黄河口生态恢复工程对湿地土壤不同形态无机硫动态变化的影响

选择黄河口生态恢复前后的未恢复区（R₀）、2007年恢复区（R₂₀₀₇）和2002年恢复区（R₂₀₀₂）的芦苇湿地为研究对象，探讨了生态恢复工程对生长季湿地土壤无机硫形态变化的影响。结果表明，生态恢复工程不同程度地改变了湿地土壤中各形态无机硫含量。相对于R₀，R₂₀₀₂和R₂₀₀₇土壤中的水溶性硫（H₂O—S）含量分别降低46.7%和44.7%，吸附性硫（Adsorbed—S）和盐酸可溶性硫（HCl—Soluble—S）含量分别增加0.4%，116.0%和50.1%，29.1%，而盐酸挥发性硫（HCl—Volatile—S）含量在R₂₀₀₂下降8.0%，在R₂₀₀₇增加19.7%。不同恢复阶段湿地土壤中各形态无机硫含量在生长季呈不同的变化特征，这一方面与不同湿地植物生长节律以及地上与地下之间的硫养分供给关系密切相关；另一方面则与不同生态补水方式导致的环境因子，尤其是pH、EC和氮养分的变化有关。随着恢复年限的增加，湿地土壤的总无机硫（TIS）含量以及其占全硫（TS）含量的比例均呈降低趋势。湿地土壤的TIS储量整体随恢复年限的增加而降低，而这种降低主要取决于H₂O—S、Adsorbed—S和HCl—Soluble—S的贡献，且以H₂O—S占优（78%~80%）。研究发现，随着黄河口湿地的逐渐恢复以及每年冬季芦苇收割活动的进行，恢复湿地土壤中的无机硫养分逐渐趋于缺乏状态，长期来看将不利于维持湿地的稳定与健康。     

Rapid salinity changes affect the survival and physiology of a penaeid prawn: Implications of flood events on recruitment to the fishery

Estuaries act as nurseries for many penaeid prawns, but these habitats are highly susceptible to salinity decline through flooding. The rate of salinity decline and duration of exposure to non‐optimal salinity may affect survival and subsequent recruitment of prawns to the fishery. This study aimed to determine the effect of salinity fluctuations observed in local estuaries during flood events using a novel dilution approach. Mortality of juvenile Melicertus plebejus (Hess) was assessed after 24 hr exposure to 24 rates of salinity decline ranging from 0.01% to 20% per hr. After the salinity decline, prawns were held at the final salinities for five days before again assessing mortality as well as aerobic metabolic rate and prawn water content. Salinity decline from 36 to ~0.8 led to 50% mortality, but continued exposure to low salinity for five days increased mortality at this salinity to 99% and shifted the 50% mortality point to salinity ~5. Aerobic metabolic rate and water content data suggested the cause of mortality due to exposure to salinities < 5 was osmoregulatory failure. Rapid salinity declines over 24 hr and sustained low salinity due to flooding could compromise the survival of juvenile prawns, potentially reducing recruitment to the fishery.     

基于GAM的长江口鱼类资源时空分布及影响因素

根据2006至2017年长江口及其邻近海域鱼类资源调查,运用广义加性模型研究长江口鱼类资源密度与环境因子之间的关系,并对2017年鱼类资源密度的时空分布进行预测。结果显示,春夏秋冬四个季节最佳GAM偏差解释率分别为69.6%、55.9%、51.4%和47.4%,交叉验证回归线斜率的平均效应为0.62～0.88。盐度、水温和溶解氧是影响长江口鱼类资源密度的主要环境影响因子且在不同季节对鱼类资源密度有不同的影响机制。总体上,在春、夏、秋季,盐度与鱼类资源密度之间存在正向相关性;在夏、秋、冬季,水温对鱼类资源密度有显著影响,在秋季与鱼类资源密度之间存在正向相关性;在春、秋、冬季,溶解氧对鱼类资源密度有显著影响,在冬季与鱼类资源密度之间存在正向线性相关。研究表明,2017年夏季鱼类资源密度较高;在长江口南支的自然延伸水域存在鱼类资源密度的相对低值,在崇明岛向海自然延伸方向水域存在鱼类资源密度的相对高值。后续研究将对长江口鱼类资源进行不同生态类型区分,以期更加准确地掌握影响各生态类型鱼类时空分布的环境因素及其时空分布信息。     

Seasonal variation of inorganic nitrogen and net mineralization in a salt marsh ecosystem

Inorganic nitrogen pools and net mineralization were estimated in three sites of a Tagus estuary salt marsh in Portugal throughout 1 year. Ammonium (NH₄ ⁺) was the major form of inorganic nitrogen found in the salt marsh soil. Extractable NH₄ ⁺ concentrations showed a marked seasonal pattern with a concentration peak during the hotter months of July/August. The great majority (>99%) of the total nitrogen in the soil was found in sedimented organic matter, not readily available for plant uptake. Net nitrogen mineralization, determined using a field incubation method, showed a peak during the months of June/July which resulted in an increase on nitrogen availability. With the exception of the lower salt marsh, estimated rates of in situ net nitrogen mineralization in the soil during summer were well related to the increase in plant aboveground biomass and plant nitrogen pools, indicating that the process is an important source of available nitrogen for plant uptake and growth. Annual net nitrogen mineralization ranged between 2.4 and 4.5gNm^–2yr^{– 1} being significantly higher for the lower salt marsh site. Rates of net nitrogen mineralization were relatively low during most of the year with a particularly active period from June to August, possibly due to an effect of temperature on soil microbial activity.     

