黄河三角洲芦苇湿地的恢复

近年来由于人类活动及自然灾害等多种因素的影响,黄河三角洲芦苇湿地生态系统的健康受到威胁,出现不同程度的退化。为进一步研究2002年开始实施的湿地恢复工程,选择未恢复区、恢复区比较其水、植被、土壤等生态特征,结合野外调查及实验分析数据,结果显示至2005年7月恢复区湿地水域面积比例增加,水质得到明显改善,植被群落呈正向演替,土壤达到中、轻度盐化土水平,水禽种类增加,生物多样性更加丰富。研究结果表明,以恢复湿地水文条件为核心措施的湿地恢复方案具有可行性。研究对于黄河三角洲其他类型湿地的恢复及改善其生态功能具有指导作用。     

Integrated stream and wetland restoration: A watershed approach to improved water quality on the landscape

Water quality in Upper Sandy Creek, a headwater stream for the Cape Fear River in the North Carolina Piedmont, is impaired due to high N and P concentrations, sediment load, and coliform bacteria. The creek and floodplain ecosystem had become dysfunctional due to the effects of altered storm water delivery following urban watershed development where the impervious surface reached nearly 30% in some sub-watersheds. At Duke University, an 8-ha Stream and Wetland Assessment Management Park (SWAMP) was created in the lower portion of the watershed to assess the cumulative effect of restoring multiple portions of stream and former adjacent wetlands, with specific goals of quantifying water quality improvements. To accomplish these goals, a three-phase stream/riparian floodplain restoration (600 m), storm water reservoir/wetland complex (1.6 ha) along with a surface flow treatment wetland (0.5 ha) was ecologically designed to increase the stream wetland connection, and restore groundwater wetland hydrology. The multi-phased restoration of Sandy Creek and adjacent wetlands resulted in functioning riparian hydrology, which reduced downstream water pulses, nutrients, coliform bacteria, sediment, and stream erosion. Storm water event nutrient budgets indicated a substantial attenuation of N and P within the SWAMP project. Most notably, (NO₂⁻ + NO₃⁻)-N loads were reduced by 64% and P loads were reduced by 28%. Sediment retention in the stormwater reservoir and riparian wetlands showed accretion rates of 1.8 cm year⁻¹ and 1.1 cm year⁻¹, respectively. Sediment retention totaled nearly 500 MT year⁻¹.     

Creating riverine wetlands: Ecological succession, nutrient retention, and pulsing effects

Successional patterns, water quality changes, and effects of hydrologic pulsing are documented for a whole-ecosystem experiment involving two created wetlands that have been subjected to continuous inflow of pumped river water for more than 10 years. At the beginning of the growing season in the first year of the experiment (1994), 2400 individuals representing 13 macrophyte species were introduced to one of the wetland basins. The other basin was an unplanted control. Patterns of succession are illustrated by macrophyte community diversity and net aboveground primary productivity, soil development, water quality changes, and nutrient retention for the two basins. The planted wetland continued to be more diverse in plant cover 10 years after planting and the unplanted wetland appeared to be more productive but more susceptible to stress. Soil color and organic content continued to change after wetland creation and wetlands had robust features of hydric soils within a few years of flooding. Organic matter content in surface soils in the wetlands increased by approximately 1% per 3-year period. Plant diversity and species differences led to some differences in the basins in macrophyte productivity, carbon sequestration, water quality changes and nutrient retention. The wetlands continued to retain nitrate–nitrogen and soluble reactive phosphorus 10 years after their creation. There are some signs that sediment and total phosphorus retention are diminishing after 10 years of river flow. Preliminary results from the beginnings of a flood pulsing experiment in the two basins in 2003–2004 are described for water quality, nutrient retention, aboveground productivity, and methane and nitrous oxide gaseous fluxes.     

