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1.
The lake investigated (Lake Heiliger See near the town of Angermünde, North-East Germany) is small (10.2 ha) but deep (zmax = 12 m, ? = 6.5 m). During summer the thermocline is at a depth of 4-5 m, and the hypolimnion is filled with H2S already by mid-June, making 60-75% of the bottom area inaccessible to fish. The native fish fauna is dominated by planktivorous roach (Rutilus rutilus). A test stocking of silver carp (Hypophthalmichthys molitrix) together with an unplanned and erroneous stocking of common carp (Cyprinus carpio), coupled with an incorrectly calculated strong stocking of eel (Anguilla anguilla), which assumed that the total lake area yielded fish food organisms, brought about a strong depression of the food biomass available to native fish. Both silver carp and common carp showed a pattern of behaviour which only partly agreed with results obtained in experimental ponds prior to lake stocking. At least for 10 years there was a very low zooplankton biomass (mostly below 1 mg/l fresh weight) caused by silver carp and a strongly reduced benthos biomass (frequently below 1 g/m2 fresh weight) caused by common carp and eel on H2S-free bottom areas. Despite this extreme situation, which lasted for 20 years and is rarely found in lakes elsewhere, it was not possible to demonstrate negative effects on the native fish fauna comprising 16 species. Also the dominance pattern seems uninfluenced in the long run. A strong decline of the catchable roach stock was observed for some years, but the stock reappeared soon in comparable quantity. During the time of roach stock depression the individual growth of roach (and common carp) was particularly low. Nevertheless, roach succeeded in reproduction during this time in spite of the reduced zooplankton and detritus concentrations. Fry numbers per year ranged from 500-15 000 individuals/ha. The pike perch (Stizostedion lucioperca) was perhaps the most endangered species of all those living at small population numbers in the lake, since its fry is confined to the limnion where competition from silver carp and adult roach and perhaps predation by roach is highest. However the pike perch stock remained unchanged at the low level of 1950, the time prior of carp and eel stocking. All other rare species of Lake Heiliger See spawn in the littoral zone where fry survival conditions were less impacted. In summary, we present more evidence that the fish fauna of cyprinid lakes is more robust than in salmonid lakes. The regulation capacity of fish communities of eutrophic lakes seems to be able to offset even severe direct and indirect influences of fisheries management.  相似文献   

2.
For the shallow lake there can be expected eutrophic conditions according to its morphometric data (z? 2.8 m, l 1.1… 1.8a), even mesotrophic conditions acc. to the catchment area (2.8 km2/hm3, 8 km2/km2, 20% wood) and eutrophic conditions acc. to load (1,340 Population Equivalents/hm3, 0.027… 0.386 g/m2 a P). The actually measured data of oxygen balance, nutrient contents and bioproduction show a eutrophic situation with a trend towards polytrophy. The difference to the expectation values can be explained by an underestimation of direct loading from a duck farm and the back-wash waters of a waterworks, so that sanitation measures for reducing the direct loading are promising. The relocation of the duck farm and of a large complex of stables as well as the introduction of extensive fishery utilization with a balanced stock of predatory fish resulted in perceptible trends of oligotrophication already after two years, especially by a remarkable promotion of the macrophyte stocks in the shallow water zone.  相似文献   

3.
The lake without any outlet (11 ha, 55000 m3, zmax 2,25 m) has a weak thermal stratification with maximum surface temperatures of 32.5 °C. The annual variation of temperature and depth of visibility is unimodal, with the maxima or minima in August. Phytoplankton consists mainly of Cyanophyceae. The primary production determined by the light-dark bottle technique (oxygen method) varies in the annual variation between 0.3… 0.5 g m?2 d?1 C (winter) and 3.4… 4.6 g m?2 d?1 C (summer); as the annual means of 1975 and 1976 there were found 1.9 and 2.4 g m?2 d?1 C, resp., gross production at a utilization of 0.42… 2.85% of the radiation energy. The chemism is a well-buffered hydrogen-carbonate water (pH 8.1… 9.0) with 74… 90 mg/1 Na and 20.5… 31.5 mg/1 K and with a good nutrient supply (20… 40 μg/1 PO4—P and 100… 240 μg/1 NO3—N) at the same time.  相似文献   

