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91.
Long-term monitoring of estuarine nekton has many practical and ecological benefits but efforts are hampered by a lack of standardized sampling procedures. This study provides a rationale for monitoring nekton in shallow (<#60; 1 m), temperate, estuarine habitats and addresses some important issues that arise when developing monitoring protocols. Sampling in seagrass and salt marsh habitats is emphasized due to the susceptibility of each habitat to anthropogenic stress and to the abundant and rich nekton assemblages that each habitat supports. Extensive sampling with quantitative enclosure traps that estimate nekton density is suggested. These gears have a high capture efficiency in most habitats and are small enough (e.g., 1 m2) to permit sampling in specific microhabitats. Other aspects of nekton monitoring are discussed, including spatial and temporal sampling considerations, station selection, sample size estimation, and data collection and analysis. Developing and initiating long-term nekton monitoring programs will help evaluate natural and human-induced changes in estuarine nekton over time and advance our understanding of the interactions between nekton and the dynamic estuarine environment. 相似文献
92.
选取闽江河口鳝鱼滩芦苇湿地、短叶茳芏湿地及二者空间扩展过程中形成的交错带湿地为研究对象,探讨了空间扩展影响下湿地植物-土壤系统氮分布、转运特征及其影响因素.结果表明,空间扩展影响下交错带湿地土壤氮含量发生了较大改变,其全氮(TN)、铵态氮(NH4+-N)含量相比芦苇湿地分别降低了15.52%和6.08%,但相比短叶茳芏湿地分别增加了20.61%和4.33%;其硝态氮(NO3--N)含量相比芦苇湿地及短叶茳芏湿地分别降低了5.79%和13.84%.空间扩展主要通过改变植物生态特征、土壤EC及其颗粒组成而对湿地土壤氮的空间分布产生影响.空间扩展影响下湿地植物不同器官的TN含量亦发生了明显变化.相对于空间扩展前的纯群落,空间扩展后交错带芦苇和交错带短叶茳芏各器官的TN含量均明显增加;同时,在空间扩展后的交错带群落中,短叶茳芏各器官的TN含量均高于芦苇,前者主要与交错带植被对悬浮颗粒物拦截作用增强从而导致更多养分输入有关,后者主要与交错带短叶茳芏和芦苇对氮养分吸收与转运能力的差异有关.研究发现,相较于 短叶茳芏,空间扩展过程中的芦苇无论在氮养分吸收利用还是在向地上转运氮养分方面均处于明显优势,而这可能是导致短叶茳芏生态空间逐步被芦苇占据的一个重要因素. 相似文献
93.
Mark W. Busby Kenneth I. Darmer 《Journal of the American Water Resources Association》1970,6(5):802-812
This paper provides background information on the effect of tide waves upon the movement of water in the Hudson River estuary. Computations based on records from three continuous stage recorders and current-meter discharge measurements made throughout a tidal cycle show that peak discharge rates in the estuary at Poughkeep-sie may be as great as 500,000 cubic feet per second and that total daily tidal volumes as great as 20 billion cubic feet move in the estuary. Computation of water movement in the estuary requires precise field data and continued efforts are needed to perfect the data-collection system and the computation procedure in order to adequately define water movement in the Hudson estuary. 相似文献
94.
95.
96.
Mark E. Hines 《Water, Air, & Soil Pollution: Focus》2006,6(5-6):523-536
Microorganisms are responsible for the bulk of transformations that occur in surficial sediments. They are most active at
redox boundaries where they can benefit from access to various oxidants and reductants generated during redox cycling events.
To illustrate the dynamics of microbially mediated processes, especially those involving sulfur and metal cycles, processes
were compared in habitats either bioturbated by a capitellid worm or inhabited by a salt marsh grass. The presence of macrofauna
and macroflora greatly altered the three-dimensional array of redox gradients in sediments, but the type and form of reductants
and oxidants provided varied greatly; clastic sedimentary infauna subducted solid phase organic material and iron oxides,
whereas plant roots released dissolved organic matter and oxygen. These differences resulted in a bioturbated system that
exhibited a rapid sulfur cycle (residence time of minutes), but a slower iron cycle (days), whereas vegetation caused a slow
sulfur cycle and rapid iron cycle. Alteration of sediments by higher life forms also greatly affected the composition and
relative abundances of sedimentary bacteria, even on short time scales. Although redox cycling at interfaces can be somewhat
predictable, variations in response to biological and physical perturbations demonstrated wide differences in the dynamics
of redox-mediated processes. 相似文献
97.
Donald R. Demetrius Kaye L. Brubaker Stanley R. Davis 《Journal of the American Water Resources Association》2002,38(1):275-288
ABSTRACT: Design of bridges spanning tidal estuaries or bays requires an estimate of peak tidal flow. One common approach to estimating these flows (Neill's method) uses a first‐order approximation of uniform water surface rise in the water body. For larger water bodies, the assumptions of this method are decreasingly valid. This study develops a simple modification that accounts for the spatial variability in the response of tidal waterways to storm surge flows. The peak tidal flow predicted by Neill's equation is compared to the peak flow determined by numerical simulation of estuaries with simple geometries, ranging from 1 to 25 km in length, using the U.S. Army Corps of Engineers one‐dimensional unsteady flow model, UNET. Results indicate that, under certain conditions, it may be appropriate to apply a correction factor to the peak discharge and peak velocity predicted by Neill's method. An algorithm, developed by nonlinear regression, is presented for computing correction factors based on estuary length, shape, mean depth, and storm‐tide characteristics. The results should permit the design of more reliable, cost‐effective structures by providing more realistic estimates of the potential for bridge scour in tidal waterways, especially when a full solution of the unsteady flow equations is impractical. 相似文献
98.