Estimating biogeochemical and biotic interactions between a stream channel and a created riparian wetland: A medium-scale physical model

Straightened channels and altered and drained adjacent riparian wetlands have adversely impacted streams and rivers throughout the US Midwest. This research investigated the biological connection and water quality of a 0.07 ha diversion wetland and adjacent stream at the Olentangy River Wetland Research Park in central Ohio. Before the flowthrough conditions were established, we demonstrated with mark and recapture techniques that the wetland already was a biorefuge for fish under extreme conditions; two species (Centrarchidae) captured in the stream before a total drawdown of the stream were found in the wetland a year later. In addition, water at the bottom remained at around 4 °C over the winter likely due to groundwater input, which possibly provided a warmer shelter for fish. Stream water quality of the lower section, downstream of the wetland outlet, generally improved with hydrologic pulsing in spring after flow-through reconnection due to the trapping of nutrients in the wetland. Mean removal per flood pulse for nitrate-nitrite, total nitrogen (TN), soluble reactive phosphorus (SRP), total phosphorus (TP) were 1.81 g-N m⁻² per pulse, 1.02 g-N m⁻² per pulse, 0.014 g-P m⁻² per pulse, and 0.004 g-P m⁻² per pulse, respectively. The wetland exported 2.8 g-C m⁻² per pulse of organic carbon. A greater attenuation of NO₃⁻ and TP occurred in the marshy outlet channel section of the wetland than the open water section. The diversion wetland successfully removed nitrate and phosphorus during storm pulses in spring. Similar designs should be applied to other locations to examine their function under different climatic and hydrological conditions.     

湿地生态系统生态特征变化及其可持续性问题

湿地是具有多种功能和价值的生态系统,是人类最重要的环境资源之一,被称为“景观之肾”［１］。湿地在蓄洪防旱、调节气候、控制土壤侵蚀、促淤造陆、降解环境污染等方面起着极其重要的作用［２］。随着人口的增长,人类对其影响的规模和速度在不断扩大,这其中有直接的...     

A method to prioritize and monitor wetland restoration for water-quality improvement

Wetland restoration can improve water quality by reducing concentrations of sediment, total phosphorus, and nitrate in runoff. Managers need a simple method to choose among many possible restoration sites, particularly in large agricultural basins covering thousands of square kilometers. The purpose of this paper is to outline a method for prioritizing and monitoring wetland restoration sites in light of the factors that affect water-quality improvement by wetlands. These factors are categorized as loading factors, path factors, and process factors. The method for prioritizing wetland restoration sites depends primarily on assessing the potential effectiveness of the wetland for improving water quality. Three types of effectiveness are considered: problem effectiveness (is the site in an area with known water-quality problems?), function effectiveness (is the site likely to improve water quality more or less than other sites?), and information effectiveness (does the site fit within an overall research plan to gain information on how wetlands improve water quality?). The variables of hydraulic residence time, hydraulic flux, and wetland area, volume, and average depth are combined into a single variable termed and used as a proxy for estimating the relative function effectiveness of potential restoration sites. Monitoring restoration sites is targeted at establishing a minimum data set that can be collected consistently at different sites over time, and that can be used for inter-site comparison with simple statistical techniques. The Minnesota River Basin is used as an example throughout to demonstrate the types of data that are available to plan wetland restoration. While this paper focuses on the water-quality benefits, wetland restoration should be a multi-disciplinary effort to integrate other benefits of restoration, such as improvement of wildlife habitat and flood abatement.     

雄安新区白洋淀生态属性辨析及生态修复保护研究

湿地是自然界生物多样性最丰富的生态系统之一,与社会发展和人类福祉息息相关。近年来,由于全球气候变化和人类活动的过度干扰,湿地正面临着面积萎缩、功能减弱、多样性降低等诸多问题,湿地退化已经成为制约区域可持续性发展的重大阻碍。伴随着生态文明建设逐渐成为中国特色社会主义建设的重要支柱,湿地生态修复工作得到前所未有的制度保障。深入剖析湿地属性,结合政策保障,有针对性的提出湿地保护与修复的治理措施,对区域的生态环境建设和可持续性发展具有重要意义。选择国家级新区-雄安新区的水命脉-白洋淀湿地为研究对象,在深入剖析其生态属性和已存在的生态问题的基础上,结合生态修复的原则、方法和步骤,提出生态修复与保护的可行性策略。研究结果表明,白洋淀本质是典型的湖泊湿地,同时兼具沼泽湿地特征,由于人类活动的剧烈干扰,白洋淀有向沼泽湿地逆向演替的变化趋势。湿地内存在面积萎缩、水资源量短缺、水环境污染问题突出及生物多样性减少等生态问题。本研究建议:为顺利建设雄安新区,首先,白洋淀湿地在算清"水账"、"污账"和"生态账"的前提下,进一步加强流域水资源调配,科学确定白洋淀湿地最佳水位,恢复淀区水量;其次,通过使用清洁生产技术和限制高排污企业建设等措施,加强污染防治,恢复湿地水质;最后,依据生态承载力理论,划分白洋淀流域的生态功能红线、环境质量红线和资源利用红线等国家生态保护红线体系,为尽快恢复湿地结构与功能提供制度保障。     

