The importance of water regimes operating at small spatial scales for the diversity and structure of wetland vegetation

1. In most cases, the most important determinant of wetland vegetation is the water regime. Although water regime is usually described and managed at the scale of whole wetlands, the patterning of vegetation is likely to be determined by water regimes that are experienced at much finer spatial scales. In this study, we assess the significance of internal heterogeneity in water regimes and the role that this heterogeneity plays in vegetation patterning. 2. The effects of water regime on wetland plant species richness and vegetation structure were studied at Dowd Morass, a 1500 ha, Ramsar‐listed wetland in south‐eastern Australia that is topographically heterogeneous. Data on plant variables and water depth were collected along 45 (50 m) transects throughout the wetland and related to water regimes assigned individually for each transect. Wetland plants were assigned to plant functional groups (PFG) that describe the response of plants to the presence or absence of water at different life stages. 3. The classification of water depth data indicated four distinct water regimes in the wetland that were differentiated primarily by the duration of the dry period. Representatives of all PFGs co‐existed over small spatial scales where topographical variation was present, and the richness and cover of understorey species declined as transects became more deeply and permanently flooded. Some PFGs (e.g. amphibious fluctuation tolerator‐low growing and amphibious fluctuation responder‐morphologically plastic) were eliminated by extended periods of flooding, which increased the cover but not richness of submerged plants. Species richness and foliage projective cover declined as water regimes shifted from shallow and frequently exposed conditions to regimes typified by deeper and longer inundation. Cover of the structurally dominant woody species was compromised by deeply flooded conditions but vegetative regeneration occurred despite high water levels. 4. Internal topographical variation generates mosaics of water regimes at fine spatial scales that allow plant species with different water regime requirements to co‐exist over small distances. Deep water and an absence of dry periods result in decreased cover of plants and an overall loss of species richness in the understorey. Water regimes are described that promote regeneration and cover of structurally dominant taxa and increased species richness in the understorey. The study demonstrates a strong association between vegetation and the diverse water regimes that exist within a single wetland, a pattern that will be useful for modelling the effects of modified water regimes on wetland vegetation.     

Effects of land use on aquatic macrophyte diversity and water quality of ponds

1. Aquatic macrophyte diversity and water quality of 55 ponds in western Japan were related to land use and morphometric variables to identify the environmental factors that sustain biodiversity and the spatial extent at which these factors operate. 2. The relevant spatial extent for floating‐leaved macrophyte richness (500 m from pond edge) was larger than that for submerged macrophyte occurrence (10, 75 and 100 m), whereas emergent macrophyte richness was best explained at much larger extents (1000 m). Total macrophyte richness was explained at the extent of 500, 750 and 1000 m. The extents relevant for explaining the physicochemical condition of pond water (100 and 250 m) were similar to those for submerged and floating‐leaved macrophytes, suggesting that these two growth forms are more sensitive to water quality compared to emergent macrophytes. 3. Diversity of all three growth forms and that of total macrophytes collectively were inversely related to turbidity and nutrient concentration; among the three growth forms, submerged macrophytes were most affected by water quality. 4. Negative relationships were found between the proportion of urban area and the diversity of the three growth forms and that of total macrophytes and water quality. Species richness of emergent, floating‐leaved and total macrophytes decreased with depth and increased with surface area up to about 5000 m², above which it declined. 5. Urbanisation and enlargement of ponds were the two main factors that decreased aquatic macrophyte diversity in irrigation ponds. To alleviate the adverse effects of urban areas on aquatic macrophyte diversity, our results suggest that management efforts should focus on the creation of buffer zones within the relevant spatial extent from the pond edge.     

