两种沉水植物对间隙水磷浓度的影响

为研究两种根系特征的沉水植物在生长过程中对间隙水中磷浓度的影响,选取根系较多的沉水植物苦草和根系相对较少的沉水植物黑藻作为实验材料,监测底泥中间隙水各形态磷含量及环境因子的变化,探讨不同根系特征沉水植物对间隙水中磷的影响。结果表明:黑藻和苦草实验组沉积物间隙水中各形态磷的浓度均呈不同程度的降低,黑藻和苦草对于稳定水质,减少底泥中磷向水中转移具有明显的效果;沉水植物不同,底泥间隙水中溶解性总磷(DTP)和溶解性活性磷(SRP)存在明显差异。实验结束时黑藻组和苦草组间隙水中DTP的浓度分别为0.24,0.01 mg/L,SRP的浓度分别为0.22 mg/L,0.004 mg/L。间隙水中磷的形态主要以DTP和SRP为主,溶解性有机磷(DOP)的含量相对较低。沉水植物对间隙水中磷的吸收是降低间隙水中磷含量的重要原因,苦草的吸收能力大于黑藻。沉水植物根系通过降低底泥p H值,提高氧化还原电位(Eh)的方式抑制了底泥中磷的释放。     

衰亡期沉水植物对水和沉积物磷迁移的影响

通过室内模拟的方式,分别研究了秋季黑藻、苦草和春季菹草的衰亡过程,分析了沉水植物在衰亡期间水、沉积物中磷与环境因子[pH、氧化还原电位(Eh)和溶解氧(DO)]的相互作用.结果表明:沉水植物黑藻和菹草在衰亡期间能显著提高水中总磷(TP)、溶解性总磷(DTP)、颗粒磷(PP)、溶解性活性磷(SRP)和溶解性有机磷(DOP)的含量;苦草在衰亡期对水体各形态磷含量影响不显著,且各形态磷含量的变化相对较小(TP,0.04-0.06 mg/L);环境因子的变化对水中磷含量影响显著,黑藻和菹草水体中TP的含量和环境因子pH、DO和Eh均呈负相关,而苦草组水中各形态磷的含量受环境因子影响不显著.实验期间不同植物组沉积物中总磷(TP)、NaOH提取磷(NaOH-P)、HCl提取磷(HCl-P)、无机磷(IP)和有机磷(OP)的含量均呈上升趋势.沉积物IP的含量主要受NaOH-P的影响,OP对TP的影响要大于IP,沉积物OP与OM(有机质)的含量存在显著正相关.     

五种沉水植物对富营养化水体的净化效果

为达到净化水质的目的,采用移栽沉水植物控制富营养化水体中营养盐含量和浮游藻类生物量。本研究在夏季藻类密度较高的富营养化水体中移栽5种长江中下游流域常见沉水植物,比较不同沉水植物去除营养盐和控制藻类总量的能力。研究结果:5种沉水植物对水体总氮含量去除率的大小顺序为:竹叶眼子菜>黑藻>苦草>微齿眼子菜>菹草,对总磷去除率大小顺序为:竹叶眼子菜>黑藻>微齿眼子菜>苦草>菹草;竹叶眼子菜控制水体中藻类总量的效果最佳,苦草、微齿眼子菜及菹草次之,黑藻对水体总磷和浮游植物的去除效果均极显著(p≤0.01),而对总氮含量的作用影响不明显(p=0.209)。综合营养盐吸收作用和藻类控制效果来看,竹叶眼子菜在整个实验过程中生长状态良好并达到较为稳定的净化作用,是夏季治理浅型富营养化静水水体的理想物种之一。     

修复白洋淀镉污染水体的沉水植物筛选试验

为了筛选出适宜修复白洋淀镉(Cd)污染水体的沉水植物,该研究通过室内模拟试验,分析了四种沉水植物黑藻、狐尾藻、金鱼藻和菹草对Cd的耐受性及对底泥Cd的富集和迁移能力。结果表明:(1)通过毒性测试研究,Cd对黑藻、狐尾藻、金鱼藻及菹草的4 d-EC₅₀(半数抑制浓度)分别为0.51、0.81、0.03、0.12 mg·L^-1,狐尾藻对Cd的耐性最强,黑藻次之,金鱼藻对Cd的耐性最低; 四种沉水植物对Cd的最大富集量分别为27.89、15.28、22.54、32.74 g·kg^-1,菹草对Cd的富集能力最强,黑藻次之,狐尾藻对Cd的富集能力最低。(2)通过Cd污染底泥修复研究,黑藻、狐尾藻和菹草体内Cd富集量整体表现为根>叶片和茎(P<0.05); 地上部、根对Cd的富集能力分别表现为黑藻>菹草>狐尾藻,菹草>黑藻>狐尾藻; 三种沉水植物对Cd的迁移能力则表现为黑藻>狐尾藻>菹草。总之,黑藻对底泥中Cd富集和迁移能力均较强,且耐性较高,是最适合修复白洋淀Cd污染水体的沉水植物。     

