硅酸盐矿物麦饭石对沉水植物生理生态的影响

沉水植物的稳定生长是重建健康湖泊生态系统重要环节, 底质条件是沉水植物生长的关键因素。研究通过观测沉水植物生理生态的变化来探讨麦饭石对其影响及作用机理。研究结果表明, 与湖泥组相比, 麦饭石可明显促进沉水植物苦草生长, 覆盖1 cm厚度麦饭石的苦草植株高度、单株生物量优于湖泥组(P<0.05); 改性麦饭石组的苦草株高、单株生物量高于麦饭石原石组(P<0.05)。麦饭石组中两种植物苦草和轮叶黑藻的光合色素、根系活力、丙二醛、过氧化物酶活等指标在一定程度上均优于湖泥组。检测发现麦饭石中含有丰富的植物生长所需的常量和微量元素, 可以明显促进沉水植物生长。可见麦饭石有益于沉水植物生长, 可进一步作为底质改良材料应用于湖泊生态修复工程。     

蓝藻胁迫条件下不同基质类型对苦草和伊乐藻生长的影响

为探讨蓝藻胁迫条件下沉水植物生长与基质营养含量的关系,研究了添加相同含量蓝藻后2 种不同基质(较贫瘠的黄色粘土和较肥沃的黑色淤泥)对苦草和伊乐藻2 种沉水植物生长的影响。结果表明:与伊乐藻相比,苦草的生物量在粘土条件下高于淤泥条件,而基质类型对伊乐藻生物量没有显著影响;苦草的最大叶片长度(用于表征株高)、无性系新株数目及其干物质重和伊乐藻的株高、分株数目和分枝干物质重也是在粘土条件下高于淤泥条件;苦草的最大根长在粘土条件下显著高于淤泥条件(p<0.05)。研究结果表明在蓝藻胁迫的条件下,高营养含量的基质不利于沉水植物的生长,并且对根生型沉水植物苦草的影响要大于假根沉水植物伊乐藻。     

叶片损害强度与基质营养水平对苦草补偿性生长的影响

通过室外双因子控制试验,研究了叶片损害强度与基质营养水平对沉水植物苦草补偿性生长的影响.结果表明：叶片损害与基质类型对苦草的累积生物量、生物量的分配（根叶比）及分株数均有显著影响.与未受损植物相比,强受损使苦草的累积生物量及无性分株数显著降低,根叶比明显升高,而弱受损与未受损处理之间没有明显差别.与营养贫瘠的岸泥相比,生长在肥力较高湖泥中的苦草的累积生物量较高,而根叶比与分株数较低;叶片损害与基质类型对苦草的相对生长率也有显著影响,受损使苦草的生长率明显提高,而两受损处理之间无显著差别.未受损与强受损时,湖泥中苦草的生长速率明显高于岸泥,弱受损时则相近.并初步探讨了水生植物受损后的补偿生长机理.     

不同基质对四种沉水植物生长的影响

通过模拟试验,研究了太湖五里湖主要3种基质类型(沙石、生土、湖泥)对4种沉水植物(苦草、马来眼子菜、金鱼藻、轮叶黑藻)生长的影响. 结果表明,生长于沙石、生土、湖泥上的苦草和马来眼子菜平均生物量分别为72.37、126.25、134.10 g和40.0、72.10、90.70 g,而金鱼藻和轮叶黑藻平均生物量分别为0.27、6.58、73.64 g和0.17、3.26、84.42 g,说明湖泥较适合这四种沉水植物生长. 苦草和马来眼子菜对相对贫瘠的生土有较强的适应性,而金鱼藻和轮叶黑藻不适宜在生土中生长. 生长在沙石上的4种沉水植物的生物量和株高最低,其中金鱼藻和轮叶黑藻于试验期间死亡.苦草的根系活力(TTC)低于马来眼子菜,生长在沙石、生土、湖泥中苦草的根系活力分别为0、(0.16±0.05) mg·g^-1·h^-1和(0.36±0.33) mg·g^-1·h^-1,而马来眼子菜则分别为(2.68±0.34) mg·g^-1·h^-1、(2.30±0.77) mg·g^-1·h^-1、(5.24±0.67) mg·g^-1·h^-1. 叶绿素、质膜透性和丙二醛(MDA)的测定结果进一步证明了以上结论.此外,苦草、马来眼子菜和轮叶黑藻对基质有较强的沁氧能力,其大小顺序为苦草＞马来眼子菜＞轮叶黑藻.     

