围湖垦殖对湖泊调蓄功能的累加效应分析

计算了长湖、洪湖在围垦前后湖泊容量在水位变化时的容量增长率和四个涝灾年份降雨条件下汛期湖泊水位逐日增加值，对四湖流域尚存的18个湖泊的围垦强度与容量损失情况进行了分析。结果发现，围垦后的长湖容量平均增长率、相对增长率、最大增长率分别从1.8436、0.1834、2.4979(10^8m^3/m）减少到了1.4321,0.1802,1.7569(10^8m^3/m0，洪湖容量平均增长率、相对增长率、最大增长率分别从5.8506、0.3000、6.5095(10^8m^3/m）减少到了3.3970、0.2900、3.4440(10^8m^3/m），围垦导致的湖泊容量损失随着水位上升呈加速增加趋势，随着围垦强度的增加呈加速增加趋势，围垦后这两个湖泊在同样降雨条件下的水位逐日增加值都有不同程度的增加且这种增加值随着雨量和围垦强度的增加而增加。18个湖泊容量变化率随着围垦强度的增加而增加且在围垦强度为40％左右时表现出门槛效应。表明围湖垦残对湖泊调蓄功能的影响具有明显的累加效应。从累加效应的角度对四湖流域围湖垦残的合理性和退田还湖问题进行了讨论。     

城市浅水湖泊治理技术初探

随着生态文明建设的发展,城市浅水湖泊在城市环境中的角色日益重要,环境治理需求日益迫切.针对城市浅水湖泊的污染特征进行了概括总结,并对污染来源进行了分析.根据污染特征及因素针对性提出了“外源性污染、内源性污染控制阶段-水体水质改善与生态系统恢复阶段-长效管理阶段”三个阶段的治理思路,并就各阶段常用的治理技术进行了简单介绍,作为城市浅水湖泊治理工作的参考.     

Managing mercury in the great lakes: an analytical review of abatement policies

Mercury, a toxic metal known to have several deleterious affects on human health, has been one of the principal contaminants of concern in the Great Lakes basin. There are numerous anthropogenic sources of mercury to the Great Lakes area. Combustion of coal, smelting of non ferrous metals, and incineration of municipal and medical waste are major sources of mercury emissions in the region. In addition to North American anthropogenic emissions, global atmospheric emissions also significantly contribute to the deposition of mercury in the Great Lakes basin. Both the USA and Canada have agreed to reduce human exposure to mercury in the Great Lakes basin and have significantly curtailed mercury load to this region through individual and joint efforts. However, many important mercury sources, such as coal-fired power plants, still exist in the vicinity of the Great Lakes. More serious actions to drastically reduce mercury sources by employing alternative energy sources, restricting mercury trade and banning various mercury containing consumer products, such as dental amalgam are as essential as cleaning up the historical deposits of mercury in the basin. A strong political will and mass momentum are crucial for efficient mercury management. International cooperation is equally important. In the present paper, we have analyzed existing policies in respective jurisdictions to reduce mercury concentration in the Great Lakes environment. A brief review of the sources, occurrence in the Great Lakes, and the health effects of mercury is also included.     

硅藻群落指示的近50年来大理西湖湖泊生态系统演变规律

近年来,增强的人类活动使得云南部分湖泊生态系统发生退化,由草型清水态向藻型浊水态转变.全球变化背景下,了解湖泊生态系统演变规律是进行有效管理的前提,具有重要的科学意义.本研究以云南大理州小型浅水湖泊西湖为例,通过对沉积物硅藻群落和理化指标的分析,探讨了20世纪60年代中期以来大理西湖环境演变历程.结果表明,大理西湖生态系统在近50年发生了明显的稳态转换,以2000年为节点,硅藻群落从2000年前偏好贫营养环境的底栖附生种Cocconeis placentula、Staurosira construens、Gomphonema angustum和Achnanthidium minutissimum为优势种的状态,逐渐演替为偏好中营养环境的底栖附生硅藻Encyonopsis microcephala和Navicula cryptocephala及偏好富营养环境的浮游硅藻Cyclotella atomus、Cyclotella meneghiniana、Stephanodiscus hantzschii和Aulacoseira granulata为主导的状态.时间序列的主成分分析表明,硅藻群落主要响应了营养的变化.冗余分析结果也证实营养盐富集是大理西湖硅藻群落长期演化的主要驱动因素.本文论述了近50年来大理西湖流域气候变化和开发活动（农业围垦、化肥施用、畜牧养殖和渔业养殖等）促使湖泊营养盐持续积累,浮游藻类大量繁殖,湖泊内部生产力显著提高,湖泊生态系统逐渐向藻型浊水态转变的演化特征.     