菹草附着物对营养盐浓度的响应及其与菹草衰亡的关系

在菹草衰亡阶段对5个静水水体中菹草叶片表面附着物进行野外调查,并将其与水体营养盐浓度、沉水植物衰亡程度进行相关性分析。附着物共调查Chl.a含量、干重、有机质含量和藻类数量4个指标,沉水植物衰亡程度用单位面积叶片Chl.a含量表示,水体营养盐含量测量了TP、TN和N/P 3个指标。结果显示：附着物生物量与水体营养盐状况存在一定的正相关;各个点的附着物生物量与菹草衰亡状况存在一定相关性但相关性趋势与水体污染程度有关。在污染程度较高的水体中附着物生物量与菹草衰亡程度呈正相关,在污染程度较低的水体中附着物生物量与菹草衰亡程度呈负相关。结论为富营养化湖泊中营养盐含量的增加会导致附着物生物量的增加,但附着物只在污染程度较高的水体中促进植物衰亡。     

光强、温度、总氮浓度对黑藻生长的影响

为寻求沉水植物生长的主效环境因子,探求富营养化水体沉水植物的衰亡机理并选择治理富营养化的先锋植物,实验选择长江中下游常见沉水植物种黑藻(Hydrilla verticillata),利用正交试验设计,通过室内静态模拟实验研究三种主要环境因子光照强度、温度、总氮浓度及其互作对黑藻断枝生长的影响。结果表明:光照强度和温度为影响黑藻生长的主效环境因子,并且光强与温度的交互作用对黑藻生长有较为显著的影响,具体表现为黑藻的生长指标(株高、生物量、分枝数)、光合指标(叶绿素a+b浓度、叶绿素a/b、叶绿体总色素含量)和生理活性指标(根活力、可溶性糖含量、MDA含量)的变化均与这两个环境因子及其互作呈显著相关;总氮浓度的变化对黑藻生长影响不大,在2-8 mg/L的总氮浓度下,黑藻均可以正常生长。根据本实验黑藻生长指标、光合色素含量以及生理活性在不同环境因子组合的变化结果可知,黑藻在5320-12000 lx光照强度、20°C-30°C、4-8 mg/L水体总氮浓度的条件下生长良好,故推测黑藻可作为春夏季富营养化水体中恢复和重建沉水植被的先锋工具种。       

沉水植物生长和腐解对富营养化水体氮磷的影响机制研究进展

沉水植物作为湖泊、河流等生态系统的主要高等植物, 在修复富营养化水体中的作用日益受到重视, 合理利用沉水植物是去除富营养化水体氮磷的有效途径。沉水植物对水体氮磷的迁移转化影响包括生长和腐解两个阶段。文章综述了沉水植物生长对富营养化水体氮、磷的净化效果和净化机制, 分析了沉水植物腐解对氮、磷迁移转化的持续影响, 并提出了今后沉水植物净化氮、磷的研究方向, 为沉水植物推广应用于修复富营养化水体提供理论基础。     

微生物抑制剂对黑藻（Hydrilla verticillata）分解过程及水体碳、氮、磷的影响研究

为了解微生物抑制剂对沉水植物衰亡分解以及水体碳、氮、磷的影响,在实验室模拟条件下研究了有无微生物抑制剂 条件沉水植物黑藻（Hydrilla verticillata）的分解过程,以及对水体与底泥碳、氮、磷的影响,并将有微生物抑制剂作为实验组,无微生物抑制剂作为对照组。结果表明：实验组沉水植物分解损失量是对照组的2.09 倍。实验组释放的碳、氮、磷量分别是对照组的2.81、1.42、1.11 倍。实验组水体碳、氮、磷含量呈现先上升后下降的变化过程,而对照组水体碳、氮、磷达到最大值后,基本保持稳定。水体碳、氮、磷的最大值,实验组条件均大于对照组,微生物抑制剂对沉水植物的分解以及在沉水植物分解过程中,对水体营养物质产生了较大的影响。因此,在进行沉水植物模拟实验时需考虑微生物对沉水植物分解的影响。     

