惠州西湖磷模型的初级研究

国家4A旅游景区之一的惠州西湖地处亚热带地区,属于典型的浅水型城市湖泊.在西湖水体完全混合的假设和西湖实地调查和2003年～2005年监测数据的基础上,对惠州西湖建立了零维总磷模型.文中对总磷模型进行了参数的率定、校正,并用模型对2003年10月到2004年9月一周年进行总磷浓度的模拟预测,从而验证了该模型在惠州西湖水质预测中的适用性和可行性.根据西湖底泥磷释放率的特征提出修正模型,大大降低了原模型模拟误差,更精确拟合惠州西湖的总磷浓度的动态变化,有助于西湖的长期预测工作的进一步开展.     

惠州西湖去除鱼类对水体磷浓度的影响

鱼类对水生生态系统的营养盐循环特别是磷循环产生重要影响.该文以惠州西湖予湖--南南湖(面积1.2×105m2)为研究对象,通过对其中鱼类的去除,研究分析了磷的变化.结果表明:水体总磷在鱼类去除后短期内浓度上升明显,与颗粒态磷浓度有显著的正相关关系;同时,叶绿素a浓度也明显上升;而溶解性总磷浓度变化不明显,可溶性活性磷在整个实验期间浓度非常低.这表明颗粒态磷浓度的增加是总磷浓度上升的直接原因.其可能机理是:鱼类去除后,短期内悬浮物含量下降,水体透明度增加,水体光合作用增强,pH值增加,促进底泥营养盐特别是磷的释放,进而促进浮游植物的大量繁殖,造成水体颗粒态磷含量明显增加;同时鱼类去除后对浮游植物牧食压力的减少也是重要原因之一.     

惠州西湖游浮植物群落对生态系统修复的响应

2004年对广东惠州西湖实施了生态系统修复示范工程,示范区目前沉水植物丰富,水体常年清澈见底。通过2008年6月至2009年5月对示范区和未进行生态修复的平湖逐月进行浮游植物调查,研究了浮游植物群落对湖泊生态系统修复的响应。结果表明,与未修复的平湖相比,示范区浮游植物数量及群落结构均发生了很大变化。示范区全年浮游植物平均生物量和细胞丰度分别为0.31 mg/L和2.75×106cells/L,均远低于未修复的平湖的3.27 mg/L和197.46×106cells/L;平湖中蓝藻在全年大部分时间占有绝对优势,一些热带富营养化水体中的代表种类（假鱼腥藻）成为优势种类;而示范区蓝藻不占优势,取而代之的是一些隐藻、硅藻和甲藻门的种类。另外,示范区浮游植物丰富度增加,年平均Margalef物种丰富度指数为3.70,显著高于平湖的2.68。因此,重建以沉水生植物为优势的生态系统是抑制浮游植物发展和改善湖泊水环境的有效途径。     

惠州西湖富营养化现状评价及治理探讨

惠州西湖属于城市型浅水湖泊,本文通过历史和现状数据整理和分析,采用Carlson的营养状况指数(TSI)进行评判,表明惠州西湖处于富营养阶段。通过近几年的疏浚湖底沉积物、截流城市污水和换水等工程措施,惠州西湖水体总氮和总磷有所下降。目前西湖水生生态系统处于逆向演替的藻形湖泊时期,其水生植物受到严重破坏,湖水的透明度等指标没有得到改善。研究结果表明,今后惠州西湖应走生态修复途径,生态系统的恢复与重建和非点源污染控制是关键。     

施氮频率和强度对内蒙古温带草原土壤pH及碳、氮、磷含量的影响

以内蒙古温带典型草原为研究对象,通过 9 个氮沉降梯度以及一年 12 次和一年 2 次的施氮频率比对,经过4年的氮沉降模拟,研究不同氮沉降强度和频率对不同土层土壤 pH 及碳、氮、磷含量的影响.结果表明: 随着施氮强度的增加,土壤 pH 及全磷含量逐渐降低,但土壤有效氮和有效磷的含量呈增加趋势,可溶性有机碳(DOC)含量无明显变化规律,而土壤全碳、全氮含量基本保持不变.与更接近于自然氮沉降状况的一年 12 次施氮相比,一年 2 次施氮明显高估了氮沉降在降低土壤 pH和增加有效磷含量上的作用,低估了氮沉降在增加土壤有效氮含量上的作用,其中0～5 cm土层差异显著.     