Many marshes in the Gulf Coast Chenier Plain, USA, are managed through a combination of fall or winter burning and structural
marsh management (i.e., levees and water control structures; hereafter SMM). The goals of winter burning and SMM include improvement
of waterfowl and furbearer habitat, maintenance of historic isohaline lines, and creation and maintenance of emergent wetlands.
Although management practices are intended to influence the plant community, effects of these practices on primary productivity
have not been investigated. Marsh processes, such as vertical accretion and nutrient cycles, which depend on primary productivity
may be affected directly or indirectly by winter burning or SMM. We compared Chenier Plain plant community characteristics
(species composition and above- and belowground biomass) in experimentally burned and unburned control plots within impounded
and unimpounded marshes at 7 months (1996), 19 months (1997), and 31 months (1998) after burning. Burning and SMM did not
affect number of plant species or species composition in our experiment. For all three years combined, burned plots had higher
live above-ground biomass than did unburned plots. Total above-ground and dead above-ground biomasses were reduced in burned
plots for two and three years, respectively, compared to those in unburned control plots. During all three years, belowground
biomass was lower in impounded than in unimpounded marshes but did not differ between burn treatments. Our results clearly
indicate that current marsh management practices influence marsh primary productivity and may impact other marsh processes,
such as vertical accretion, that are dependent on organic matter accumulation and decay. 相似文献
99.
周期性的潮汐是滨海湿地重要的水文特征,为了探讨潮汐的半月周期(包括小潮期和大潮期)对土壤理化性质的影响及可能的机制,于2009年7月中下旬测定了长江口崇明东滩湿地土壤理化性质在小潮期和大潮期交替周期内的变化规律。结果表明,与小潮期相比,由于频繁的潮水淹没,大潮期0~5 cm土壤含水量的增加量从低潮滩向高潮位依次为:44.8%、18.5%、10.9%和14.3%,5~10 cm含水量的增加量从低潮滩向高潮位依次为:19.2%、9.8%、12.6%和16.2%,10~20 cm则依次为:5.6%、6.1%、2.5%和7.3%。大潮期,从低潮滩向高潮滩增加的盐度依次为0.18、0.13、0.10和0.09 ms·cm-1,增加的硫酸盐依次为0.32、0.21、0.16、0.13 mg·g-1。与小潮期相比,大潮期氧化还原电位(Eh)显著降低;土壤容重、pH、可溶性有机碳和可溶性氮在大小潮期间无明显差异。此外,在潮汐的半月周期内,低潮滩土壤比高潮滩有更高淹水频率和更长淹水时间,受潮水的影响更明显,大潮期低潮滩土壤含水量、盐度和硫酸盐的增加幅度大于高潮滩,低潮滩土壤Eh降低幅度则小于高潮滩。半月周期的潮汐可以显著影响滨海湿地的部分土壤理化性质,且不同潮位的土壤性质对潮汐的响应程度不同,进而可能会对湿地植物生长和相关生态过程起到重要的调控作用。 相似文献
100.
Elijah Ramsey III Amina Rangoonwala Terri Bannister 《Journal of the American Water Resources Association》2013,49(6):1239-1260
Satellite Synthetic Aperture Radar (SAR) was evaluated as a method to operationally monitor the occurrence and distribution of storm‐ and tidal‐related flooding of spatially extensive coastal marshes within the north‐central Gulf of Mexico. Maps representing the occurrence of marsh surface inundation were created from available Advanced Land Observation Satellite (ALOS) Phased Array type L‐Band SAR (PALSAR) (L‐band) (21 scenes with HH polarizations in Wide Beam [100 m]) data and Environmental Satellite (ENVISAT) Advanced SAR (ASAR) (C‐band) data (24 scenes with VV and HH polarizations in Wide Swath [150 m]) during 2006‐2009 covering 500 km of the Louisiana coastal zone. Mapping was primarily based on a decrease in backscatter between reference and target scenes, and as an extension of previous studies, the flood inundation mapping performance was assessed by the degree of correspondence between inundation mapping and inland water levels. Both PALSAR‐ and ASAR‐based mapping at times were based on suboptimal reference scenes; however, ASAR performance seemed more sensitive to reference‐scene quality and other types of scene variability. Related to water depth, PALSAR and ASAR mapping accuracies tended to be lower when water depths were shallow and increased as water levels decreased below or increased above the ground surface, but this pattern was more pronounced with ASAR. Overall, PALSAR‐based inundation accuracies averaged 84% (n = 160), while ASAR‐based mapping accuracies averaged 62% (n = 245). 相似文献