茅尾海营养盐污染控制对策研究

针对茅尾海营养盐污染的现状,通过海湾近10 年的富营养化状况变化趋势及污染来源分析,确定主要污染源,并根据环境容量计算结果,从陆源污染治理和养殖污染控制两方面,提出了海湾营养盐污染控制对策,为海湾水环境的可持续发展和海岸带综合管理提供科学依据和技术支持。结果表明：茅尾海富营养化状态总体呈上升趋势,并长期处于磷限制状态,入海河流和海水养殖是营养盐的主要来源。通过环境容量计算,在维持现有养殖水平的前提下,钦江和茅岭江总磷均需削减,削减率最高达67.4%;若养殖负荷削减30%,仅钦江仍需削减66%氨氮负荷和34.5%总磷负荷。因此,茅尾海营养盐污染控制应重点控制入海河流污染负荷和水产养殖规模。     

黄河口及邻近海域氮、磷及环境质量评价

根据2008年和2009年5、8月4个航次黄河口及邻近海域监测数据,分析了该海域氮磷含量和分布,与历史数据进行比较,分析年际动态变化、营养类型,并进行有机污染和营养状态评价。结果表明:整个黄河口及邻近海域氮营养水平较高,大部分海域磷酸盐营养水平较低,营养类型为磷限制潜在性富营养;整个监测海域处于中～富营养状态,春季(5月)富营养水平稍重于秋季(8月),河口近岸海域和南部海域富营养水平较重;2008年5月和2009年8月监测海域有机污染评价为开始受污染,2008年8月和2009年5月水质较好。     

四十里湾营养状况与浮游植物生态特征

研究了2006-2010年5月、8月和10月四十里湾的营养盐结构、海水营养级、有机污染状况、浮游植物数量及多样性变化特征,并对上述因子进行了相关性分析.结果表明,近5年N/P值先增加后降低,5月和8月海水多为贫营养和磷限制中度营养,而10月多呈磷限制潜在性富营养;除2006年和2007年10月水质分别达到轻度和中度污染外,其他时期基本未受有机污染,四十里湾有机污染状况有向好趋势.浮游植物多样性指数年际变化显示,总体呈先降低后增加的趋势,与其数量变化趋势相反.相关性分析显示,有机污染指数A与无机磷(IP)浓度呈显著正相关(P＜0.01),与DIN相关不显著(P＞0.05),这说明IP是影响四十里湾有机污染水平的首要因素;浮游植物多样性指数与其数量呈负相关,而与Si/P和IP浓度分别呈正相关(P＞0.05),浮游植物多样性指数与Si/P和IP的Pearson相关系数分别达到0.446和0.413.IP是四十里湾海水营养状况、有机污染及浮游植物多样性的主要影响因子之一.     

福建南日群岛秋季海洋生态环境诊断与评价

根据2007年9月和10月福建南日岛生态调查资料,从海水水质、海水营养结构与营养水平、生物多样性等3个方面诊断与评价了南日群岛海域环境现状,利用综合质量指数法对海洋生态环境质量进行综合评价,并探讨了不同评价指数的关系及合理性.结果表明:海域的pH、溶解氧(DO)、化学需氧量(COD)、Pb、Cd、Hg、As含量均符合第二类海水水质标准.71%站位的磷酸盐、14%站位的无机氮和7%站位的石油类污染物超第二类海水水质标准.海水水质总体属于较好等级,营养结构表现为氮限制,大部分海域处于富营养化状态,依据浮游生物的多样性指数评价结果为轻污染-清洁水平.生态环境综合质量指数评价结果表明南日群岛海域生态环境总体处于良好水平.利用不同的评价指数对海域环境健康状况进行诊断的结果存在一定差异.在实际评价中应综合运用化学指标和生物指标,才能得到相对客观的结论.     

