分别从太湖的梅梁湾和贡湖湾两个不同类型的湖区采集水样,利用切向流超滤方法分离出胶体物质,对太湖水体中胶体磷含量进行了初步研究．结果表明:太湖水体春季胶体磷含量在0．017-0．029 mg／L间,其中梅梁湾藻型湖区胶体磷含量范围是0 023- 0．029 mg／L,贡湖湾草型湖区胶体磷含量在0．017-0．022 mg／L间．梅梁湾水体胶体磷占总磷比例平均为28．6%;而贡湖湾胶体磷占总磷比例平均达到39．3%．梅梁湾水体真溶解态磷含量显著高于贡湖湾水体,达贡湖湾的4倍．与澳大利亚的17个湖泊相比,太湖属胶体磷含量偏低的湖泊,但相对于海洋的研究结果,太湖胶体磷含量明显偏高． 相似文献
6.
水深是影响浅水湖泊沉水植物生长的主要因素之一.莲座型苦草（Vallisneria natans）和冠层型穗花狐尾藻（Myriophyllum spicatum）是我国长江中下游浅水湖泊中常见的沉水植物种类,二者在形态特征上具有较大的差异.在自然水体中,水深变化对这两种植物的生长以及竞争格局的影响还有待研究.本文设计了3个水深梯度（水深0.5、1.5、2.5 m）,探讨混栽条件下苦草和穗花狐尾藻生长和竞争格局对水深变化的响应.结果显示在实验系统内,中水深（1.5 m）处理组对两种植物的生长均最有利,表现为两种植物的相对生长率和生物量均最高.低水深（0.5 m）处理组苦草的生物量和相对生长率均显著低于高水深（2.5 m）处理组;穗花狐尾藻则相反,高水深对其生长的抑制作用更大.2种沉水植物在高水深胁迫时均表现出地上部分（叶长或茎长）增加,地下部分（根长）减少的形态响应特征.此外,随着水深由高到低,苦草与穗花狐尾藻生物量之比逐渐减小,表明苦草在两种植物中的竞争优势逐渐降低.研究表明湖泊水深变化不仅能够影响沉水植物的丰度,同时还可能会影响沉水植物的群落结构,而在我国浅水湖泊的生态修复实践中,在通过水位调控恢复沉水植物时,调控范围应考虑目标植物（如苦草）的光合特征. 相似文献
7.
过去40年,全球气候变暖、辐射变暗和变亮、风速减弱、气候异常波动等自然环境变化以及筑坝建闸、岸堤硬质化和调水引流等强烈人类活动势必会深刻改变太湖湖泊物理环境和过程,驱动湖泊生态系统演化.基于历史文献、档案数据以及气象水文和透明度等长期观测数据,本文系统梳理了太湖气温、水温、风速、水位和透明度等物理环境空间分布和长期变化特征,探讨了气温和风速、水位和透明度相互协同作用机制及其潜在生态环境意义.受全球变化和城市化等影响,过去40年太湖气温和水温呈现显著升高趋势,而近地面风速则表现为持续下降,湖泊增温和风速下降有利于藻类生长和蓝藻水华漂浮聚集,某种程度上增加了蓝藻水华出现频次和集聚的面积.为防洪和满足流域日益增长的水资源需求,闸坝管控和调水引流使太湖水位呈现缓慢增加趋势,而入湖污染物增加和富营养化则造成水体透明度逐渐下降,致使透明度与水位(水深)的比值明显降低,减少了湖底可利用光强,恶化水下光环境,在一定程度上驱动了太湖水生植被和草型生态系统退化.湖泊物理环境长期变化逐渐拓展了太湖藻型生境空间而压缩了草型生境空间,加剧了草型生态系统向藻型生态系统转化和增强了藻型生态系统的自我长期维持.太湖湖泊物理环境的显著变化也会部分抵消流域营养盐削减和湖体营养盐下降对藻类生物量和蓝藻水华的控制,增加了太湖蓝藻水华防控和湖泊富营养化治理的难度.这意味着未来流域控源截污需要更加严格的标准,而湖泊水位等物理环境的有效管控是应对藻华加剧和恢复草型生态系统的适应性管理策略. 相似文献
8.