螺类牧食与沉积物类型对苦草生长的影响

在室外实验条件下,研究了螺类牧食与沉积物类型对苦草生长的影响。结果表明:椭圆萝卜螺的牧食对苦草生长有显著影响,牧食损害使苦草的相对生长率明显降低、块茎数量及重量下降。沉积物类型对苦草生长也有明显影响,苦草的相对生长率在营养盐相对丰富的湖泥处理组中要远高于岸泥处理组,而根须数与块茎重量在湖泥处理组中显著低于岸泥处理组。螺类牧食与沉积物类型对苦草的各项生长指标无明显交互作用。     

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。     

不同功能型沉水植物对溶解氧影响及环境效应

研究选用刺苦草(Vallisneria spinulosa)、黑藻(Hydrilla verticillata)和穗花狐尾藻(Myriophyllum spicatum)分别代表底层型、冠层少根型和冠层多根型沉水植物,通过中宇宙实验,探索不同功能型沉水植物在生长过程中水柱和沉积物中溶解氧(DO)浓度及其相关指标的差异。实验结果表明:不同处理组水柱DO浓度存在显著差异,空白组水柱DO浓度显著低于植物处理组,且空白组水柱总氮(TN)和总磷(TP)浓度降低程度最少;黑藻组比叶面积、叶面积指数、净增长生物量、相对生长速率和水柱DO浓度最大,能够有效降低水柱TP和TN浓度;穗花狐尾藻组株高最高,提升水柱DO浓度显著高于刺苦草,水柱TP降低程度最大;刺苦草组比根长、单株总根长和根冠比最大,提升沉积物深度6 cm以内的DO效果最好,沉积物铁含量最高,沉积物总氮(TN)、总碳(TC)含量和间隙水总溶解性磷(TDP)浓度最低。在修复富营养湖泊过程中,可根据水和沉积物缺氧状况,合理配置底层型和冠层型沉水植物,构建释氧能力较强的群落,从沉积物表层到水柱上层均为湖泊提供充足的氧气,从而更加有利于清水态的形成。     

根际促生菌对沉水植物的促生效应及其与沉积物氮磷赋存形态的关系

研究在沉积物高有机质条件下, 通过接种根际促生菌(Plant growth-promoting rhizobacteria, PGPR) PC2(Bacillus stratosphericus)、H19(Bacillus subtilis)和L3(Bacillus cereus)的方式探讨其对苦草(Vallisneria natans)植株的促生效应及其与沉积物氮磷赋存形态的关系。结果表明, 接种组对苦草生长具有显著促进作用, 空白处理种植的苦草生长受到抑制, PGPR对苦草生长促进的综合影响为PC2>H19>L3, PC2处理组株高、根长、地上鲜重和根鲜重比空白分别增加了165.0%、17.4%、378.8%和165.1%。进一步分析不同时期苦草的各种生长指标增量与氮磷赋存形态增量的关系, 通过RDA分析及皮尔森相关分析, 苦草生长指标增量与沉积物中无机氮(Inorg-N)、亚硝态氮(NO₂-N)、硝态氮(NO₃-N)、无机磷(Inorg-P)和铁/铝磷(Fe/Al-P)等增量显著负相关, 表明PGPR对沉积物中无机态N、P具有一定的控制作用。因此, 接种PGPR对解决受污染湖泊沉水植物恢复及内源污染等问题具有一定潜力。     

不同光照强度下物种组合对沉水植物苦草种间关系的影响

为了解种间关系对沉水植物群落结构的影响，在不同光照(20%自然光和50%自然光)和不同物种组合下，研究了长江中下游常见优势沉水植物苦草(Vallisneria natans)与黑藻(Hydrilla verticillata)和穗状狐尾藻(Myriophyllum spicatum)的相互作用。结果表明，在低光下，苦草与穗状狐尾藻混种时，苦草生物量、株高和叶数均没有明显变化，当穗状狐尾藻的比例较高时，苦草根长生长受到抑制，根叶比呈下降趋势；在高光下，穗状狐尾藻比例的增加会促进苦草单株生物量和叶生物量的增加，而对苦草株高、根长和叶数无显著影响；与黑藻混种相比，苦草与穗状狐尾藻混种时，苦草的株高、根长和叶数均无显著差异，而苦草的单株生物量和叶生物量均呈降低趋势。因此，物种组合和混种比例均会影响苦草与其他物种的相互作用关系，进而影响沉水植被的群落动态。     