广州海域潜在性富营养化特征研究

主要根据广州海洋资源环境监测中心的监测资料,运用一种反映营养盐限制特征的近海海水富营养化评价模式,对2003年广州海域富营养化水平特征进行了研究。结果表明,广州海域营养盐含量较高,无机氮浓度全年劣于国家海水水质四类标准(GB3097-1997),无机磷浓度在春夏季大部分处于三、四类水质标准之间,秋冬季则劣于国家海水水质四类标准;广州海域主要为磷限制潜在性富营养水平或磷中等限制潜在性富营养水平。同时,近二十年来,广州海域的无机磷、无机氮浓度的年平均值呈逐年增长趋势。     

苕溪流域非点源污染特征及其影响因子

应用土壤水体评价模型（SWAT）对苕溪流域径流量、泥沙、营养盐负荷进行模拟计算,分析了2008年苕溪流域非点源污染的时空分布特性.结果表明：苕溪流域非点源污染单位面积产生量表现为北部高于南部、东部高于西部、中部地区最少;耕地是泥沙和污染物产生的主要来源,其单位面积负荷远大于其他土地利用类型;产流量、产沙量与降水量呈显著正相关关系（P<0.05）,雨季(6-9月)的营养盐输出大于旱季(12月至次年3月);平均坡度与泥沙负荷、有机氮负荷及硝态氮负荷呈显著相关关系（P<0.05）.     

舟山附近海域富营养化的时空分布及其与环境因子的关系

根据2008年春季(5月)和夏季(8月)在舟山附近海域调查监测资料,采用改良后的营养指数法,结合N/P(物质的量比)潜在性富营养化法,对该海域在春季和夏季的富营养化水平进行了评价,并分析了该海域富营养化的时空分布特征,对富营养化指数与环境因子的相关关系进行了讨论,同时对两种方法的结果进行了比较分析.营养指数法计算结果显示:舟山附近海域的富营养化程度较低,各调查站位富营养化指数均小于富营养化阀值;春季的富营养化水平高于夏季;春季、夏季富营养化指数的平面分布均表现出沿岸到离岸方向呈逐渐降低的特点;春季调查海域N/P平均值为17.35,略高于Redfield系数,夏季N/P平均值为56.34,具有明显的营养盐比例不平衡的特征.潜在性富营养化法计算结果显示:春季属于富营养水平,夏季属于磷限制潜在性富营养;富营养化指数与盐度、溶解氧、pH相关性均不显著,调查海域富营养化水平的时空变化主要受地表径流冲谈水、浮游植物、外海海流等的共同影响.     

海河流域水体沉积物碳、氮、磷分布与污染评价

从全流域尺度上研究海河流域水体沉积物碳、氮、磷元素含量与分布特征,对研究海河流域水环境污染现状具有重要意义.本研究采集海河流域河流与水库163个表层沉积物(0～10 cm)样品,测定沉积物有机碳(TOC)、总氮(TN)、总磷(TP)的含量,运用有机指数与有机氮方法评价沉积物污染状况.结果表明: 海河流域沉积物TOC、TN、TP含量具有较大的空间异质性,下游平原区明显高于山区,北四河下游平原、黑龙港及运东平原含量较高,永定河山区、北三河山区、滦河流域含量相对较低,河流沉积物TOC含量显著高于水库沉积物,而TN、TP含量与水库沉积物没有显著差异.TN与TOC、TP含量呈显著正相关(r=0.704,P<0.01;r=0.250,P<0.01).全流域有机指数总体属于“较清洁”水平,北四河下游平原总体已接近有机污染水平.全流域有机氮总体处在“尚清洁”水平,北四河下游平原、黑龙港及运东平原流域存在有机氮污染.海河流域河流、水库沉积物具有相似的污染强度.沉积物C/N平均值为12.71,表明TOC多来源于藻类等浮游动植物,其次是高等植物,水库C/N值比河流高,陆源物质输入对水库沉积物TOC的贡献比对河流大.     