长江中下游湖泊沉积物中磷的形态及藻类可利用量 总被引：13，自引：1，他引：13
调研了长江中下游地区25个浅水湖泊的35个样点表层沉积物中磷的地球化学形态特征,以及太湖沉积物中藻类可利用磷(AAP)的空间分布,垂向分布特征及其蓄积量,探讨了浅水湖泊表层沉积物中磷的赋存量,地球化学形态及其与水草,湖水磷浓度,叶绿素(Chl-a)浓度之间的关系.结果表明,长江中下游地区浅水湖泊的表层沉积物中可交换态磷(Ex-P)含量与水体总磷(TP),溶解性总磷(DTP)及溶解性反应活性磷(SRP)浓度关系密切,有水草湖区的沉积物中生物易利用磷(Bio-P)含量显著低于无水草湖区及藻型湖区.太湖梅梁湾沉积物泥芯中,表层3 cm沉积物中Ex-P含量显著增高,而夏季还原条件下容易转变为溶解态磷的铁磷(Fe-P)含量峰值则出现在4～10cm深度.太湖表层沉积物的Bio-P含量与夏季叶绿素浓度密切相关,说明表层沉积物的Bio-P及AAP可以作为沉积物内源释放风险的指示参数.太湖表层1 cm底泥中所含有的AAP量估计多达268.6吨,风浪扰动能将大量的AAP带入水体,对太湖蓝藻水华暴发起着不可忽视的作用. 相似文献
9.
微生物是湖泊生态系统重要的有机组分。了解不同时期青藏高原湖泊细菌群落特征、环境驱动因子及其群落构建过程的差异,对高原湖泊水生态管理具有重要的指导意义。分别于2020年6和12月采集青藏高原东北部5个湖泊水样,基于高通量测序技术、统计分析和模型分析,解析高原湖泊群在非冰封期和冰封期细菌群落结构、环境驱动因子和中性过程、确定性过程以及随机性过程在细菌群落构建过程的贡献。结果表明：（1）非冰封期湖泊细菌群落的Chao1丰度指数、Simpson和Shannon多样性指数低于冰封期,Spearman相关性分析结果表明非冰封期细菌群落的Chao1丰度指数和多样性指数与水温和海拔显著相关,而冰封期细菌群落的Chao1指数和多样性指数与总氮显著相关;（2）水体细菌群落的优势门均为变形菌门（Proteobacteria）,非冰封期细菌中拟杆菌门（Bacteroidetes）、放线菌门（Actinobacteria）和厚壁菌门（Firmicutes）的平均相对丰度明显高于冰封期。另外,主坐标分析和相似性分析结果表明非冰封期和冰封期的细菌群落组成差异极显著;（3）冗余分析结果表明不同时期湖泊群细菌群落结构的... 相似文献
10.
太湖草/藻型湖区沉积物-水界面环境特征差异 总被引：3，自引：0，他引：3
在太湖草、藻型湖区进行冬、夏两季多点采样,分别对采样点的水环境特征、泥面以上5 cm上覆水中营养盐以及沉积物的含水量、中值粒径、有机碳、氮、磷、金属元素和溶解氧进行测定.结果表明:夏季藻型湖区表层水体pH高于中、底层,冬季草型湖区各层水体pH高于藻型;草型湖区水体浊度夏季低于藻型,冬季反之;藻型湖区上覆水中的硝态氮和磷酸根浓度显著高于草型;草型湖区沉积物中含水量冬季显著高于夏季;草型湖区沉积物中总有机碳显著高于藻型;Fe、Zn、Ca、Pb、Na和K等元素在草、藻型湖区间差异显著;沉积物中溶解氧表现为冬季深于夏季,藻型深于草型的规律. 相似文献
11.
A non-linear morphodynamic model of a microtidal coastal shelf is used to study the response of shoreface-connected sand ridges and the net sand balance of the shelf to large-scale interventions. The model describes the interaction between storm-driven currents and the erodible bottom. The transport of sediment comprises both bedload and suspended load contributions and is due to the joint action of waves (stirring of sediment from the bed) and net currents (causing transport). Three basic types of interventions are studied: extracting sand from ridges, nourishing sand at the shelf and constructing navigation channels. The model results indicate that for all interventions studied a relatively fast local recovery (time scale of decades to centuries) of the disturbed bathymetry to its original pattern takes place. Readjustment of the global system to its original equilibrium state (the saturation process) occurs on a longer time scale (several centuries). During the adjustment stage, significant net sand exchanges between inner shelf and adjacent outer shelf and near-shore zone occur. The results further suggest that extraction of sand from the shelf and dredging of navigation channels have negative implications for the stability of the beach (its sand volume decreases).Responsible Editor: Iris Grabemann 相似文献
12.