河漫滩湿地生态阈值——以二卡自然保护区为例

以典型河漫滩湿地 —— 二卡自然保护区为研究区域,进行生态阈值研究。根据湿地补给河流 —— 海拉尔河的月均流量频率分布特征,选取58.72 m³/s(P=74.6%)、119.26 m³/s(P=44.4%)、190.35 m³/s(P=23.8%)分别代表河流的低、中、高径流期,分析各径流期湿地分布特征。结果表明,低、中径流期内草本沼泽及盐化沼泽所占比例较高,而高径流期则以季节性河流湿地及湖泊湿地为主。低径流期内,作为湿地中心区的湖泊湿地景观破碎度出现一个较明显的跃变,由中径流期的0.57增加到1.37。此时的湿地状态可近似的作为区域的生态阈值,即维持湿地面积占全区域面积的43.03%。而中、高径流期湿地面积比例可近似作为保护区湿地面积的适宜值和理想值,分别为53.66%和69.53%。其研究结果为二卡自然保护区的管理及保护提供支持,并为河漫滩湿地研究提供思路。     

稳定碳同位素在滨海湿地碳生物地球化学循环中的应用

碳作为滨海湿地中重要的生命元素,其生物地球化学循环过程是滨海湿地研究的核心内容之一.稳定同位素技术越来越多地被应用到滨海湿地碳生物地球化学循环过程的研究中,提高了其研究水平,并推动了其研究的进程.本文从有机物质生产、土壤有机质来源、食物链传递、温室气体排放以及可溶性有机碳输出5个方面,综述了滨海湿地碳生物地球化学循环过程的稳定同位素研究进展.通过植物及土壤δ13C值的测定进行有机质的生产机理研究及外源追溯,通过对比各生物种群的δ13C值分析碳在生态系统中的流动过程,通过湿地排放温室气体及可溶性有机碳δ13C值的测定揭示影响碳输出的环境因子.最后,文章总结了当前研究中存在的问题,并对其研究前景进行了展望.     

东洞庭湖丁字堤苔草群落特征及其影响因子

近20年来,洞庭湖湿地的湖草面积大幅度减少,退化严重.为寻求湖草的恢复途径,本文以位于洞庭湖丁字堤的短尖苔草为对象,依高程差划分成7条样带,调查了63个样方的植被特征(株高、盖度、密度、生物量、多样性指数)和土壤理化特征(土壤有机碳、全氮、全磷、土壤容重、土壤含水量).结果表明: 除多样性指数先下降后升高外,其余生物学指标均随高程增加呈现倒“U”型分布,即靠近水域(低海拔区)和堤岸(高海拔区)的苔草长势较差,而位于中间的苔草长势较好;土壤容重随高程增加而增加,土壤含水量的变化则相反,土壤有机碳和全氮含量均呈中海拔区高、低和高海拔区低的分布规律.主成分分析表明,影响苔草生物量的关键因子依次为土壤有机碳含量、氮含量、含水量和土壤容重.可见,提高土壤肥力和保持适当的土壤含水量可能是短尖苔草恢复的有效途径.     

RS和GIS支持的洪河地区湿地生态健康评价

洪泛平原淡水自然湿地对于生态多样性保护具有重要意义。当前自然湿地普遍面临气候变化与人类活动干扰和影响,其生态健康的状况令人担忧,结合新的地学信息技术探索自然湿地生态健康评价分析方法具有重要意义。本研究选择位于三江平原东北部的洪河国家级自然保护区湿地及其周边农场湿地为研究区,依据遥感和地理信息系统技术支持,结合野外生态调查与水文气象监测数据,从水文地貌特征、景观特征和人类扰动3方面选取一系列评价指标因子,利用层次分析法和综合指数方法,对研究区湿地进行了定量生态健康分析评价。研究结果表明：（1）洪河自然保护区的湿地生态健康状况是最好的,其周边农场从鸭绿河农场、前锋农场到洪河农场的湿地生态健康状况依次递减。（2）洪河自然保护区功能分区生态健康状况由好到差的顺序为：核心区>缓冲区>实验区,与实际野外调查情况一致。（3）本研究建立的评价指标体系和相应分析方法能够科学的评价湿地生态健康。评价分析结果显示水文地貌要素是影响湿地生态健康的关键性因素。本研究利用RS和GIS技术与传统生态学评价分析方法结合,以栅格为单位基于区域生境特征进行湿地生态健康综合评价具有一定的方法先进性。     