中国主要入海河流河口集水区划分与分类

采用GIS技术开展中国主要入海河流的流域边界及其汇水单元、河口集水区的划分及其分类。基于ArcGIS水文分析模块划分出15条入海河流的汇水单元,并通过5种不同汇水单元面积等级的划分来表达各入海河流汇水单元的详细程度;划分的流域面积与相关文献资料对比偏差在10%以内;在流域与汇水单元划分的基础上,基于感潮河段的数据收集,确定出88个中国主要入海河流的河口集水区。通过建立分类指标体系,采用聚类分析方法,划分出5类河口:第一类EDA主要分布在环渤海地区、山东半岛和广东沿海;第二类EDA主要分布在长江口和杭州湾周围;第三类EDA主要分布在江苏北部沿海和辽东半岛;第四类包括山东江苏交界处沿海、江苏南部沿海;第五类主要分布在福建浙江沿海、珠江口、长江口、海河口附近、辽河河口附近,并利用快速生物评价法验证河口分类的合理性。研究成果可为进一步开展我国近海河口和海域营养盐基准制订与生态分区提供基础空间数据与方法借鉴。     

启东海域水质营养状况及其与陆域农村水环境质量的关系

根据启东近岸海域2003—2009年7个站点的监测数据,研究了该海域的水质营养状况,并初步分析了与相邻陆域农村水环境质量的关系。结果表明:除平台站点之外,多数站点的COD、DIN、DIP和DO有增加的趋势;仅平台站点在2003年未富营养化,其他6站点都处于富营养状态,在2007年富营养化指数达到最高值,其后逐年显著降低;2003—2009年重污染海域比例达到4.1%,在2007和2008年是污染较为严重的年份;富营养化指数与综合标准指数之间存在显著的正线性相关;相对于城市工业生产生活排放,启东近岸陆域农村水环境质量变化和长江径流对近岸水质营养状况的影响较小。     

Influence of anthropogenic activities on water quality of a tropical stream ecosystem

Water samples were collected from three sites located in the middle reach of the Njoro River, Kenya, and analysed for total phosphorus (TP), orthophosphate, ammonia‐nitrogen, and nitrate‐nitrogen to evaluate stressor sources (e.g. factories and wastewater ponds) and the general stream water quality. The stream surface water was also analysed for biochemical oxygen demand (BOD₅) to provide an overview of organic matter loading. Mugo, Egerton Bridge and the canning factory sites of the Njoro River had low water quality which is likely to be due to poor farming, partially treated effluents and poor provision of sanitation facilities to the riparian communities. The concentrations of the selected nutrients did not differ significantly among the three sites, presumably due to pollution of the whole stream reach by the catchment nutrient sources. High phosphate concentrations (i.e. ～0.76 mgPO₄ l^?1 and ～0.87 mgTP l^?1) at Canning Factory were recorded during the low flow dry season. Nitrate‐nitrogen concentrations varied significantly with water discharge which explained between 63 and 87% of the nutrient variability in the three sites. BOD₅ differed significantly among the three sites, with historical effects of wastewater and factory effluent discharge being reflected in the results of Egerton Bridge and Canning Factory. The concentrations of ammonia‐nitrogen, TP and orthophosphate were higher in the wastewater than in the river water whereas nitrate‐nitrogen was lower. This study indicates that the Njoro River is stressed by nutrients from the activities within its catchment. With the increasing population, the nutrient load to the river will continue to increase and the water quality will continue to deteriorate. Reductions of nutrient loads into the river as well as provision of sanitation facilities to the riparian communities are needed to control further water degradation.     

基于氮磷比解析太湖苕溪水体营养现状及应对策略

生态化学计量学是评价水体营养状态的重要手段,利用其氮磷比指标探讨了我国太湖主要入湖河流苕溪的营养状态。野外监测结果显示,苕溪水体氮素超标严重,磷素污染轻度,硝酸盐、颗粒态磷为氮磷的主要赋存形态,且氮磷浓度呈现相似的季节变化规律,表明苕溪主要受农业面源污染影响。氮磷比分析表明,苕溪水体春、秋季处于磷素限制状态,夏季适合藻类生长,冬季低温条件下不利于藻类的大量繁殖;苕溪生物量增长受磷素限制,线性拟合亦显示其氮磷比主要受磷素波动的调控;苕溪干流大面积暴发蓝藻水华的风险较部分支流及死水区低,苕溪水入湖后,特别是夏季其暴发风险将显著提高。针对苕溪水体的富营养化现状,提出若干条水质改善应对策略。     