4.
放养鲢(Hypophthalmichthys molitrix)、鳙(Aristichthys mobilis)控制富营养化湖泊蓝藻水华暴发是当前最有效的手段之一.为评估富营养化初期湖泊鲢、鳙控藻的生态效果,2016年在洱海红山湾开展原位围栏鲢、鳙控藻实验,对围栏内外的浮游生物群落结构及水环境因子的变化进行对比分析,同时测定了围栏内鲢、鳙的生长及摄食节律.结果表明:围栏内鲢、鳙呈现匀速生长,围栏生存环境适宜.根据Egger''s模型估算鲢、鳙的日摄食量分别为24.96%和18.18%,鲢的日粮高于鳙;滤食率结果表明,鲢对浮游植物的摄食率高于鳙(分别为3.01和2.19 L/(g·h),而鳙对浮游动物的滤食率高于鲢(分别为18.61和13.54 L/(g·h)).研究期间,围栏内外水体理化因子无显著差异;但围栏内外微囊藻生物量差异明显,并且在7月达到生物量峰值(围栏内为1.7 mg/L,围栏外为2.4 mg/L).鲢、鳙对浮游植物的优势种类——微囊藻和隐藻有明显的削减效果,6-8月逐渐上升并在8月达到最高(64%);当浮游植物优势种由微囊藻替换为硅藻门和绿藻门的种类时,鲢、鳙的削减效率不明显(10-11月为负值).此外,鲢、鳙放养显著降低了浮游甲壳动物的总生物量和枝角类生物量.因此,结合实验结果得出,鲢具有更高的控藻能力,尤其对微囊藻水华,但同时具备了较高对浮游甲壳动物的削减能力,需要进一步分析富营养化初期湖泊——洱海中实施非经典生物操纵的适宜性.  相似文献   

5.
张风菊  薛滨  姚书春 《湖泊科学》2019,31(6):1770-1782
湖泊沉积物碳埋藏及其驱动机制是陆地生态系统碳循环及全球变化研究的热点问题之一,但以往湖泊碳循环的研究大多局限于有机碳,较少考虑无机碳的地位和作用.我国干旱-半干旱地区湖泊众多、无机碳储量丰富,在区域碳循环过程中的作用日益突出,因此探讨这些地区湖泊沉积物无机碳埋藏变化对深入理解区域碳循环具有重要意义.本研究通过对内蒙古高原呼伦湖15个沉积岩芯样品无机碳含量(TIC)的测定,结合沉积岩芯210Pb、137Cs年代标尺,分析了1850年以来呼伦湖无机碳埋藏速率时空变化,并揭示了影响呼伦湖无机碳埋藏的主要因素.结果表明,1980s之前,呼伦湖无机碳含量总体维持在相对稳定的低值,1980s之后开始快速增加,且近百年来呼伦湖平均无机碳含量在不同湖区差异不显著.1850年以来呼伦湖无机碳埋藏速率变化范围约为7.10~74.29 g/(m2·a),平均值约为36.15 g/(m2·a),且大体上可分为3个阶段,即1900s以前相对稳定的低值阶段、1900s-1950s期间的快速增加阶段以及1950s以来的波动增加阶段,各阶段无机碳埋藏速率平均值分别约为10.40、26.29和41.00 g/(m2·a).空间上,呼伦湖无机碳埋藏速率整体表现为中部高、南北两端低的分布格局,这可能与湖心水动力条件相对稳定,有利于碳酸盐沉积有关.此外,呼伦湖无机碳埋藏速率与湖区温度变化呈显著正相关,而与周边人类活动影响关系不明显,表明在未来全球变暖背景下,呼伦湖无机碳埋藏速率将进一步增加,湖泊在区域碳循环中的作用将更加显著.  相似文献   

6.
乌伦古湖是我国十大内陆淡水湖之一,同时也是新疆维吾尔自治区的第二大湖泊和主要渔业基地.近年来,随着气候变化和人为因素的影响,湖区水体营养状况、生物群落组成等均发生了较大变化.为揭示该湖大型底栖无脊椎动物的群落结构特征及其对生态系统变化的响应,2006年11月至2008年7月设28个采样点对大型无脊椎底栖动物的群落结构特...  相似文献   