氮、磷添加对不同林型土壤磷酸酶活性的影响

研究了鼎湖山3种森林类型(南亚热带季风常绿阔叶林、马尾松人工林和针叶阔叶混交林)的土壤酸性磷酸单酯酶活性(APA)对施肥的响应情况。在3种林型中分别设置对照、加氮(150 kg N hm-2a-1)、加磷(150 kg P hm-2a-1)以及N和P同时添加(150 kg N hm-2a-1+150 kg P hm-2a-1)4种不同处理。结果表明,季风林土壤APA((15.83±2.46)μmol g-1h-1)显著高于混交林((10.71±0.78)μmol g-1h-1)和马尾松林((9.12±0.38)μmol g-1h-1),且3种林型土壤APA与土壤有效磷含量均呈显著负相关。施加N肥显著提高了季风林土壤APA,而对混交林和马尾松林的作用不显著。施加P肥显著降低了混交林和马尾松林土壤APA,但对季风林的影响不明显。N和P同时添加仅显著降低了马尾松林土壤APA,但在季风林中存在交互作用。因此,N沉降会加剧亚热带成熟林土壤P的限制,可以考虑施加P肥作为森林管理的一种方式来缓解这种限制作用。     

惠州西湖生态修复对浮游甲壳动物群落结构的影响

为研究湖泊生态修复对浮游动物群落结构的影响,该文于2010年1-12月份对惠州西湖未修复的子湖-平湖及已实施生态修复后的子湖-元妙观湖、南南湖的浮游甲壳动物群落结构进行了调查。结果表明:龟状笔纹溞、卵型盘肠溞、矩形尖额溞和右突新镖水蚤仅出现在修复后的元妙观湖与南南湖,而颈沟基和溞与平直溞仅在平湖中检出;元妙观湖和南南湖浮游甲壳动物种属数、丰度及多样性指数均高于平湖。冗余分析结果表明:哲水蚤、剑水蚤和枝角类丰度与透明度呈正相关,哲水蚤密度与营养盐呈负相关。研究显示,湖泊生态修复对浮游动物群落结构有重要的影响。     

浅水湖泊浮水植物芡实收割对浮游植物群落的影响

浅水湖泊生态系统正遭受广泛而强烈的人为干扰,但是对收割水生植物干扰的研究甚少。于2019年8月对芡实过度生长的陈瑶湖进行通道式分区收割工程,分析了收割芡实（Euryale ferox）前后不同处理组浮游植物群落的变化。研究期间共鉴定出浮游植物6门47属72种,其中收割前63种,收割后71种。收割后浮游植物的细胞密度和生物量均高于收割前,分别增加了39.78%和5.09%。收割芡实导致陈瑶湖浮游植物群落为由蓝藻-绿藻-硅藻-隐藻群落转变为蓝藻-绿藻-硅藻群落。其中蓝藻细胞密度和生物量显著高于收割前（P<0.05）,归因于有害蓝藻（铜绿微囊藻Microcystis aeruginosa、水华束丝藻Aphanizomenon flos-aquae、小颤藻Oscillatoria tenuis、卷曲鱼腥藻Dolicospermum circinale、小席藻Phormidium tenu）的增加。收割还导致了硅藻群落由附生型向浮游型硅藻的转变,表现为尖针杆藻（Ulnaria acus）减少,而颗粒直链藻极狭变种（Aulacoseira granulata var.angustissima）、梅尼小环藻（Cyclotella meneghiniana）增加。在芡实收割过程中,未收割组和河道的浮游植物群落结构在时空分布上无显著性差异（P>0.05）,但收割组在收割后的不同阶段内差异较为明显,其细胞密度和生物量随着收割实验的结束逐渐降低。浮游植物与环境因子的相关性分析表明,水生植被覆盖度、总磷、总氮、溶解氧和叶绿素a浓度是影响浮游植物细胞密度和生物量变化的主要环境因子。综合陈瑶湖水质状态,本研究认为收割芡实并不能缓解浅水湖泊富营养化状况,研究结果为浅水湖泊水生植被的管理提供理论依据。     