Hydrologic similarity to reference wetlands does not lead to similar plant communities in restored wetlands

Few wetland restoration projects include long‐term hydrologic and floristic data collection, limiting our understanding of community assembly over restored hydrologic gradients. Although reference sites are commonly used to evaluate outcomes, it remains unclear whether restoring similar water levels to reference sites also leads to similar plant communities. We evaluated long‐term datasets from reference and restored wetlands 15 years after restoration to test whether similar water levels in reference and restored sites led to vegetation similarity. We compared the hydrologic regimes for three different wetland types, tested whether restored wetland water levels were different from reference water levels, and whether hydrologic similarity between reference and restored wetlands led to similarity in plant species composition. We found restored wetlands had similar water levels to references 15 years after restoration, and that species richness was higher in reference than restored wetlands. Vegetation composition was similar across all wetland types and was weakly correlated to wetland water levels overall. Contrary to our hypothesis, water table depth similarity between restored and reference wetlands did not lead to similar plant species composition. Our results highlight the importance of the initial planting following restoration and the importance of hydrologic monitoring. When the restoration goal is to create a specific wetland type, plant community composition may not be a suitable indicator of restoration progress in all wetland types.     

Planning for the recovery of Lake Toolibin,Western Australia

Lake Toolibin, an intermittently flooded freshwater wetland in the southwest of Western Australia, is threatened by salinization due to extensive clearing within its catchment. The lake is a Wetland of International Importance under the Ramsar Convention because of the extensive stands of trees on the lake bed and its significance as a waterbird breeding site. Past research and monitoring have identified the causes of wetland vegetation and water quality decline and this information has been used to design a Recovery Plan for the lake. The plan is currently in the early stages of implementation and includes both short-term engineering measures to reduce salinity within the lake and long-term rehabilitation measures within the catchment. Community involvement in the recovery process is an integral part of the plan and ensures that recovery of the lake remains as the focus for ongoing catchment rehabilitation.     

滇西北高原入湖河口退化湿地生态修复效益分析

选取滇西北高原典型退化湿地剑湖,对入湖河流永丰河入湖河口退化湿地进行的生态修复措施及其效益进行研究,评估其恢复效果,为高原退化湿地的修复和污染湖泊的治理提供依据。研究地修复2a后,入湖河口湿地景观格局得到较大改善,空间结构得到优化配置;水质状况明显改善,水体透明度提高101%,水体中总氮(TN)、氨氮(NH+4-N)、硝氮(NO-3-N)、总磷(TP)、化学需氧量(COD)的含量较恢复前明显下降,去除率分别达到62.5%、89.3%、62.5%、91.7%、68.0%,这一水质降解结果表明:基底修复促进了入湖河口水文状况的改善,而依据植物对不同浓度污水的适应状况进行多生活型、多种类的植物配置,并适当增加沉水植物比例,有效发挥了植物的净化作用,但不同湿地植物群落之间净化效果存在差异,显示了植物对氮磷的喜好程度和植物间的互作关系,而相同植物群落在不同浓度污水条件下的表现同样存在差异。因此,污染水体的治理必须选择性利用适合不同污水浓度的水生植物进行合理的群落配置,同时,根据水质变化及时对植物进行适应性调整,有利于植物的生长和湿地生态系统的稳定,以及湿地生态系统结构和功能的恢复。该退化湿地修复后,每年可产生以净化功能效益为主的生态系统服务功能价值185万元,以水源涵养和生物多样性保育、生态旅游等的生态系统服务功能价值32.7万元,以及以生态农业系统为主的市场价值270万元,呈现了较好的经济、社会效益和生态效益价值。     

Prediction of potential macrophyte development in response to restoration measures in an urban riverine wetland