7.
Lake sediment can sequestrate large amounts of carbon and this issue has become a research hotspot. However, most of research on carbon burial in lakes is based on a single (or a few) sediment core records and so may underestimate the variability of carbon burial features within a single lake. In this study, therefore, Chaohu Lake, a typical large shallow lake in the middle and lower reaches of the Yangtze River, was selected to conduct multiple, high resolution sediment core studies to elucidate that variability. Overall 18 sediment cores are analyzed according to paleolimnological proxies (including 210Pb/137Cs for 3 master cores); sediment accumulation rate, total organic carbon, grain size and loss of ignition is measured or estimated for most cores. The spatiotemporal variations of organic carbon burial rate (OCBR), carbon storage and their driving factors were examined. Results show: 1) There was a clear temporal difference in carbon burial during the past 150 years, with OCBR varying from 1.1 g C/m2/y to 25.6 g C/m2/y (mean 9.8 g C/m2/y). OCBR began to increase after around 1900, a rapid increase followed after 1950s and a downward trend after 1970s. Total carbon burial amount (OCBA) in the lake since the 1850s is 1.11 x 1010 g. 2) The average OCBR of six sediment cores in the northwest lake area is 13.4 g C/m2/y, significantly higher than that for sediment cores in other areas (9.6 g C/m2/y). 3) TOC, OCBR, OCBA in all 18 cores exhibited similar temporal patterns (i.e. marked increase since 1950s in most of the cores) but with significant differences in several lake locations. 4) During the last 150 years, carbon burial in Chaohu Lake appears to be greatly affected by changes in regional temperature and population size, according to their significant correlations. OCBR also has a significant correlation with the average lake level in the past 50 years, indicating human activity (notably dam building). This has imposed an important impact on OCBR in Chaohu Lake. This multi-sediment core study reveals the spatiotemporal characteristics of carbon burial in the lake and provides an important basis for increasing the accuracy of calculating carbon storage in large shallow lakes.  相似文献   

8.
从细菌、浮游植物、浮游动物、底栖动物和有机碎屑等几个方面分析了养鱼对伊乐藻种植区(以下简称为有草区)和无草区水域环境的影响。结果表明:两个区域存在着显著的差异性。有草区由于生长着茂密的水生植被,对环境压迫的缓冲能力增强,水生生物的群落结构较为稳定,物种多样性指数高于无草区,有机物的沉降速率也大大低于无草区。与此相比,无草区对环境压迫的缓冲能力较差,水体浮游植物数量增加,富营养化加剧。通过本项实验可以看出,人工种植伊乐藻对养鱼区水质有着明显地控制作用,是发展生态渔业的一条有效途径。  相似文献   

9.
湖北浮桥河水库浮游植物初级生产力及其管理   总被引:3,自引:2,他引:1  
浮桥河水库浮游植物水柱日生产量变幅为0.34-4.99 g/(m2·d),最低值出现在下游冬季,最高值出现在中游秋季,年平均值2.75 g/(m2·d)季节变化:秋季>夏季>春季>冬季,与浮游植物叶绿素a含量和生物量的季节变化一致;水平分布:中游略高于上游,下游最低,与浮游植物叶绿素a含量的水平分布完全一致表层日生产量占水柱日生产量53.81%.与1980年同期相比,浮游植物初级生产力增加了1.2倍.分析表明,磷含量增加是浮游植物初级生产力提高的关键因子.应用能量收支法估算浮桥河水库鲢鳙渔产潜力为772t,516.0 kh/hm2.从渔业管理和水质管理角度讨论了合理利用浮游植物初级生产力的措施.  相似文献   

10.
滇池东北岸生态修复区的环境效应——Ⅱ.污染净化效应   总被引:2,自引:0,他引:2  
研究了滇池东北沿岸带生态修复区去除水体中污染物和营养盐的能力.对修复区在重富营养水体迎风岸、无陆源污染情况下通过收获水生植物和促进悬浮物沉降方式去除的湖泊内源污染物质进行了定量的监测分析.结果显示,修复区对外来的悬浮物质具有强大的凝集、固定作用,植被区内每平方米湖面平均年沉积量达118.9 kg(干重),其中的氮、磷、有机碳含量分别达120 g/(m2·a)、70 g/(m2·a)、1080 g/(m2·a):修复区内的底质环境得到明显改善,表层沉积物中氮和有机碳含量比原初提高了4倍以上;修复区内水生植被具有极高的生产能力,仅2002年修复区就收割打捞水生植物113t(干重),由此去除氮、磷分别为30.0 g/(m2·a)和4.8 g/(m2·a).因此,沿岸带生态修复完全可以作为湖泊内源污染净化的一项工程措施在滇池东北沿岸或类似重污染水体推广应用.  相似文献   