常熟新建水源地湖泊轮叶黑藻和穗状狐尾藻的生长差异及对水环境的影响

为了探明沉水植物群落构建对新建水源地湖泊水环境的作用效果,于2019年5—11月在常熟新建应急水源地湖泊比较研究了轮叶黑藻(Hydrilla verticillata)和穗状狐尾藻(Myriophyllum spicatum)两种沉水植物在人工栽种条件下的生长及对水质和叶绿素a(Chl.a)的影响。结果表明:两种沉水植物在试验湖泊均可正常生长,二者的生物量在5月至9月均呈上升趋势,但轮叶黑藻在5—7月处于快速生长期,而穗状狐尾藻在7—9月处于快速生长期;轮叶黑藻的衰亡期较穗状狐尾藻早,且衰亡过程持续时间短, 11月轮叶黑藻完全衰亡,而穗状狐尾藻仍处于衰亡中期。两种沉水植物在生长期均可有效降低水体Chl.a浓度,对藻类生长起到抑制作用,但是在衰亡期会造成水体营养水平上升, Chl.a浓度升高。由总磷(TP)、总氮(TN)、高锰酸盐指数(COD_Mn)、Chl.a、溶解氧(DO)和透明度(SD)计算综合隶属函数值表明在两种沉水植物生长的高峰期,沉水植物组的水质状况优于对照组,衰亡期水质趋于恶化。Pearson相关分析表明轮叶黑藻生物量与Chl.a存在显著负相关关系,轮叶...     

沉水植物菹草对富营养化水体中TN 生态效应及模型研究

通过室内模拟构建水体营养盐和菹草生物量正交试验, 研究菹草从石芽萌发至菹草植株衰亡腐烂整个生命周期中, 对水体中TN 的生态效应, 并以此为依据建立菹草对富营养化水体生态效应模型。研究表明: 在不同生物量菹草作用下, 富营养化水体中TN 含量是先下降后上升的一个周期式过程; 在相同营养水平条件下, 菹草对TN 的吸收量随菹草生物量的增大而依次递增, 而在相同生物量的前提下, 菹草对TN 的修复力存在一个最佳营养水平范围, 即13.95-20.56 mg·L–1 之间; 菹草对富营养化水体生态效应模型分两部分: 菹草对富营养化水体中TN 与时间关系模型以及菹草生态修复水体TN 限度理论模型, 通过这两个模型的构建可以为生产实践中菹草在生态修复富营养化水体的投放量和菹草的最佳收割时间提供有力依据, 为工程实践提供有效保障。     

Sediment and Water Nutrient Characteristics in Patches of Submerged Macrophytes in Running Waters

(1) The relative importance of sediments and water as nutrient sources for submerged macrophytes in running waters is poorly understood. Here we present water and sediment nutrient characteristics within macrophyte patches in Bavarian rivers. (2) No significant differences between early (June/July) and late summer (August/September) sediment nutrient characteristics could be detected within macrophyte patches. Therefore, a single sediment sample per macrophyte patch was considered to be sufficient for characterising nutrient concentrations during the main growing season in running waters. (3) Sediment TP (total phosphorus) is not a useful parameter for predicting trophic status in running waters. Sediment porewater SRP (soluble reactive phosphorus) concentration is not correlated to water body SRP or TP concentration; nor is it correlated with sediment TP content. Potamogeton coloratus, a oligotrophic species, is associated with low overlying and porewater SRP concentrations but high sediment TP content. Eutrophic species, such as Potamogeton pectinatus, are associated with low sediment TP. (4) It is hypothesized that Chara hispida primarily takes up sediment ammonia for nitrogen nutrition. (5) Nutrient characteristics of the water body and the sediment of eight macrophyte species in Bavarian rivers are described.     

黄河三角洲菹草生长模型及其对水质的影响

通过连续对菹草生长过程的观测 ,用指数方程拟合了菹草从 10月中旬至第 2年 5月底的整个生长过程 (p<0 .0 0 2 ) ,设K=2 .5 kg/ m2时 ,用 L ogistic方程拟合了从 3月到 5月底的生长过程 (p<0 .0 0 0 )。通过 7月底至 8月初、10月、翌年 3月和 5月份对一个菹草型水库和无或有不同规模水草的 5座水库水生生物的周年调查发现 :(1)菹草型水库 TP最高峰的月份比其它水库的推迟 ,其它水库 10月份 TP最高 ,而菹草型水库 3月份最高 ;(2 )菹草型水库浮游植物最高峰的月份比无水草水库的推迟 ,无水草水库出现在夏季 (7～ 8月份 ) ,草型水库的出现在秋季 (10月份 ) ;(3)菹草型水库 3月份浮游植物生物量明显高于其它水库的 ,其硅藻占据更高的优势度 ;(4 )菹草型水库和其它水库之间的总磷和浮游植物数量的年平均值无明显差别 ;(5 )不同水库藻类数量年平均值与 TP年平均值相关极显著 (p<0 .0 0 5 ) ,而 TP又与氯化物 (Cl)相关极显著 (p<0 .0 0 5 ) ;(6 )水草的存在使p H略有提高 ,并使其在不同时间的波动幅度减小     