惠州西湖底泥中氮磷特征的初步研究

惠州西湖为典型的亚热带城市浅水湖泊.为了调查该湖泊底泥性质了解底泥对水质的影响.2004年8月在惠州西湖5个子湖(南湖、丰湖、平湖、菱湖和鳄湖)采集了6个底泥柱样,对其含水率、烧失量(LOI)、总氮(TN)、总磷(TP)、藻类可利用性磷(AAP)和粒度的垂向特征进行了初步研究.结果表明,各子湖中南湖内源负荷最大,底泥中的LOI、TN、TP和AAP含量高于其他湖区数倍以上,表层值较高,表明曾遭受过严重的污染,而其它湖区的垂向变化不明显.底泥成分以粘土、粉砂为主,水体混浊度高可能与底泥粒径较小以及鱼类和游船活动的强扰动性有关.     

氮、磷对水华发生的影响

简要介绍了水华的发生与氮、磷元素的关系,包括总氮、总磷的浓度、氮与磷的比值、以及氮、磷在水体中的存在形态等。同时提及水华发生是一个复杂的过程,只有经过多学科配合,进行多因子及其相互作用的综合性研究,才能真正揭示水华发生的杌理。     

The importance of avian-contributed nitrogen (N) and phosphorus (P) to Lake Grand-Lieu,France

The largest natural lake in France, Grand-Lieu, has suffered eutrophication. The objective of the study was to estimate the annual input of nutrients (N, P) resulting from avian excrement, deposited by birds feeding out of the lake and returning to its waters for breeding or roosting, as compared to the input by the rivers that enter in the lake. Two years are compared: 1981–82 and 1990–91. About 1600–2000 breeding herons and cormorants, 20 000–33 000 wintering ducks, gulls and cormorants and 1–2.4 million starlings deposited about 5800 kg total N in 1981–82 and 7640 kg in 1990–91. Respectively, 2000 and 2530 kg total P were deposited over the same time periods. These represent 0.7% and 0.4% of the total N input of the lake and 2.4 and 6.6% of the total P input in 1981–82 and 1990–91. Starlings account for 74% of the N and mallards most of the rest. P input by starlings (36% in 1981–82, 41% in 1990–91), and by mallards and herons (35% and 27% in 1981–82 and 22% and 24% in 1990–91 respectively) plays an appreciable role among birds. During the plant growing period (April–September), the contribution by birds can increase to 37% of total P input of the lake. Piscivorous bird colonies concentrate Phosphorus 42 times more within the colony than outside the colony. Overall, the role birds play in total N and P input is relatively small due to very high inputs from human sewage and agriculture run off. The monthly mean concentration of the water of the two rivers reaches currently 10 mg l^–1 of N (to 23 mg during peak floods) and 394 mg m^–3 of P (to 468 mg during peak floods). Earlier, for example in the 1960's, water in Brittany only contained 0.1 to 1.1 mg 1^–1 of N and 1 to 5 mg m^–3 of P during the maximum flow period. At this time, birds could probably have represented annually up to 37% of the N input and up to 95% of the P input to the lake.     