Wetland restoration efforts require practical models for predicting the effects of various measures on ecosystem structure and function. The present study examined the species diversity and abundance of macrophytes in relation to hydrological parameters in the Alluvial Zone National Park along the Austrian Danube with a main focus on the Lobau, an urban riverine wetland within the city limits of Vienna. A macrophyte regression model was developed based on the output of a 2D hydraulic model for different wetland management options. These management options describe possible rehabilitation measures by re-connecting the riverine wetland with the Danube. Stepwise multiple regressions revealed that the most important predictors of macrophyte diversity and abundance were water velocity at bankfull discharge (maximum water velocity) and size of shallow water areas (<1 m depth) during the growing season. Macrophyte abundance and diversity increased with decreasing water velocity and increasing shallow water area. These parameters integrate information about environmental features such as nutrients, light availability and hydrological disturbance for macrophytes and explained between 65 and 85% of the macrophyte distribution in an analysis. The model results enabled us to predict quantitatively the development and spatial distribution of macrophytes for different management options in this urban riverine wetland. These predictions suggest that partial reconnection could be a compromise solution at the scale of the whole riverine wetland, increasing the availability of suitable aquatic habitats and diversifying the types of existing wetland water bodies to establish potential new habitats for macrophyte species.     

普者黑岩溶湖泊湿地湖滨带景观格局演变对水质的影响

湖滨带作为湖泊与陆地之间的过渡带,是健康湖泊生态系统的重要组成部分。湖滨带景观格局的演变会对湿地水质产生重要影响,因此探究影响岩溶湿地水质变化的湖滨带关键景观因子,对深入了解景观格局对岩溶湿地水质的影响过程与机制具有重要意义。选择普者黑岩溶湖泊湿地为研究对象,以2005、2007、2009、2011年共4年的Landsat遥感影像及水质监测数据为基础,通过划定湖泊湿地湖滨带缓冲区域,运用秩相关分析和冗余分析研究湖滨带景观格局对普者黑岩溶湖泊湿地水质的影响。结果表明,湖滨带不同缓冲区内景观结构类型比例差异较大;枯水期水质与土地利用类型和景观格局指数的影响大于丰水期;景观格局在不同缓冲区尺度对岩溶湿地的水质具有不同的效应;随着监测点缓冲距离的增加,个别景观指数可较好的揭示湖滨带景观格局演变对岩溶湿地水质的影响,其中,蔓延度指数(CONTAG)、斑块结合度指数(COHSION)、均匀度指数(SHEI)对水质参数的影响较大,边界密度(ED)、聚集度(AI)对水质参数的影响随缓冲距离的增加逐渐减弱,其他景观指数对水质影响差异并不明显,最大斑块指数(LPI)在缓冲距离≤300m的区域内与水质的关系较密切,面积加权平均斑块分维数(AWMPFD)与水质参数有显著负相关性,多样性指数(SHDI)对水质的影响具有不确定性;另外,大部分水质参数与土地利用面积比例有较好的相关性,且湿地面积比例是表征岩溶湖泊湿地水环境质量的主要指标。     

盐沼湿地大规模恢复的概念生态模型——以盐城为例

大规模湿地生态恢复是一项耗资巨大、复杂的系统工程,需要以整个区域湿地结构和功能恢复作为基本目标,将时间和空间上分散的研究成果进行系统梳理,形成对区域湿地生态变化及其驱动因素的规律性认识。本研究以盐城盐沼湿地为案例,以1987年作为未干扰或干扰较少的状态,从结构-过程-功能耦合作用角度,确定区域湿地恢复的关键生态特征,包括:健康与动态潮间带湿地系统、碱蓬生态系统生产力与弹性、复杂景观镶嵌与相互作用、潮间带底栖动物丰富与鸟类觅食基地,以及濒危与关键水鸟种群保护。在此基础上,将围垦与土地利用、水管理、全球变化与海平面上升作为驱动区域湿地生态变化的三大外部因素;海岸侵蚀与沉积、区域水格局变化、地形地貌变化、湿地空间变化与连通性丧失,以及互花米草入侵等是影响湿地生态系统变化的内在压力因子;基于这些压力因子与湿地生态系统变化之间复杂作用关系分析,形成了外部驱动力-内在压力源-生态影响-生态特征之间联合作用下的区域湿地恢复概念生态模型。此模型以复杂因果关系研究为基础,直观展示了湿地恢复需要去除或减缓各种压力因子的一般路径,有利于指导大规模盐沼湿地恢复规划与实践。     