Mobilization of sediment phosphorus by submersed freshwater macrophytes

SUMMARY. The mobilization of sediment phosphorus (P) by three submersed freshwater macrophyte species was investigated on five different sediments. The study was conducted under controlled environmental conditions in lucite columns that enabled the separation of sediment and plant roots from the overlying P-free 'complete' nutrient solution. The species investigated ( Egeria densa, Hydrilla verticillata , and Myriophyllum spicatum ) had minor root systems (on a biomass basis), but were demonstrated to be fully capable of deriving their P nutrition exclusively from the sediments. Phosphorus absorption and translocation into shoots (i.e., mobilization) was substantial, and in some cases suggested a greater than 1000-fold turnover of interstitial water PO₄-P over a 3-month period. Sediment P mobilization, a function of both plant growth and tissue P concentration, differed considerably among plant species and sediments. Phosphorus release from the species investigated appears to be primarily dependent upon tissue decay rather than excretory processes. The mobilization of sediment P by submersed macrophytes represents an important aspect of the P cycle, and may affect the overall metabolism of lacustrine systems.     

沉水植物菹草的人工种子技术

为满足水生态系统重建及水体景观对沉水植物种苗的需求,本文建立了菹草（Potamogeton crispus L.）人工种子的制作方法,并分析了菹草人工种子的萌发条件。结果表明,以海藻酸钠为包埋剂,在包埋剂中添加IBA 1.0 mg/L + 6-BA 0.5 mg/L,制备的菹草人工种子在灭菌自来水中萌发率可达80％,且转株率达20％。在15－25℃之间,温度对菹草人工种子萌发和转株的影响不显著;氮磷水平对菹草人工种子萌发和转株的影响不显著;光强对菹草人工种子的萌发和转株有显著影响,较高的光强有较高的萌发率和转株率,光强为40μmol/ m2. s时,菹草人工种子萌发率、转株率可达67.8％、35.6％;底质对菹草人工种子的萌发和转株有显著影响,菹草人工种子在黄沙壤上的萌发率、转株率分别为60%和42.2%,黄沙壤比淤泥和砂石更适合菹草人工种子萌发和转株;菹草人工种子在野外湖水的试验中萌发率、转株率分别达到28%、15%。     

西湖引水工程絮凝剂余铝对菹草生长及水质的影响

为分析杭州西湖引水工程絮凝剂残余铝盐对水质和沉水植物的影响,研究采用室外模拟试验,考察了连续投加不同浓度梯度的明矾(KAlSO412H2O)絮凝剂对菹草(Potamogeton crispus)的生理影响和对水质的影响。试验设置了4个处理: 对照组、低剂量组(35050) g/L、中剂量组(65070) g/L、高剂量组(1100150) g/L。结果表明: (1)低、中剂量投加对水中铝盐含量无显著影响,高剂量投加导致水中铝盐含量显著上升; (2)水中铝盐含量呈先升高后降低的趋势,pH随铝盐含量升高而降低,总磷(TP)随之有所下降,各处理组水中总氮(TN)、浮游植物密度、浊度均明显下降; (3)3个剂量组菹草各生化指标较对照组几乎无显著变化,试验浓度的铝盐投加对菹草的生长没有造成明显损害,在菹草耐受范围内,建议在西湖引水工程入水口附近[水中铝盐含量约(25050) g/L]可选用菹草进行植被恢复。     

Measurements of phosphorus uptake by macrophytes and epiphytes from the LaPlatte River (VT) using 32P in stream microcosms