11.
Changes in the soluble sugar, starch, total non-structural carbohydrate (TNC) and nutrient (N, P, K) concentration in the reed rhizome were investigated in different reed habitat types in Lake Fertõ/Neusiedlersee during the vegetation period in 1993 to 94. Three die-back and four vigorous reed stands were monitored.For biomass estimations rhizomes were collected twice, in early summer and in autumn. They were calculated to be 1.9 to 2.7 kg/m2 at die-back and 3.1 to 6.1 kg/m2 at vigorous sites.The carbohydrate and nutrient concentrations of the reed rhizomes were high at the beginning of the vegetation period; they reached their minima in May–June, which was followed by a gradual increase until the end of the vegetation period. From autumn to spring the concentrations decreased, e.g. TNC concentration by 15 to 40% at vigorous, 50 to 70% at die-back sites.In both years the lowest carbohydrate concentrations were recorded at the end of May, a month before the inflorescence developed (vigorous sites: 50–70 mg TNC/g, die-back sites: 70–120 mg TNC/g). In that period the standing stock of the TNC in the rhizome did not separate the sites clearly, and the smallest carbohydrate standing stock was measured at a vigorous site with a high water cover.At the beginning of summer and in autumn the soluble sugar, TNC and N concentration values were higher at the die-back than at the vigorous sites but the standing stock was higher at the vigorous sites. In autumn the TNC standing stock of the rhizomes was between 780 and 1200 g/m2 at vigorous, between 380 and 690 g/m2 at die-back sites. This is especially important for the reactions and resistance of die-back reed stands to unfavourable conditions.  相似文献   

12.
湖泊沉积物有机碳埋藏是陆地碳循环中重要的环节,对全球碳平衡起着重要的作用.洱海是云贵高原第二大淡水湖,目前对洱海生态环境变化、重金属与营养盐污染等已展开了较为深入的研究,但对近百年来沉积物有机碳埋藏时空变化与驱动因素缺乏系统的分析.本文通过对洱海北部湖区典型岩芯(编号EH2012)以及其他湖区13个沉积岩芯中有机碳(OC)含量的分析,结合湖泊生态环境与气候因子变化,研究了近百年来沉积物有机碳埋藏时空变化特征与影响因素.C/N摩尔比值表明洱海沉积物中OC以湖泊内源为主,不同湖区岩芯中OC含量变化趋势基本相似.以EH2012岩芯为例,OC含量历史变化可分为3个阶段:1970年以前,表现出较稳定的低值;1970-2000年,OC含量逐渐增加;2000年以来,OC含量增加更加明显并达到近百年来的最大值.近百年来,EH2012岩芯有机碳累积速率(OCAR)呈逐渐增加趋势,变化范围为7.9~87.2 g/(m2·a),平均OCAR(OCAR)为24.1 g/(m2·a);OCAR变化与OC含量和区域气温呈显著正相关,全球变暖与营养驱动下的湖泊生产力提高可能是近年来OCAR增加的主要原因之一.基于重金属Cd污染初始时间建立的时标,1982年以来不同湖区OCAR为17.1~44.7 g/(m2·a),采用克里金插值得到的全湖OCAR均值为31.4 g/(m2·a);不同湖区OCAR与磷累积速率呈显著正相关,指示了湖泊营养水平对有机碳埋藏空间变化的重要影响.  相似文献   

13.
The wetland of 56 ha is situated at a height of 1565 m in the valley of the Jehlum river. Among macrophytes prevail Typha, Phragmites, Scirpus and Sparganium, and they are investigated at eight stations in the annual cycle. The mineral composition of the aboveground and belowground biomass and of the sediment was determined. The mean total biomass shows considerable variations, but also a pronounced annual variation with the summer maximum of 1445 g/m2 above-ground and 1550 g/m2 below-ground. The mineral constituents show clearly decreasing concentrations during the season of vegetation as far as potassium, calcium, magnesium and nitrogen are concerned, the nutrient contents lying between 0.041 and 1.9% P or 0.57 and 1.65 % N. In a regression analysis the biomasses show significant multiple regressions to concentrations of chloride-ions, nitrogen and partly TPP and oxygen in the water and sediment.  相似文献   

