小型湖泊应用于地表水源热泵时的热承载能力分析

分析了小型湖泊应用于地表水源热泵时的两种热承载能力计算方法——水面温度法和均匀混合法,并采用其计算了杭州小型湖泊应用于地表水源热泵时的热承载能力。计算结果表明：水面温度法较客观地反映了实际的排水混合及水温恢复过程,可信度更高。用水面温度法对7个代表性城市小型湖泊热承载能力进行分析的结果表明：夏季热承载能力在23-4—29．5W／m2之间,冬季热承载能力在31．6～45．7W／m2之间;设计这类系统的关键在于满足夏季热承载能力的约束。     

三峡水库蓄水期长江中游湖泊调蓄能力变化

长江中游通江湖泊的调蓄能力与整个区域的水安全密切相关。在对洞庭湖、鄱阳湖(下称“两湖”)调蓄机理探讨的基础上,揭示了两湖泊调蓄的临界状态及临界条件,分析了三峡水库蓄水期两湖泊调蓄能力的变化。研究结果表明:洞庭湖与鄱阳湖具有相同的调蓄机理,其调蓄能力变化受入湖流量和长江干流顶托的双重影响,湖泊调蓄过程表现为入湖与出湖水量的动态调整,湖泊调蓄量不断向0趋近。三峡水库运用后,两湖泊9—10月份调蓄能力下降明显,与2003—2007年相比,2008—2014年两湖汛后调蓄水量的减小更大。     

我国盐湖资源开发利用的现状及对策分析

我国盐湖资源丰富,蕴藏着极其丰富的石盐、钾、锂、镁、溴、硼、芒硝、铷、铯等有用资源,开发及应用前景极其广阔.盐湖资源综合利用新技术研究及整体开发,有利于提高资源利用率和企业经济效益,保障资源的可持续发展.文章概述了我国盐湖的资源概况,论述了盐湖资源综合利用的研究及开发现状,指出了盐湖资源综合开发利用中存在的问题,并提出了相应的建议.     

The impact of tourism on dune lakes on Fraser Island, Australia

In view of the increasing tourism to Fraser Island, Queensland, a tourist pressure index (TPI) was developed to assess the potential threat of tourism to 15 of the most accessible dune lakes on the island. Tourist pressure index scores indicated that the two clear lakes on the island, Lake McKenzie and Lake Birrabeen, are most threatened by tourist activities owing to their accessibility, facilities and prominence in advertising campaigns. In addition, limnological investigations of the same 15 lakes were conducted in February 1999 to determine their current trophic status and potential susceptibility to adverse impacts from tourism, particularly with reference to eutrophication. On the basis of nutrient and chlorophyll a concentrations, the two water table window lakes, Ocean Lake and Lake Wabby, were classed as mesotrophic and oligo‐mesotrophic, while all of the perched dune lakes were oligotrophic. Lake McKenzie and Lake Birrabeen, the two most threatened lakes according to TPI scores, had the lowest nutrient concentrations of all of the lakes examined and, consequently, we suggest that nutrient additions might elicit rapid algal growth responses in these systems. Comparisons between current data and historical data from Arthington et al. (1990 ) indicate that increases in planktonic chlorophyll a concentrations were not always directly mirrored by increases in total phosphorus concentrations. We found that while chlorophyll a concentrations were significantly higher in the 1999 samples than in the 1990 samples for all lakes, total phosphorus concentrations were higher in Ocean Lake, lower in Lake Jennings and similar in lakes McKenzie, Birrabeen and Wabby.     

青藏高原典型河流与湖泊表层水体碳时空变化特征初步分析

为了研究青藏高原典型河流与湖泊水体碳时空变化特征,采集了典型河流、湖泊、冰川等水体样品,通过实验室测试分析获取了总碳、无机碳和有机碳观测数据。结果表明青藏高原典型河流与湖泊水体碳以无机碳为主、有机碳为辅。其中,长江、黄河和澜沧江源区典型河流与湖泊水体总碳平均含量分别为62.46,32.88,17.70 mg/L,长江南源当曲源、正源沱沱河源和北源楚玛尔河源水体总碳含量分别为32.90,36.56,32.90 mg/L;青藏高原封闭性湖泊水体碳含量比河流水体较高,封闭性湖泊水体总碳、总无机碳和总有机碳平均含量分别为403.82,398.35,1.24 mg/L,而河流水体则分别为17.03,14.56,2.46 mg/L,河流水体有机碳含量比封闭性湖泊水体较高。该成果可为我国青藏高原水域碳循环研究提供基础数据,对高海拔区域气候变化研究具有参考价值。     