不同光照强度和底质营养对三种沉水植物的影响

沉水植物的生长不但与光照强度的关系密切, 也受底质营养的影响, 因此研究光照强度和底质营养两种环境因子的共同作用对沉水植物的影响尤为重要。本文选择轮叶黑藻(Hydrilla verticillata)、苦草(Vallisneria natans L.)和大茨藻(Najasmarina L.)3 种沉水植物为研究对象, 设置3 种光照强度(高、中、低)和2 种底质营养(高、低)处理, 通过测定植物生长指标(生物量和叶绿素)及水质指标(水体溶氧量和pH)的变化反映光照强度与底质营养对三类沉水植物生长的影响。结果表明: (1)高底质营养处理促进了三种沉水植物的生长, 生物量、叶绿素含量、水体溶氧量和pH 均高于低底质营养处理组。(2)高底质营养处理组中, 轮叶黑藻在中光照强度处理下其生物量最高为4.87 g, 苦草在低光照强度处理下生物量最高为3.13 g, 大茨藻在高光照强度处理下生物量最高为4.71 g, 相应的叶绿素含量和水体溶氧量也都达到了最大值。因此根据修复湿地环境中的光照和底质条件, 因地适宜的选择沉水植物必须研究各种沉水植物不同的生态影响因子。     

Impacts of sediment type on the performance and composition of submerged macrophyte communities

To restore deteriorated lake ecosystems, it is important to identify environmental factors that influence submerged macrophyte communities. While sediment is a critical environmental factor for submerged macrophytes and many studies have examined effects of sediment type on the growth of individual submerged macrophytes, very few have tested how sediment type affects the growth and species composition of submerged macrophyte communities. We constructed submerged macrophyte communities containing four co-occurring submerged macrophytes (Hydrilla verticillata, Myriophyllum spicatum, Ceratophyllum demersum and Chara fragilis) and subjected them to three sediment treatments, i.e., clay, a mixture of clay and quartz sand at a volume ratio of 1:1 and a mixture at a volume ratio of 1:4. Compared to the clay, the 1:1 mixture treatment greatly increased overall biomass, number of shoot nodes and shoot length of the community, but decreased its diversity. This was because it substantially promoted the growth of H. verticillata within the community, making it the most abundant species in the mixture sediment, but decreased that of M. spicatum and C. demersum. The sediment type had no significant effects on the growth of C. fragilis. As a primary nutrient source for plant growth, sediment type can have differential effects on various submerged macrophyte species and 1:1 mixture treatment could enhance the performance of the communities, increasing the overall biomass, number of shoot nodes and shoot length by 39.03%, 150.13% and 9.94%, respectively, compared to the clay treatment. Thus, measures should be taken to mediate the sediment condition to restore submerged macrophyte communities with different dominant species.     

Development of submerged macrophyte and epiphyton in a flow-through system: Assessment and modelling predictions in interconnected reservoirs

Every approach to lake restoration requires the reestablishment of submerged macrophytes. However, macrophyte overgrowth in shallow lakes may lead to deterioration and a consequent necessity for restoration treatments. We assumed that a major threat to the increased trophic level in the Jankovac flow-through system arises from the sediment, where the accumulation of deciduous leaf litter and decayed macrophyte fragments could generate anoxic conditions. The integrated Water Quality Model (WQM) and the Submerged Aquatic Vegetation Model (SAVM) were combined in the Jankovac Model (JanM) and applied during the vegetated season in 2008 and 2014, with the aim to offer a possible approach to the maintenance of good water quality. The impacts of flow velocity and epiphyton growth on submerged macrophyte coverage and biomass were simulated. Biocenotic analyses suggested that epiphyton growth was more extensive in 2014 in comparison to 2008. The results of JanM indicated that increased flow velocities enhanced macrophyte growth and dissolved oxygen concentrations concurrently with the decline of epiphyton biomass. Furthermore, results suggested that epiphyton growth rate of 0.4 d⁻¹ maintained macrophyte coverage and biomass at a satisfactory level of 70% reservoir coverage. Considering the proposed scenarios hydraulic treatment could be applied to regulate submerged macrophytes in shallow reservoirs, as an efficient and less invasive approach than sediment removal, especially in sensitive karst areas.     