三江平原恢复湿地土壤种子库特征及其与植被的关系

通过幼苗萌发法和样方调查相结合的方法对三江平原不同演替恢复阶段的种子库特征及其与植被的关系进行了研究。将开垦湿地、不同演替恢复阶段湿地以及天然湿地不同土壤层次(0-5、5-10 cm和根茎)的种子库在两种水分条件下(湿润、淹水10 cm)进行萌发处理。结果表明: 随着演替恢复阶段的进行, 种子库的结构和规模逐渐扩大, 地表群落表现出由旱生物种占优势的群落逐渐演变成以小叶章(Calamagrostis angustifolia)占优势的湿生群落的演替趋势。恢复7年湿地、恢复14年湿地、天然湿地土壤种子库萌发物种数分别为24种、29种、39种, 植被物种数为21种、25种、14种。湿地类型、水分条件和土壤层次均显著影响种子库萌发的物种数及幼苗数(p < 0.01)。种子库具有明显的分层现象, 天然湿地0-5 cm土层种子库种子萌发密度是5-10 cm土层的4倍左右, 而恢复湿地仅1.3倍左右, 且土层间萌发物种相似性系数较低。湿润条件下的萌发物种数显著高于淹水条件, 且两种水分条件下萌发物种的生活型不同。由于恢复时间较短, 不同演替恢复阶段的种子库与植被相似性维持在30%以下。湿地中根茎分蘖出大量的湿地物种, 对于小叶章等优势物种的繁殖具有重要作用。研究表明, 在开垦湿地退耕后的次生演替阶段, 种子库能够保持大量的湿地物种, 通过对湿地种子库与植被的关系研究, 能够为三江平原湿地群落演替与湿地恢复提供策略指导。     

Algal assemblage responses to acid mine drainage and steel plant wastewater effluent up and downstream of pre and post wetland rehabilitation

Algae give a time-integrated indication of specific water quality components and respond rapidly to water quality changes making them useful for biomonitoring purposes. Freshwater algae were employed to differentiate between water quality conditions up and downstream before and after wetland rehabilitation to determine the feasibility of wetland enlargement as a possible rehabilitation measure. Grootspruit valley bottom wetland, impacted by acid mine drainage, was severely degraded before restoration. Rehabilitation was done through redirection of water flow using concrete structures to enlarge the surface area by 9.4 ha. After wetland rehabilitation, pH values, suspended chlorophyll-a and alkalinity concentrations increased downstream, while electrical conductivity, sulphate, total suspended solids decreased up to 80%. Algae species diversity and richness corresponded with the improvement of water quality and also increased downstream after rehabilitation. Overall, results indicated an improvement in algal diversity and water quality after enlargement of the bottom wetland.     

基于生态系统评价的山水林田湖草生态保护与修复体系构建研究——以乌梁素海流域为例

山水林田湖草系统保护与修复工程实施的重要目标是维护和提升区域生态系统服务。从乌梁素海流域山水林田湖草的生态现状与功能出发,对乌梁素海流域水土流失、土地沙化等生态敏感性及土壤保持、水源涵养、生物多样性等生态功能重要性进行系统评价,形成基于生态敏感性和生态功能重要性相结合的空间格局评价结果。以维护和提升人类福祉所需的重要生态系统服务为目标,以乌梁素海流域生态敏感性和生态功能重要性相结合的空间格局评价结果为基础,制定了“一中心、二重点、六要素、七工程”的乌梁素海山水林田湖草生态保护与修复体系,并基于此将乌梁素海流域生态保护修复分为6个主要治理区域,形成“四区、一带、一网”的生态安全格局,通过具体工程实施,流域生态环境质量和生态服务能力将取得明显提升,防风固沙能力有效增强,生物多样性持续改善,水环境质量稳定达标,生态系统的稳定性明显加强。通过乌梁素海流域的分析案例为流域山水林田湖草生态保护与修复关键区域的识别提供了定量分析方法,为流域尺度构建生态安全格局、实现山水林田湖草系统保护和修复提供思路和途径。     