平面二维数模研究闸下淤积的缺陷

以姚江大闸和武障河闸为例，对河口水域建闸后的闸下淤积的机理进行了研究。通过应用二维悬沙模型的模拟计算，分析了数学模型在模拟近闸段的淤积时存在的缺陷，对产生问题的原因进行了初步探讨。由于闸下淤积问题存在明显的时空性和区域性特征，应积极研究解决措施。     

辽河三角洲湿地景观演变研究——以盘锦市为例

利用多时期的遥感数据和基于地理信息信息系统的景观格局研究方法,分析了辽河三角洲近30a来的景观演变规律。通过对比分析研究区4个时期的景观格局图(1976年、1989年、1998年、2004年),并计算主要景观类型的面积、斑块数、景观指数以及不同年代间的景观类型转移矩阵。结果表明:研究区近30a来景观类型并没有发生变化,景观格局的变化主要体现在主要景观类型的空间转化上,而且转化的速度和程度较大,其主要原因是人类活动和干扰,尤其是农业开发、油田开发以及城市化发展。     

Sedimentary characterization of Tagus estuarine beaches (Portugal)

Background, Aim and Scope  The distribution of sediments in estuarine beaches is controlled by the interactions between sediment supply, hydrodynamic processes and human intervention. The main purpose of this study is to characterize the sediments of Tagus estuarine beaches in order to understand their origin and to contribute to a better knowledge of the Tagus estuary sediment budget. Methods  Surface sediment samples were collected across beach profiles and sand grain size analysis was performed by dry sieving. Grain size statistics for the median (d₅₀) and standard deviation (SDM) were obtained using the Moment method. This study was complemented by a qualitative evaluation of the sediment composition. Cross-shore topographic surveys were conducted for selected sampling sites. Results  Tagus estuarine beach sediments are mainly composed of quartz sand particles which are fine-grained and well sorted near the mouth of the estuary and medium to coarse-grained and moderately sorted in the inner domain. Compositional results show evidence of active anthropogenic sediment sources, especially in the coarser fractions. Discussion  The analysis of the textural and compositional characteristics of beach sediments in the inner estuarine domain is compatible with local sedimentary sources, while a marine signature is present at the mouth and inlet channel sediments. In the inner domain, differences in the sedimentary processes are represented by the textural characteristics of the sediments, such as the sorting degree and the gravel content. Sediment characteristics also reflect human intervention in the system, with the introduction of anthropogenic and allochthonous particles and the mixture of sediments from different sources. Conclusions  The sediments of the inner Tagus estuarine beaches are derived from local Plio-Pleistocene outcrops while inlet and outer estuary beaches reveal a dominant marine source. Beach textural variability observed in the inner domain is not related to wave forcing gradients, but mainly to variations in the sedimentary processes along the estuarine margins and to human intervention. Results show that the Tagus estuarine beaches depended, almost exclusively, on sediment input from local sources until the last century. With increasing human occupation, sediment transfers became dominated by anthropogenically related activities mainly connected with the occupation of estuarine margins and dredging. Recommendations and Perspectives  Further studies should extend the present level of knowledge in what concerns sand transport patterns through additional compositional and geochemical analysis, and the development of new techniques in order to allow the quantitative evaluation of the impact of human activities on the sediment budget.     

珠江河口重金属镉的含量与分布的季节特征

对珠江河口水体、沉积物和生物体中重金属镉(Cd)的含量与分布进行调查研究,结果表明,水体中Cd含量范围在0.022～0.047 1 mg/L,并且Cd含量在时间上由高到低依次为:2月、5月、11月、8月,2月Cd含量显著高于5月、8月和11月(P＜0.05).以海水水质标准衡量,珠江河口水体2008年中大部分时间为海水二类水质.沉积物中Cd含量范围在5.062～9.239 mg/kg,平均含量为6.974 me/kg,并且沉积物中Cd含量均超过海洋沉积物3类标准.与国内外河口比较,珠江河口沉积物中Cd含量处在较高水平,污染比较严重,并且有逐年升高的趋势.生物体中Cd含量范围在0.144～0.430 mg/kg,鱼类Cd含量均超过国家水产品卫生标准,并且肉食性鱼类Cd含量略高于杂食性鱼类,但差异不显著(P＞0.05).与往年调查进行比较发现,珠江河口鱼类Cd含量2000年较1988年有大幅增加,并且2000年以后增加也比较明显.     

闽江河口区稻田土壤和植物的C、N、P含量及其生态化学计量比

选取闽江河口区稻田为研究区域,对土壤和植物的C、N、P含量及其生态化学计量比进行测定和分析。研究表明：土壤C、N、P元素的变化范围分别为5.72-13.41、0.47-0.82和0.33-0.89 mg.g-1,平均值分别为9.50、0.62和0.56 mg.g-1,其C与N、C与P、N与P的比值分别为12.18-16...     

基于多目标规划理论的辽宁双台河口湿地水资源合理配置研究

为了恢复湿地生态功能,合理确定湿地水资源开发利用方案,促进湿地的生态功能持续发展.根据辽宁双台河口湿地开发利用现状及规划目标,选取湿地天然生态环境需水量、农业灌溉及养殖需水量、生活用水量为3个目标,以湿地各类面积为决策变量,并以恢复到2000年的湿地各类面积值为约束条件,以系统工程的观点为指导,运用多目标规划理论,构建了湿地水资源合理分配的多目标规划模型,建立了3种配置方案进行比较.结果表明:只有优先满足湿地生态环境的需水量,使水资源得到合理有效的利用,才能使湿地得到较好较快的恢复,达到可持续发展的生态功能效果,对构建湿地系统生态恢复持续发展和水资源协调利用的框架模式具有重要的指导意义.