温度对湖泊沉积物中沉水植物残体厌氧分解的影响

淡水湖泊水生植物残体的腐烂分解过程为沉积物中的异养微生物提供了重要的碳源,但是目前关于温度对沉水植物残体有机质分解的影响研究还不够深入.本研究通过室内微宇宙模拟实验,研究了4℃和25℃时马来眼子菜残体在沉积物中厌氧分解特征及其主要的微生物代谢途径.结果表明,温度对马来眼子菜残体的分解影响显著,25℃实验组沉积物中总有机碳（TOC）和纤维素去除率显著高于4℃实验组.25℃实验组沉积物初始腐殖质占TOC比例为18.23%±1.47%,90 d后达到约46%,这说明微生物对马来眼子菜残体的分解促进了沉积物腐质化.此外,温度升高促进了纤维素降解细菌（如拟杆菌门,Bacteroidetes）的生长繁殖,且硫酸盐还原细菌（如GOUTA19、脱硫球菌属（Desulfocuccus）、LCP-6、HB118）和铁还原细菌（如地杆菌属,Geobacter）是沉积物中主要的优势菌种.在25℃条件下,微生物硫酸盐还原、铁还原和产甲烷作用占马来眼子菜残体厌氧代谢的比例分别达到37.3%、27.8%和10.3%.综上所述,本研究表明温度升高促进了沉积物中马来眼子菜残体的厌氧分解,且微生物硫酸盐还原、铁还原和产甲烷过程在其厌氧分解过程中发挥了重要作用.     

我国东部浅水湖泊水生态效应特征

为探究我国东部浅水湖泊生态系统的时空异质性及其演替的响应指标,基于东部浅水湖泊长时间序列（1986-2014年）的监测数据,分析了不同湖泊类型的水质和浮游植物群落分布特征,并综合运用稳态转换理论和典范对应分析方法（CCA）,研究了富营养化湖泊浮游植物群落的演替特征以及响应因子.结果表明:①从水系上看,太湖水系湖泊的水质最差,ρ（TP）、ρ（TN）和ρ（Chla）最高,分别为（0.276±0.606）（3.563±1.430）mg/L和（14.801±10.117）μg/L,SD（透明度）为（0.486±0.272）m;从水文连通性上看,湖泊的水质为通江湖泊>非通江湖泊>阻隔湖泊.②空间分布上,湖口以下干流浮游植物密度最高,为2.674×107 L-1.蓝藻门为东部浅水湖泊的优势种群,密度最高达1.897×107 L-1,绿藻门和硅藻门次之,黄藻门最少,仅为3.951×103 L-1.③东部浅水湖泊生态系统演替发生在ρ（Chla）为5.21~10.57 μg/L阈值范围内.④以东部典型湖泊-太湖为例,浮游植物群落分别在1997-1998年和2000-2001年两个时间梯度达到最大值.EC（电导率）和ρ（TN）是影响太湖浮游植物群落分布的显著因子.研究显示,随着东部浅水湖泊水质恶化,浮游植物群落结构特征发生突变,导致其生态系统发生演替,预防东部浅水湖泊生态系统演变应严控EC和ρ（TN）.      

Potential Effects of Metals in Reacidified Limed Water Bodies in Norway and Sweden

The goal of this work was to assess risk of chemical andbiological effects of metals in reacidified, limed water bodiesin Norway and Sweden. The risk assessment is based on aliterature review and evaluations of water chemical data fromthe 1995 Nordic Lake Survey. Compared to the pre-liming period,it us unlikely that enhanced remobilization of inorganicaluminium (Al) or other toxic metals (metal bomb hypothesis)from the catchment, the lake sediment and/or the streambed willoccur when limed waters reacidify. Rather, the concentrationsin surface waters are expected to be lower than before limingstarted, because of reduced atmospheric inputs of both strongacids and metals as Cd, Hg, Pb, and Zn during the last 10–20 yr. The concentrations in lakes relative to the biologicaleffect levels, as well as the chemical properties of thedifferent metals suggest that the potential biological risksassociated to reacidification of limed lakes decrease in theorder Al > Cd > Pb. The risks associated with Cr, Cu, Fe, Mn, Ni and Zn are very low and do not have to be consideredexcept in waters with known concentrations larger than the lowest biological risk level. Such waters are very rare (<2%). Aluminium is the metal that should be used to set the limit for judging the risk of biological damage due to reacidification of limed surface waters.     

Estimation of Critical Loads of Acidity for Lakes in Northeastern United States and Eastern Canada

The New England Governors and Eastern Canadian Premiers (NEG/ECP) adopted the Acid Rain Action Plan in June 1998, and issued a series of action items to support its work toward a reduction of sulfur dioxide (SO₂) and nitrogen oxide (NO_x) emissions in northeastern North America. One of these action items was the preparation of an updated critical load map using data from lakes in the NEG/ECP area. Critical load maps provide a more complete index of the surface water sensitivity to acidification. Combined sulfur and nitrogen critical loads and deposition exceedances were computed using Henriksen's Steady-State Water Chemistry (SSWC) model. Results show that 28% of all 2053 lakes studied have a critical load of 20 kg/ha/year or less, making them vulnerable to acid deposition. Emission reductions, and more specifically SO₂ emission reductions have proven beneficial because critical loads were exceeded in 2002 for 12.3% of all studied lakes. Those lakes are located in the more sensitive areas where geology is carbonate-poor. Of these lakes, 2.9% will never recover even with a complete removal of SO₄ deposition. Recovery from acidification for the remaining 9.4% of the lakes will require additional emission SO₂ reductions.     

云南九大高原湖泊水体总α、总β调查与评价

报道了对云南九大高原湖泊水体中总α、总β放射性水平的调查结果,并对调查结果进行了分析比较,为开展水体的环境辐射评价提供一定的依据。调查结果表明,这九大高原湖泊水体的总α、总β放射性水平属正常本底水平。