惠州西湖底泥疏浚对后生浮游动物群落的影响

结合在一个热带浅水湖泊--惠州西湖的一个子湖--湖所实施的底泥疏浚工程,对比分析了底泥疏浚前后部分水质指标和后生浮游动物群落的种类组成、丰度、生物量和物种多样性的变化,研究了底泥疏浚对平湖后生浮游动物群落的影响.结果表明:疏浚后平湖的部分水质指标较疏浚前有所恶化;后生浮游动物的丰度由疏浚前的186.08 ind.·L-1增加到659.22 ind.·L-1,其中轮虫和桡足类的丰度显著增加,枝角类丰度降低;生物最由1.49 mg.·L-1增加到3.72 mg.·L-1,其中轮虫和枝角类的生物量均有所增加,但其在浮游动物总生物量中所占比例却有所下降,桡足类的生物量则由0.08 mg·L-1增加到0.80 mg·L-1,在总生物量所占比例明显上升;Shannon-Weaner指数由2.24下降到1.84.底泥疏浚造成水体营养盐的上升,促进了浮游植物的生长,从而为浮游动物的种群发展提供了充足的食物供给,加之由于干湖底泥疏浚所导致的鱼类捕食压力的减少,多种因素共同导致了疏浚后平湖后生浮游动物种群的生物量、丰度和个体火小的增加.结果看,惠州西湖的清淤不能有效改善水质,也不能恢复生态系统,湖泊恢复必须结合其他措施.     

Abundance of picophytoplankton in the halocline of a meromictic lake, Lake Suigetsu, Japan

Numerous (0.5 to 4.8 × 10⁵ cells/ml), small phytoplankton (smaller than 0.5–1 × 1–2 μm in cell size, picophytoplankton) were distributed in the halocline (depth 2–12 m, 4–14 practical salinity units) of the saline meromictic lake, Lake Suigetsu (35°35′ N, 135°52′ E), located in the central part of the coast of Wakasa Bay along the Japan Sea in Fukui Prefecture, Japan. Vertical distribution of phytoplankton revealed that the maximum number of picophytoplankton was always observed near or a little deeper than the oxic-anoxic boundary layer (depth 5–6 m); they were dominant phytoplankton in the water layer deeper than the oxic-anoxic boundary from July to late September 2005. Spectral analysis of autofluorescence emitted from the particle fractions smaller than 5 μm measured with a spectrofluorometer and from individual cells measured with a microscope photodiode array detector revealed that the major component of picophytoplankton was phycoerythrin-rich, unicellular cyanobacteria (picocyanobacteria). Eukaryotic phytoplankton about 2.5 μm in diameter were also found, but the numbers were low. Fluorescence intensity of chlorophyll a at 685 nm (room temperature) emitted from the particle fractions smaller than 5 μm was increased by the addition of 3-(3,4-dichlorophenyl)-1,1-dimethylurea. These observations indicated that at least some picophytoplankton had a functional photosystem II in the halocline where sulfide, the potential inhibitor of oxygenic photosynthesis, was always present. The large abundance together with their physiological potency suggest that picophytoplankton are one of the important primary producers in the halocline of Lake Suigetsu. Electronic Supplementary Material Supplementary material is available for this article at and is accessible for authorized users.     

Appearance and establishment of diazotrophic cyanobacteria in Lake Kinneret,Israel

1. We propose that the appearance and establishment of Nostocales (cyanobacteria) species of the genera Aphanizomenon and Cylindrospermopsis in the warm subtropical Lake Kinneret (Sea of Galilee, Israel) from 1994 was linked to changes in climate conditions and summer nitrogen (N) availability. 2. From 1994 to 2009, an increase in frequency of events of elevated water temperature (>29 °C) in summer, and to some extent a greater frequency of lower summer wind speed events, affected water turbulence and water column stratification, thus providing better physical conditions for the establishment of these populations. 3. In recent years, N‐depleted conditions in Lake Kinneret in early summer have promoted the development and domination of Nostocales that could gain an ecological advantage owing to their N₂‐fixing capability. 4. Nitrogen fixation rates coincided both with heterocyst abundance and with Nostocales biomass. The N supplied to the lake via nitrogen fixation ranged from negligible quantities when Nostocales represented only a minor component of the phytoplankton community to 123 tonnes when Cylindrospermopsis bloomed in 2005. This high N₂ fixation rate equals the average summer dissolved inorganic nitrogen load to the lake via the Jordan River.     