How light conditions influence theoretical pelagic to benthic primary production ratios in small lakes

Theoretical pelagic primary production of phytoplankton and benthic primary production of periphyton were modelled for two small lakes in Estonia (Northeast Europe). Although located only 500 m apart, the water colour and light attenuation of these two lakes differed markedly. The Secchi depth (SD) in the clear‐water lake was 4.5 m and only 0.47 m in the dark‐water lake. The total phosphorus (TP) concentrations were, respectively, 15 μg/l and 28 μg/l. An empirical model whose inputs were morphometric, light conditions and dissolved organic carbon parameters obtained from in situ measurements was employed for the present study. The model calculated primary production with a time‐step of 10 min, and a spatial resolution of 10 cm, from sunrise to sunset and from lake surface to lake bottom. The primary production of periphyton and phytoplankton was almost equal in the clear lake, whereas only phytoplankton contributed to whole‐lake primary production in the dark lake because of the stronger light attenuation in the water column. The results of the present study indicated the depth‐distribution profiles differed dramatically between the two lakes. The clear lake had a deep, U‐shaped curve, with the productive layer reaching considerable depth soon after sunrise and maintaining a similar profile throughout the light hours. In contrast, the dark lake production declined rapidly with increasing depth, whereas the profile changed over the day reaching the greatest depth at noon.     

建设大王滩湿地公园的必要性和可行性分析

通过实地调查和资料分析,从大王滩国家湿地公园建设的优势和综合效益等方面分析了建设大王滩湿地公园的必要性和可行性,该湿地公园以水源地保护为主要功能,在保护湿地生态系统的基础上,供人们进行科学研究和合理开展生态旅游。     

广州花都湖工程规划设计

对花都湖工程的规划设计进行介绍,规划方案注重保护河道自然生境,充分利用历史和现状场地条件,突破了以往传统水利工程的生硬、单一和枯燥,将水安全、水生态、水文化、水景观融为一体,为河道整治、人工湖建设与现代城市水利建设理念相结合提供了一宗成功的案例。     

What makes an elongated lake ‘large’? Scales from wind-driven steady circulation on a rotating Earth

When investigating wind-induced steady circulation, the effect of the acceleration due to Earth’s rotation is often neglected in narrow lakes, but the argument behind this assumption is blurred. Commonly, when the horizontal dimension is smaller than the Rossby radius, the Coriolis force is considered unimportant, but this is correct only for inertial currents and barotropic and baroclinic waves. In this work, we revisit the classical Ekman transport solution for wind stress acting along the main axis of an elongated lake in steady-state conditions. We demonstrate that a secondary circulation develops and that the resulting crosswise volume transport, constrained in the closed domain, produces downwelling and upwelling that cannot be predicted by the standard Ekman formulas. We claim that the Rossby radius does not play any role in this process, which on the contrary is governed by the ratio between the actual depth and the thickness of the Ekman layer. The theoretical analysis is supported by numerical experiments to show the dependence on latitude, width, depth and turbulence closure.     

The thermal behaviour of French water bodies: From ponds to Lake Geneva

The management of French freshwater bodies (lakes, reservoirs, ponds, etc.) needs to face the challenges imposed by the effects of climate change and by legal requirements to develop standards for water temperature and other physicochemical indicators. While 1D hydrodynamical models could be helpful in improving the knowledge of the thermal and hydrodynamic behaviour of French water bodies, the scarcity of data for calibration and validation, in addition to the unavailability of some forcing data, makes their application difficult for most French water bodies. In this article we explore an alternative statistical approach that takes advantage of the available data in order to inform future modelling applications. We used official monitoring data and satellite measurements to study the thermal characteristics of more than 400 French water bodies (depth: 1–310 m, surface area: 0.1–577 km², volume: 0.1–89,000 hm³). The objective was to identify the importance of size on their thermal behaviour. For this we analysed the annual temperature cycle, the summer temperature profiles and within-lake spatial variability. Together with size, geography and transparency determine the thermal behaviour of water bodies through complex interactions. As a result of the analysis we propose a classification of French water bodies as a function of depth and surface area that reflects the summer vertical temperature gradient and the processes influencing the deepening of the thermocline.