14.
The wastewater treatment is carried out in two parallel pond groups: South–9200 m3/d, 1748 kg/d BOD5, preliminary clarifier (1.1 ha, 22000 m3), three ponds (9.8 ha, 88000 m3), naturel aeration; North ?5700 m3/d, 2394 kg/d BOD5, Imhoff tank, three ponds (7.9 ha, 71000 m3), the pond 1 artificially aerated by gyroscopic units. The different loads of 15.9 and 33.7 g/m3 d BOD5 results in rates of removal of 11.2 and 22.5 g/m3d BOD5, resp. Therefore, the efficiency of the naturally aerated system is higher than that of the artificially aerated system. In the aerated system mainly the bacterial growth is promoted, a typical algal state being achieved only slowly, whereas the naturally aerated system gains a summer-time algal maximum in the ponds 2 and 3, which is accompanied already by zooplankton populations. In the dynamics of the biomass development, the higher efficiency of the four-stage, naturally aerated system is especially obvious.  相似文献   

15.
向启华 《湖泊科学》1991,3(1):35-45
水文报道1987年河南封丘曹岗湖底栖动物的调查结果。该湖底栖动物主要由寡毛类8种, 水生昆虫47种和腹足类2种组成, 其中克拉泊水丝蚓和刺铗粗腹摇蚊群为优势种类, 平均密度为2087个/m2, 生物量为4.8690g/m2, 并与长江中游浅水湖泊中的底栖动物作了比较, 对某些环境因素与底栖动物种类组成、数量分布的关系也作了扼要的分析。  相似文献   

16.
Chlorophyll a-concentrations, AFWD (ash-free-dry-weight) and photosynthesis rates were estimated for periphyton assemblages in Amazonian black-and white-water habitats over 14 months. Cellulose-acetate strips were incubated in situ and showed few major differences in periphyton quality as compared to natural substrata. The only exceptions were submersed Igapó forest leaves, which exhibited higher proportions of green algae and cyanobacteria though not producing differences in total periphyton biomass. Enclosure experiments showed a considerable nutrient release by inundated non-senescent Igapó forest leaves. Periphyton biomass and productivity were found to be highest in black-and white water mixing zones, where biomass peaked at 41.6 mg Chla/m2 and 19.8 g/m2 AFDW. Production was estimated to be 380 gC/m2·a. Maximum biomass of periphyton in floating meadows was 46 mg Chla/m2 and 10.6 g/m2 AFDW, with an annual production of 170 gC/m2·a. Solimões main channel periphyton values were low: maximum Chla was 7.1 mg/m2, AFDW 0.8 g/m2 and annual production was estimated to be 30 gC/m2. Blackwater periphyton values were lower compared to whitewater and mixed water values but an enlarged trophogenic zone has to be taken into account. Highest Chla content reached 30.9 mg/m2, AFDW 1.43 g/m2. Estimated annual production was 110 gC/m2. Observed mean periphyton productivity of Amazonian blackwater habitats approximately corresponded to mesotrophic attached algae productivity in temperate zones, whereas productivity of whitewater periphyton approached those of temperate eutrophic lakes. The role of periphyton in the Amazon food web is discussed.  相似文献   