惠州西湖风景名胜区维管植物资源与多样性研究

为了明确惠州西湖风景名胜区维管植物资源及多样性特征,该研究通过野外实地调查和文献查阅,统计惠州西湖风景名胜区维管植物种类构成及其科、属、种层面的具体组成,并分析其分布区类型、濒危物种、药用植物和水生植物状况。结果表明:(1)惠州西湖风景名胜区共有维管植物169科650属1 061种,其中被子植物种类最丰富,有145科613属1 002种,科、属、种数分别占总数的85.80%、94.30%、94.44%;裸子植物9科20属36种,科、属、种数分别占总数的5.33%、3.10%、3.39%;蕨类植物15科17属23种,科、属和种数分别占总数的8.88%、2.60%、2.17%。(2)惠州西湖风景名胜区植物资源的优势科明显,含10种及以上的科有29科653种,占总种数的61.55%,其中菊科最多(有63种),禾本科次之(有60种);研究区有单属、种的植物442种,表明单种或少数种的科在研究区维管植物中占大多数。(3)惠州西湖风景名胜区有种子植物154科,分属13个分布区类型,其中泛热带分布区类型有60科,所占的比例最高(55.56%),表明该区种子植物具有明显的热带特性,其种子植物区系以热带分布为主。(4)惠州西湖风景名胜区有珍稀濒危植物29种(其中国家保护植物26种),药用植物702种,水生植物150种。研究表明,惠州西湖风景名胜区维管植物资源种类丰富,多样性程度高,应特别加强植物资源的保护和利用以及生态景观的建设。     

Vertical diffusion and nutrient transport in a tropical lake (Lake McIlwaine,Rhodesia)

Measurements of the vertical temperature in tropical Lake McIlwaine were used to calculate the time-averaged ( 6 months) vertical diffusivity coefficient (K_z) in the metalimnion and hypolimnion. The mean value of K_z (0.21 cm² s^–1) was correlated with the lake surface area. The mass transport rates of PO₄-P and NH₄-N, upward from the hypolimnion to the metalimnion, were calculated using K_z and measured values of the nutrient concentration gradients. During a period of 4.5 months when the water was stably stratified, PO₄-P was transported upward at a mean rate of 42 kg day^–1 and NH₄-N at a mean rate of 162 kg day^–1 over the entire lake.     

The recovery of a very shallow eutrophic lake, 20 years after the control of effluent derived phosphorus

1. Monitoring at fortnightly to monthly intervals of a very shallow, lowland lake over 24 years has enabled the time course of recovery from nutrient enrichment to be investigated after high external P loading of the lake (>10 g P m^?2 year^?1) was reduced between 1977 and 1980. 2. The lake showed a relatively rapid response during the spring and early summer, with a reduction in phytoplankton biomass occurring after 5 years when soluble reactive phosphorus concentration was <10 μg L^?1. 3. However, during the later summer the response was delayed for 15 years because of sustained remobilisation of phosphorus from the sediment. The greater water clarity in spring and a gradual shift from planktonic to benthic algal growth may be related to the reduction in internal loading after 15 years. 4. Changes in the phytoplankton community composition were also observed. Centric diatoms became less dominant in the spring, and the summer cyanobacteria populations originally dominated by non‐heterocystous species (Limnothrix/Planktothrix spp.) almost disappeared. Heterocystous species (Anabaena spp. and Aphanizomenon flos‐aquae) were slower to decline, but after 20 years the phytoplankton community was no longer dominated by cyanobacteria. 5. There were no substantial changes in food web structure following re‐oligotrophication. Total zooplankton biomass decreased but body size of Daphnia hyalina, the largest zooplankton species in the lake, remained unchanged, suggesting that the fish population remained dominated by planktivorous species. 6. Macrophyte growth was still largely absent after 20 years, although during the spring water clarity may have become sufficient for macrophytes to re‐establish.