水淹频率变化对鄱阳湖增强型植被指数的影响

水淹状况是湿地植被动态的重要影响因素。该研究基于谷歌地球引擎(GEE)平台, 利用2000-03-01至2020-02-29所有覆盖研究区域的MODIS遥感影像数据, 分析20年间水淹频率(IF)、增强型植被指数(EVI)的时空变化以及湿地植被对IF变化的响应, 得出以下结论: (1) 20年来鄱阳湖水文节律发生了明显改变, 高IF (IF > 75%)水域面积呈现下降趋势, 从2000年1 435.3 km²下降至2019年的510.25 km², 降幅为64.45%; (2)区域平均EVI呈显著上升趋势, 植被扩张主要集中在中部IF下降区域; (3)分析不同总水淹频率区域中平均EVI年际变化, 发现EVI与水淹状况的变化趋势相似, 2009年之后鄱阳湖水域面积萎缩趋势缓解, EVI增长速度出现下降; (4)鄱阳湖湿地植被主要沿水域面积萎缩方向扩张, 基于像元统计20年间IF与EVI的变化趋势, 发现它们在空间分布上高度吻合, 这种空间异质性进一步证实水淹状况起到调节植被动态变化的作用。     

基于水文地貌法模型的城市湿地水环境功能评估——以南京仙林典型湿地为例

我国正处于快速城市化发展过程中,许多湿地被改造利用成为城市湿地。如何科学评估城市湿地功能及其改变程度,是科学认识城市湿地的重要内容。基于水文地貌法,通过选取区域受城市化影响小、生态系统结构与功能接近于自然湿地的湿地作为参考湿地,利用遥感和GIS的手段以及野外实地调查方法,从湿地水环境功能角度,对南京仙林区域内典型城市湿地的水环境特征与功能进行评估。结果表明:(1)城市湿地水环境功能明显降低,其蓄水功能、净水功能、水文调节功能明显低于参考湿地;(2)受城市化景观复杂性影响,城市湿地水环境功能的改变程度呈现个性化特征,纪家边、采月湖和西湖西这3个湿地可以作为城市化过程中湿地改造的典范。这一结论可为城市化区域内湿地的合理开发利用以及湿地的保护、恢复提供科学依据。     

管网雨水补给河道用水的人工湿地水质净化流程研究

中国北方部分地区水资源短缺,河道干涸,但夏季雨水资源潜力丰富。虽径流受到一定污染,但较于生活污水和工业废水,其污染程度更低,成分更简单。雨水通过低运行成本的人工湿地净化系统,可以实现较好的净化效果,满足河道景观需求和生态补水。城市管网雨水承载能力过重的城市边缘区,建设更新过程中进行雨污分流制度,更适于采用人工水质净化的方式将城市雨水管网中的雨水进行就近消纳,减轻城市雨水管网压力,并利用表面负荷率（ALR）来确定并校核人工湿地面积。在综合现在人工水质净化主流程预处理单元、人工湿地单元和消毒存储单元3个环节的基础上,以低运营成本、低管理成本、最优净水量为指向,引入物联网技术智能管控系统,行程具有能控制各级出水水质监测、多级管控、净水生态功能与游览景观功能相结合等多重优点的人工水质净化全流程,达到符合河道水质标准的净化效果。该流程为缓解北方城镇河道缺水现状、解决城市雨洪问题提供新思路。     

长江口崇明东滩湿地沉积物对磷的吸附特征

研究了崇明东滩湿地低(S1)、中(S2)、高(S3)潮滩沉积物对磷的吸附特征。结果表明,沉积物吸磷过程主要发生在前24 h内,随后近于达到平衡状态。沉积物对PO43--P的平均吸附速率在0~0.5 h内最大,均超过了140 mg.kg-1.h-1;快速吸附过程主要发生在前11 h,前11 h的平均快速吸附速率表现为S1>S3>S2,且沉积物中细颗粒成分越多,沉积物对PO43--P的平均快速吸附速率越大。沉积物对磷的吸附等温线符合Langmuir吸附等温方程,根据Langmuir方程计算,沉积物对磷的吸附容量均>200 mg.kg-1,同时沉积物对PO43--P的吸附容量也表现为S1>S3>S2。原因可能同S1中细颗粒成分、有机碳和常量金属元素(Al、Ca、Fe、Mg)的百分含量较多而S2中细颗粒成分、有机碳和常量金属元素的百分含量较少有关。温度和pH值也影响沉积物对PO43--P的吸附作用。