17.
Otoliths are biogenic carbonate minerals in the inner ear of teleost fish, whose compositions can record the physical and chemical conditions of the ambient water environment inhabited by individual fish. In this research, the fishbones and otoliths of naked carp sampled near the Bird Island, offshore Lake Qinghai, were dated and analyzed for mineralogy and microchemical compositions. Comparing the microchemical compositions of ancient otoliths with those of modern otoliths, we conclude that the ancient naked carps inhabited a relict lake formed when the lake shrank from a high lake level, by combining with the AMS-14 C ages of fishbones and otoliths, the stratigraphy and surrounding topography of the sample site. AMS-14 C dating results of ancient fishbones and otoliths show that these naked carps lived from 680 to 300 years ago, i.e. during the Ming Dynasty of China. The X-ray diffraction(XRD) patterns demonstrate that the ancient lapillus is composed of pure aragonite, identical to modern one, indicating that the mineral of lapillus didn't change after a long time burial and that the ancient lapillus is suitable for comparative analysis thereafter. Microchemical results show that both ratios of Mg/Ca((70.12±18.50)×10?5) and ? 18O((1.76±1.03)‰) of ancient lapilli are significantly higher than those of modern lapilli(average Mg/Ca=(3.11±0.41)× 10?5 and ? 18O=(?4.82±0.96)‰). This reflects that the relict water body in which the ancient naked carp lived during the Ming Dynasty was characterized by higher Mg/Ca and ? 18 O ratios than modern Lake Qinghai, resulting from strong evaporation after being isolated from the main lake, similar to today's Lake Gahai. Based upon the stratigraphy and altitude of naked carp remains, it can be inferred that the altitude of lake level of Lake Qinghai reached at least 3202 m with a lake area of 4480 km2 during the Ming Dynasty, approximately ~5% larger than it is today.  相似文献   

18.
The two eutrophicated reservoirs Husinec (2.6 km3, 35 ha, zmax 18 m, MQ 1.87 m3/s) and ?ímov (34.5 hm3, 216 ha, zmax 44 m, MQ 4.14 m3/s) show concentrations of total phosphorus of 10… 50 mg/m3 and chlorophyll contents of 7… 36 mg/m3 in the summer season. For both reservoirs a good correlation exists between the chlorophyll concentration and the density of the phytoplankton (20 · 103… 13 · 106 ind./l). With average concentrations of 10… 20 mg/m3 chlorophyll a in summer, the water can be treated for producing drinking water only at a higher expenditure. The water quality will be improved by a reduction of the phosphorus load.  相似文献   

19.
宜兴太湖防护林对农业面源污染的减源增汇作用浅析   总被引:1,自引:1,他引:0  
为探讨太湖沿岸防护林宜兴段对农业面源污染物的控制效果,通过在宜兴市太湖防护林采集土壤样品,测定其中营养元素含量,结合周边农业生产施肥概况,初步分析了该区域防护林对农业面源污染的减源—增汇效应.结果表明,2009年10月份防护林地上部分固定的C、N、P和K分别为2439.48、18.34、2.48和13.42 g/m2;2011年5月份固定量分别为3114.12、23.42、3.16和17.13 g/m2;而2013年8月份固定量分别为4722.46、35.53、4.81和25.99 g/m2.可见C、N、P和K的固定量是逐年增加的,相比2009年,分别增加了93.6%、93.7%、94.0%和93.7%.结果说明宜兴段太湖沿岸防护林对农业面源污染的控制效果较显著,有助于太湖水污染的治理.  相似文献   

20.
An enzyme assay was developed for studies on peroxidase activities in humic lake water. 3,4-Dimethoxybenzyl alcohol (veratryl alcohol, VeraOH) was used as tracer substrate, and peroxidase (EC 1.11.1.7) activity was measured by high-performance liquid chromatography. The chemical stability of VeraOH and its application as peroxidase substrate was tested under light and dark conditions, different hydrogen peroxide (H2O2) concentrations and humic matter contents. VeraOH was stable under low UV radiation at in situ conditions in lake water (<0.010...0.25 kJ m–2 d–1), laboratory conditions (<0.05...0.30 kJ m–2 d–1), and low (1...100 μM) H2O2 concentrations. However, peroxides oxidized VeraOH above 1...10 mM H2O2 concentration in sterile Millipore-Q and humic lake water. Dark incubations showed little VeraOH oxidation products. The developed peroxidase assay was tested in the growth medium of Phanerochaete chrysosporium and a bacteria isolate (P.M.D. 20.4.3.1) from mesohumic lake Pääjärvi. Peroxidase activities were also measured in natural microbial communities under standard laboratory and under in situ conditions in humic lake water. Incubation times of about 5 to 12 days were usually needed to record significant (P < 0.05) peroxidase activities, in lake waters. In situ peroxidase activities varied in pelagial surface water (0...0.5 m) on a seasonal scale between 74 nmol L–1 h–1 and 273 nmol L–1 (mean: 176 nmol L–1 h–1) and within the water column between 110 nmol L–1 h–1 and 800 nmol L–1 h–1 (mean: 500 nmol L–1 h–1) in polyhumic lake Mekkojärvi.  相似文献   

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