Effects of an artificial protection structure on the sandy shore macrofaunal community: the special case of Lido di Dante (Northern Adriatic Sea)

Biomanipulation of eutropicated peaty lakes has rarely been successful; clear water with dense macrophyte stands fails to develop in most cases. It was unclear whether (1) high turbidity due to resuspension by benthivorous fish or wind is the major cause of low macrophyte density or whether (2) the establishment of submerged macrophyte stands is prevented by a lack of propagules, low cohesive strength of the lake sediment, high concentrations of phytotoxics, grazing by waterfowl and/or shading by periphyton growth. These hypotheses were tested in an experiment in a shallow peat lake in the Netherlands (Terra Nova). Removal of fish from a 0.5 ha experimental site resulted in clear water and the development of a dense (90% coverage) and species-rich (10 species) submerged vegetation. At a fish-stocked site and a control site the water remained turbid and dense macrophyte stands did not develop. The establishment of submerged macrophytes appeared not to be limited by a lack of propagules. Introduced plants grew poorly in turbid water, but very well in clear water. Exclosures showed that bird grazing reduced the plant biomass. In clear water grazing seemed to enhance the vegetation diversity. Periphyton development did not prevent plant growth in clear water. After the experiment, the fish stock was greatly reduced in the whole lake (85 ha), to test if (3) in a large lake, submerged macrophyte stands will not develop after biomanipulation. In the first season after fish reduction, transparency increased and species-rich submerged macrophyte stands developed, covering 60% of the shallow parts of the lake. Most of the species known to have occurred in the past re-established. The results indicate that high turbidity caused by benthivorous fish in combination with bird grazing were the major causes of the absence of submerged macrophyte stands in this lake. Abiotic conditions after the clearing of the lake were suitable for the growth of macrophytes. We infer that the restoration potential of submerged macrophyte stands in eutrophicated peaty lakes can be high, and results can be obtained quickly.     

衰亡期黑藻与生长期菹草交替生长对水体磷迁移的影响

为利用冷暖种交替控制水体磷污染、抑制水体富营养化,揭示湖泊演化规律和机理。研究设置单季植物组(黑藻组、菹草组)和交替生长组(黑藻组+菹草组)进行实验。交替生长组在黑藻衰亡期种植菹草,监测各组上覆水和底泥中各形态磷含量的变化,计算黑藻衰亡释放磷及菹草生长吸收磷的总量,同时测定环境因子指标。分析沉水植物交替生长(黑藻+菹草)过程对衰亡期沉水植物(黑藻组)释放磷所带来的二次污染的消减作用,并分析环境因子变化与磷含量之间的关系。实验结果表明:黑藻+菹草组显著(P<0.05)降低了上覆水中总磷(TP)、溶解性总磷(DTP)和溶解性活性磷(SRP)的浓度;显著(P<0.05)降低了间隙水中DTP和SRP的浓度。底泥TP含量黑藻组呈上升趋势,黑藻+菹草和菹草组呈下降趋势。在采用菹草生物量期望2倍于衰亡植物黑藻生物量的模拟实验条件下,每实验组沉水植物黑藻衰亡分解所释放的磷为1.51 g,沉水植物菹草生长所富集吸收的磷为1.83 g。因此,菹草具备消减黑藻所释放磷的能力,可作为冷暖种交替控制水体富营养化的备选物种。实验组磷的迁移方向分别为:黑藻组磷迁移最终方向为底泥,黑藻+菹草组和菹草组磷的迁移方向为植物。黑藻+菹草组通过提高环境中DO和ORP,使得水相中磷向沉积物相中迁移,从而使得水相中各形态磷浓度保持在相对较低的水平。     

Phytoplankton biomass in Lake Xolotlán (Managua): Its seasonal and horizontal distribution