上海大莲湖湖滨带湿地的生态修复

采用改变土地利用模式、水系改造和植被配置等技术开展了上海青浦大莲湖湿地修复示范工程。本文从2008年8月到2010年3月跟踪调查了土地利用方式、鸟类群落、两栖爬行类、水质等多类指标来对示范工程进行评估。结果表明,实验区生态系统的生境结构和生物多样性组成都发生了明显的变化。实验区内土地利用由主要以人工养殖鱼塘和林地为主的人工湿地(人工鱼塘占50%,林地占25%),转变为以开放性水域和乔灌草相结合的半自然状态下的自然湿地(明水面面积占30%,各类植被群落占50%,人工鱼塘完全消失),植被从只有片段化林地转变为乔木、灌木丛、草本植物及各类水生植物相结合的格局;工程后鸟类种类和数量均高于工程前(新纪录到11种鸟类),鸟类多样性指数和均匀性指数也有明显增加,其中目标鸟类——雁鸭类新增6种,种类和数量都呈显著增加;两栖爬行类种类变化不大,共记录到6科12种,但整体数量比工程前增长了59.1%;水质指标的变化也很突出,与工程前人工鱼塘相比,实验区内水体中总氮(TN)、硝态氮(NO3-N)、总磷(TP)、叶绿素a(Chla)、高锰酸钾指数(CODMn)等主要指标均有显著下降(P<0.05),水质改善显著。由此说明,修复工程改善了大莲湖湖滨带湿地的生态环境,生物多样性得到较好的恢复,呈现出良好的湿地修复效果。     

南京东郊城市湿地水质多尺度空间分异

对南京市东郊的17个城市湿地进行水质监测和植物群落调查,从生态系统、集水区和景观功能区3个尺度揭示城市湿地水质的分异特征.结果表明:湿地类型和植物群落特征是生态系统尺度上影响湿地水质的主要因素;原生湿地的水质普遍优于改造湿地,而改造湿地的水质则普遍优于次生湿地;湿地植物的盖度越大,水质越好.土地利用类型是集水区尺度上影响湿地水质空间分异的主要因素,建设用地对流域湿地营养盐影响程度较大,而林地对溶解氧影响程度较大.人类活动是功能区尺度上影响湿地水质空间分异的主要因素,而其对不同水质指标的影响程度不同.     

Managed flooding can augment the benefits of natural flooding for native wetland vegetation

Managed flooding is increasingly being used to maintain and restore the ecological values of floodplain wetlands. However, evidence for its effectiveness is sometimes inconsistent and water available for environmental purposes often limited. We experimentally inundated a floodplain wetland (or “billabong”) in late spring by pumping water from its adjacent creek, aiming to promote the native wetland flora and suppress terrestrial exotics. Vegetation was surveyed before (spring) and after (late summer) the managed flood in the experimental billabong and in three control billabongs. Floodplain water levels were continuously monitored. Wet conditions caused two of the control billabongs to also flood, but to a lesser extent than the experimental billabong. We therefore assessed vegetation changes relative to flooding duration. With increasing flooding duration, the cover of wetland vegetation (amphibious and aquatic species) increased and the cover of terrestrial and exotic vegetation decreased, with these effects largest in the deliberately flooded billabong. Flooding durations greater than 20 days generally resulted in increased cover of wetland plants and restricted the growth of terrestrial plants. Reinstatement of more appropriate flooding regimes can thus promote native wetland plants, while suppressing terrestrial exotic species. Our study also provides evidence for the use of modest water allocations to augment the benefits of natural flooding in the maintenance and restoration of native wetland plant communities.     

Assessing hydrogeochemical heterogeneity in natural and constructed wetlands

While water quality function is cited as animportant wetland function to design for and preserve,we demonstrate that the scale at which hydrochemicalsamples are collected can significantly influenceinterpretations of biogeochemical processes inwetlands. Subsurface, chemical profiles for bothnutrients and major ions were determined at a site insouthwestern Wisconsin that contained areas of bothnatural and constructed wetlands. Sampling wasconducted on three different scales: (1) a large scale(3 m between sampling points), (2) an intermediatescale (0.15 m between sampling points), and (3) a smallscale (1.5 cm between sampling points). In mostcases, significant vertical heterogeneity was observedat the 0.15 m scale, which was much larger thanpreviously reported for freshwater wetlands and notdetected by sampling water table wells screened overthe same interval. However, profiles of ammonia andtotal phosphorus showed tenfold changes in the upper0.2 meters of the saturated zone when sampled at thesmall (1.5 cm) scale, that was not depicted bysampling at the intermediate scale. At theintermediate scale of observation, one constructedwetland site differed geochemically from the naturalwetlands and the other constructed wetland site due toapplication of off-site salvaged marsh surface anddownward infiltration of rain. While importantdifferences in dissolved inorganic phosphorus anddissolved inorganic carbon concentrations existedbetween the constructed wetland and the naturalwetlands, we also observed substantial differencesbetween the natural wetland sites for theseconstituents. A median-polishing analysis of our datashowed that temporal variations in constituentconcentrations within profiles, although extensivelyrecognized in the literature, were not as important asspatial variability.