1. Phosphorus (P) uptake by macrophytes and epiphytes from the LaPlatte River (VT) was examined in the laboratory by adding ³²PO₄‐P to recirculating stream microcosms.
2. Water, plugs of sediment and plants were removed from the river and placed into the microcosms. ³²PO₄‐P was then added either to the water or the sediment, and its incorporation into plants and epiphytes was monitored over 3 days. Uptake was examined at both ambient (5 μg L^–1) and increased (50 μg L^–1) soluble reactive phosphorus (SRP) concentrations. A computer program was developed to fit curves to the radiotracer data and calculate rate constants for the simultaneous transfer of ³²P among compartments.
3. Both macrophytes and epiphytes removed P from the water, but epiphyte uptake of P was more rapid. Phosphate enrichment stimulated P uptake by both macrophytes and epiphytes. Macrophytes also obtained P from the sediment. The relative contribution of P to macrophytes from the water vs. that from the sediment appeared to vary with SRP in the overlying water. Accurate estimates of rates of P uptake from sediments by macrophytes were difficult to obtain however, due to very low and highly variable unit rate constants for P uptake and uncertainty about the magnitude of the phosphate pool available for uptake.
4. SRP concentrations were greater in the overlying water than in the sediment pore water of stream microcosms in the present study. Numerous reports in the literature have suggested that this condition favours uptake by macrophyte stems and leaves rather than by roots.
5. Phosphate uptake from the water by macrophytes in shallow streams may be more common than for macrophytes in lakes.     

The contribution of <Emphasis Type="Italic">Potamogeton crispus</Emphasis> to the phosphorus budget of an urban shallow lake: Lake Monger,Western Australia

Lake Monger (Perth, Western Australia) is a highly eutrophic lake, characterised by very low species richness of macrophytes with the dominance of Potamogeton crispus. Mesocosm experiments were performed using water and plants collected from the lake to determine the effects of vegetation decay on the phosphorus (P) concentrations in the overlying waters. After 2 weeks of experimental incubation of mesocosms with and without re-oxygenation, P concentrations in the water column were significantly higher, showing a quite similar effect of P. crispus on the phosphorus release in different mesocosms. The results of our study provide clear evidence that the P concentrations in overlying waters mainly depend upon the plant P content and developmental stage. Although many sources contribute to the nutrient load of Lake Monger, macrophyte harvesting, prior to its senescence, might constitute a significant in-lake measure for reducing the internal P load.     

Distribution and release of sedimentary phosphorus in Lake Ladoga

Sedimentary phosphorus fractions and phosphorus release from the sediments were studied in Lake Ladoga at altogether 46 sampling sites, representing the full range of sediment types encountered in the lake. Determination of P fractions and physico-chemical analyses were made of surface sediment cores (10–20 cm long, each sampled at 3–4 levels) and in the overlying water. The range of total phosphorus per dry weight of sediment was 0.2–3.3 mg g^–1, and that of inorganic P 0.1–2.5 mg g^–1. The levels of interstitial soluble phosphorus, range 2–613 µg 1^–1 for total P and 1–315 µg 1^–1 for inorganic P, were higher than those of dissolved P concentrations in the overlying water. Diffusive fluxes of phosphate from sediment to the overlying water were estimated using three independent methods. The estimated range was 4–914 µg P m^–2 d^–1; the mean value for the whole bottom area, 0.1 mg P m^–2 d^–1, is lower than previously published estimates. The estimated annual contribution of sedimentary inorganic P flux to Lake Ladoga water is equal to 620 tons of P per year, which amounts to more than 10% of the estimated external P load into the lake. 68% of the total diffusive flux emanates from deep water sediments, which are not exposed to seasonal variation of conditions. In deep lakes, such as Lake Ladoga, phosphorus release from the sediments is controlled primarily by diffusive mechanisms. Wave action and currents as well as bioturbation are probably of importance mainly in shallow near-shore areas. Phosphorus release by gas ebullition and macrophytes is considered negligible.     

Modelling phosphorus fluxes in the hypertrophic Loosdrecht Lakes

A dynamic, deterministic model is presented to simulate the phosphorus cycle and plankton growth in the shallow, hypertrophic Loosdrecht Lakes (The Netherlands) before and after restoration measures. Besides inorganic phosphorus (SRP) in both the surface water and the interstitial water, the model comprises three algal groups, zooplankton, fish, detritus, zoobenthos and upper sediment (all modelled both in carbon and in phosphorus). Within the model system, the phosphorus cycle is completely closed. Carbon and phosphorus are described independently, so that the dynamics of the P/C ratios can be modelled. Sediment processes are described in a simplified form.Simulated values are largely within the range of observed ones. The detrital fraction of the seston (=phytoplankton+detritus) varies from 50–60% in summer to about 90% in winter. SRP in the surface water is very low during most of the year. Sensitivity for external phosphorus input is larger for algal and detrital P than for algal and detrital C and chlorophyll-a. So the P/C ratio of the seston decreases following restoration measures, as is observed in the lakes, while the much higher P/C ratios of zooplankton and fish remain constant. Phosphorus mobilisation from the sediment decreases with decreasing external input. Adaptation of the model system to the reduced loading takes place within about two years.Sources of uncertainty in the model include the limited knowledge on selective grazing as well as on mortality and mineralisation processes.