The geology of Western and Central Europe is significantly influenced by the Variscan orogen that developed during Devonian and Carboniferous time. Numerical models are essential in understanding and quantifying the involved endogenous and exogenous processes and their interactions. These are mainly based on the large-scale mass redistribution caused by erosion and fluvial sedimentary transport. The sedimentary mass flux leads to changing loads on the lithosphere and affects therefore the evolution of the orogen and the foreland-basin. The complex feedback-mechanism of the surface and tectonic processes is studied by three-dimensional elastic–plastic numerical models. The calculated uplift rates are used to model the interaction between tectonic and surface processes such as erosion and sedimentation. An iterative application of the numerical models for the tectonic and surface processes yields a detailed view of the evolution of the foreland-basin. The tectonic model itself (excluding surface processes) already shows some of the palinspastically reconstructed important features of the lower Carboniferous like the London-Brabant Massif, and the northward propagation of the Variscan deformation front. The results obtained from the coupled analysis can be compared to studies of the sedimentary record (i.e. time, thickness, and sedimentation rates) and other geological concepts (i.e. stability of geological provinces). The results demonstrate that both processes are essential in understanding the complex structural evolution of the Variscides and their foreland. The numerical approach on the tectonic–surface process interaction can also be applied easily to other geological settings. 相似文献
13.
本文综述了国外近年来在不完美岩浆过程中微量元素效应研究方面的进展。在完美平衡过程（平衡部分熔融或者平衡部分结晶）中和在完美分离过程（分离熔融或者分离结晶）中，熔融或者结晶对于高度不相容元素和高度相容元素相对浓度变化的差异悬殊的影响效应是众所周知的。完美分离过程需要满足以下３个条件：（１）每一批次被分离的熔体或者晶体的量趋向于无穷小；（２）晶体与熔体的彻底分离；（３）体系相对于源区物质和残留物质是完 相似文献
14.
Abstract In this paper a method for solving the equation for the mean magnetic energy <BB> of a solar type dynamo with an axisymmetric convection zone geometry is developed and the main features of the method are described. This method is referred to as the finite magnetic energy method since it is based on the idea that the real magnetic field B of the dynamo remains finite only if <BB> remains finite. Ensemble averaging is used, which implies that fields of all spatial scales are included, small-scale as well as large-scale fields. The method yields an energy balance for the mean energy density ε ≡ B 2/8π of the dynamo, from which the relative energy production rates by the different dynamo processes can be inferred. An estimate for the r.m.s. field strength at the surface and at the base of the convection zone can be found by comparing the magnetic energy density and the outgoing flux at the surface with the observed values. We neglect resistive effects and present arguments indicating that this is a fair assumption for the solar convection zone. The model considerations and examples presented indicate that (1) the energy loss at the solar surface is almost instantaneous; (2) the convection in the convection zone takes place in the form of giant cells; (3) the r.m.s. field strength at the base of the solar convection zone is no more than a few hundred gauss; (4) the turbulent diffusion coefficient within the bulk of the convection zone is about 1014cm2s?1, which is an order of magnitude larger than usually adopted in solar mean field models. 相似文献
15.
Miniature sorted patterned ground features (nets and stripes) occur at an elevation of ca. 35 m in the L'Antioja valley, East Falkland. The features have developed following recent soil erosion and display many of the characteristics associated with the operation of frost-related processes in regolith materials. The patterns are currently active and indicate that in cool oceanic climates the distribution of frost-sorted patterns is controlled by the presence of bare ground on suitable regolith rather than by altitude. 相似文献
16.