Some well-documented studies on restoring eutrophic lake systems in The Netherlands by fish stock management have been evaluated with the emphasis on the role of macrophytes. Furthermore, the factors determining the light climate for submerged macrophytes in a large shallow eutrophic lake (Lake Veluwe) have been assessed and the potential success of biomanipulation in large scale projects is discussed. Today relatively little attention has been paid to macrophyte management although the importance of macrophytes in lake restoration has been recognized regularly. The biomanipulation strategy was successful in small scale projects. In a large scale project, however, wind-induced resuspension may largely determine the underwater light climate through attenuation by the water column and periphytic layer. Therefore, restoration of relatively large waterbodies by fish stock management only is expected not to lead to any noteworthy improvement of the light climate for submerged macrophytes. Additional measures aimed at reducing wind-induced resuspension of sediment particles and reestablishing of the macrophyte stands are required for successful biomanipulation strategies. Water quality managers should pay more attention to macrophyte stands in biomanipulation projects because macrophytes enhance a more stable and diverse ecosystem. Restoration objectives and the methods of their achievement must be carefully planned since an abundant submerged macrophyte vegetation may have undesirable effects as well.     

The interaction between water movement,sediment dynamics and submersed macrophytes

Water movement in freshwater and marine environments affects submersed macrophytes, which also mediate water movement. The result of this complex interaction also affects sediment dynamics in and around submersed macrophyte beds. This review defines known relationships and identifies areas that need additional research on the complex interactions among submersed macrophytes, water movement, and sediment dynamics. Four areas are addressed: (1) the effects of water movement on macrophytes, (2) the effects of macrophyte stands on water movement, (3) the effects of macrophyte beds on sedimentation within vegetated areas, and (4) the relationship between sediment resuspension and macrophytes. Water movement has a significant effect on macrophyte growth, typically stimulating both abundance and diversity of macrophytes at low to moderate velocities, but reducing growth at higher velocities. In turn, macrophyte beds reduce current velocities both within and adjacent to the beds, resulting in increased sedimentation and reduced turbidity. Reduced turbidity increases light availability to macrophytes, increasing their growth. Additionally, macrophytes affect the distribution, composition and particle size of sediments in both freshwater and marine environments. Therefore, establishment and persistence of macrophytes in both marine and freshwater environments provide important ecosystem services, including: (1) improving water quality; and (2) stabilizing sediments, reducing sediment resuspension, erosion and turbidity.     

Sources of nutrients to rooted submerged macrophytes growing in a nutrient-rich stream

1. The relative contribution of roots and leaves to nutrient uptake by submerged stream macrophytes was tested in experiments where plants were grown in an outdoor flow-channel system. Water was supplied from a nutrient-rich stream with inorganic nitrogen and phosphorus concentrations typical of Danish streams.
2. Four submerged macrophyte species were tested, Elodea canadensis , Callitriche cophocarpa , Ranunculus aquatilis and Potamogeton crispus, and all species were able to satisfy their demand for mineral nutrients by leaf nutrient uptake alone. This was evident from manipulative experiments showing that removal of the roots had no negative impact on the relative growth rate of the plants. Further, the organic N and P concentrations of the plant tissue was constant with time for the de-rooted plants.
3. Enrichment of water and/or sediment had no effect on the relative growth rate of two species, E. canadensis and C. cophocarpa , indicating that in situ nutrient availability was sufficient to cover the needs for growth. Despite the lack of a response in growth rate, a reduced root/shoot biomass ratio was observed with nutrient enrichment of water and/or sediment, and an increased tissue-P concentration in response to open-water enrichment.
4. The open-water nutrient concentrations of the stream in which the experiments were performed are in the upper part of the range found for Danish farmland streams (the majority of Danish streams). Still, however, the negligible effect of nutrient enrichment on the growth of submerged macrophytes observed suggests that mineral nutrient availability might play a minor role in controlling macrophyte growth in most Danish streams.     

湖泊底质与水生植物相互作用综述

简要阐述了湖泊生态系统中底质和水生植物的概念及重要性,综述了底质理化性质对水生植物生长的影响,以及水生植物对底质营养盐的释放和底质再悬浮的作用。通过大量的研究综述回顾论述了不同的湖泊底质类型在一定程度上决定了水生植物的生长状态,适合的底质营养盐范围能促进水生植物生长,不同水生植物对底质营养盐的耐受性有差异。水生植物能促进底质沉降并减少再悬浮,水生植物的存在对沉积物中磷的活性有显著的影响。污染底泥的修复能为水生植物的立地与生长提供了良好的底质条件,有利于富营养化湖泊水生植被的恢复与重建。