Measurements from recently installed 5 MHz high-frequency radar (CODAR) stations south of Point Arena, California, are used to describe surface current patterns during the upwelling season (June-August 2007). The systems provide hourly current maps on a 5-km grid, covering a region from approximately 10 to 150 km offshore (the continental shelf into the deep ocean). These HF-radar observations provide an unprecedented view of circulation in this “coastal transition zone”, between the wind-driven circulation over the shelf and the California Current circulation offshore. Circulation patterns include: (1) bifurcation of the coastal upwelling jet downstream of Point Arena into an along-shelf (down-coast) branch and an offshore branch, and (2) a large-scale anticyclonic meander that often develops into an eddy-like recirculation south of the bifurcation. The “recirculation” feature extends well offshore, with surface currents 50-100 km from the coast consistently opposing the wind stress. The spatial and temporal evolution of the surface current features during upwelling events affects surface transport from Point Arena to areas in the south, increasing the travel time of a substantial fraction of newly upwelled water from a few days to roughly two weeks. Thus, surface currents even far offshore influence coastal transport of nutrients, phytoplankton and larvae on ecologically relevant timescales, with resultant connectivity patterns very different than implied by a simple examination of the mean flow. 相似文献
17.
Postglacial topographic evolution of glaciated valleys: a stochastic landscape evolution model 总被引：1，自引：0，他引：1
The retreat of valley glaciers has a dramatic effect on the stability of glaciated valleys and exerts a prolonged influence on the subsequent fluvial sediment transport regime. We have studied the evolution of an idealized glaciated valley during the period following retreat of ice using a numerical model. The model incorporates a stochastic process to represent deep‐seated landsliding, non‐linear diffusion to represent shallow landsliding and an approximation of the Bagnold relation to represent fluvial sediment transport. It was calibrated using field data from several recent surveys within British Columbia, Canada. We present ensemble model results and compare them with results from a deterministic linear‐diffusion model to show that explicit representation of large landslides is necessary to reproduce the morphology and channel network structure of a typical postglacial valley. Our model predicts a rapid rate of fluvial sediment transport following deglaciation with a subsequent gradual decline, similar to that inferred for Holocene time. We also describe how changes in the model parameters affect the estimated magnitude and duration of the paraglacial sediment pulse. Copyright © 2005 John Wiley & Sons, Ltd. 相似文献
18.
Susan Friedlander 《地球物理与天体物理流体动力学》2013,107(1-2):151-167
Abstract The effects of compressibility on the stability of internal oscillations in the Earth's fluid core are examined in the context of the subseismic approximation for the equations of motion describing a rotating, stratified, self-gravitating, compressible fluid in a thick shell. It is shown that in the case of a bounded fluid the results are closely analogous to those derived under the Boussinesq approximation. 相似文献
19.
Ourania Tzoraki Nikolaos P. Nikolaidis Anna Rosa Trancoso Frank Braunschweig Ramiro Neves 《水文研究》2009,23(2):272-283
The RS‐tempQ Model ( r each– s cale t emporary flow biogeochemical model) is a conceptual model that can describe the hydrologic, sediment transport and biogeochemical processes of temporary rivers at the reach scale. The model takes into account the expansion–contraction of the inundated area of the river. It simulates the sediment transport and the nutrient fluxes that are transferred to the coastal area due to the first flash flood and during extreme rain events. The RS‐tempQ Model simulates the in‐stream processes during the wet and dry cycles as the river corridor expands and contracts. The model was used to assess and quantify the hydrologic and geochemical processes occurring in a temporary river reach (Krathis River) in Greece. Since the conventional gauging techniques cannot measure the flow in rivers that are split into small braided streams, discharge measurements could not be obtained in order to calibrate and verify the model. Other field measurements such as infiltration losses and sediment accumulation were used for model calibration. Copyright © 2008 John Wiley & Sons, Ltd. 相似文献
20.
Lon D. Drake 《地球表面变化过程与地形》1977,2(4):309-317
The fabrics of tills deposited by continental glaciers are usually assumed to reflect clast orientation during transportation and yet might only be imprinted during depositional processes. However, the striated surfaces of clasts must be acquired during transportation and by relating striation patterns to clast shape one can deduce the positions most frequently maintained by each group of clasts. Comparison of these orientations with the actual depositional fabrics of the same shape groups, demonstrates that dast orientations are maintained from transportation through deposition. Therefore subglacial transportation processes grade smoothly into those of deposition. The favoured interpretation is that bottom melting is the dominant mechanism leading to final deposition and that lodgement and smearing are likely restricted more to preliminary cycles of redeposition and re-erosion. 相似文献