Primary nutrients and the biotic integrity of rivers and streams

1. Controls to reduce loadings of primary nutrients to maintain biotic integrity in rivers and streams have not been widely implemented because the relation between nutrients and chlorophyll, and its consequences for higher trophic levels, is confounded in lotic ecosystems by their openness, the variable degree of nutrient limitation and by the effect of physical factors.
2. The relationship between primary nutrients and biotic integrity in rivers and streams was tested using biological, physical and chemical information collected since 1982 from similar locations in streams throughout Ohio using standard procedures.
3. There was a negative correlation between nutrients, especially total phosphorus, and biotic integrity. The deleterious effect of increasing nutrient concentration on fish communities in low order streams was detectable when nutrient concentrations exceeded background conditions (total inorganic nitrogen and phosphorus > 0.61 mg L^–1 and 0.06 mg L^–1, respectively).
4. These results suggest that the control of release of toxins and oxygen‐demanding wastes to rivers is insufficient to protect aquatic life, and confirm the importance of non‐point sources of pollution in catchment planning as well as the combined effect of habitat and riparian quality on nutrient assimilation.     

Composition of inorganic and organic nutrient sources influences phytoplankton community structure in the New River Estuary, North Carolina

The New River Estuary, NC, is a nutrient-sensitive, eutrophic water body that is prone to harmful algal blooms. High annual loading from the watershed of varying nutrient forms, including inorganic phosphorus and inorganic and organic nitrogen, may be linked to the persistence of algal blooms in the estuary. In order to evaluate phytoplankton response to nutrient inputs, a series of in situ nutrient addition experiments were carried out during June 2010 to July 2011 on water from an estuarine site known to support algal blooms. Estuarine water was enriched with nutrients consisting of individual and combined sources of dissolved inorganic nitrogen, orthophosphate, urea, and a natural dissolved organic nitrogen (DON) addition derived from upstream New River water. The combined inorganic N and P addition most frequently stimulated phytoplankton biomass production as total chlorophyll a. The responses of diagnostic (of major algal groups) photopigments were also evaluated. Significant increases in peridinin (dinoflagellates), chlorophyll b (chlorophytes), and myxoxanthophyll (cyanobacteria) were most frequently promoted by additions containing riverine DON. Significant increases in zeaxanthin (cyanobacteria) were more frequently promoted by inorganic nitrogen additions, while increases in fucoxanthin (diatoms) and alloxanthin (cryptophytes) were not promoted consistently by any one nutrient treatment. Evaluating the impact of varying nutrient forms on phytoplankton community dynamics is necessary in order to develop strategies to avoid long-term changes in community structure and larger-scale changes in ecosystem condition.     

不同林窗马尾松凋落叶与土壤养分变化研究

以现有42年生的马尾松（Pinus massoniana）人工纯林,经过采伐形成4种不同大小有效面积的林窗（100、400、900和1 600 m²）为研究对象,以未经采伐的42年生马尾松人工纯林为对照样地,采用凋落叶分解袋法,研究不同大小有效面积林窗对马尾松凋落叶、土壤C、N、P及化学计量比和养分损失率的影响。研究结果表明：（1）不同大小有效面积林窗下的马尾松凋落叶、土壤C、N、P含量及养分损失率除土壤P含量和马尾松凋落叶P养分损失率外,均存在显著差异。随着林窗有效面积G1~G4的增大,马尾松凋落叶C、N、P含量均呈降低趋势,三者均在G3林窗体现出较小值。马尾松凋落叶C、N、P养分损失率、土壤C、N、P养分含量多呈抛物线趋势,且均在G2或G3林窗体现出最大值。（2）不同大小有效面积林窗下的马尾松凋落叶、土壤C/N/P均存在显著差异。随着林窗有效面积G1~G4的增大,马尾松人工林土壤C/N/P基本呈抛物线变化趋势,土壤C/N在G3林窗出现最大值,土壤C/P、N/P均在G2林窗体现出最大值;土壤C/N、C/P、N/P变异系数分别为13.31%、16.51%、17.21%。马尾松凋落叶C/N、C/P均在G3体现出最小值。（3）马尾松凋落叶C、N含量与土壤C、C/N/P及环境因子的相关性较强,P含量与它们的相关性较弱;C/N与土壤P、C/N/P及环境因子的相关性较强,C/P、N/P与土壤C/P及环境因子的相关性较强;C、N养分损失率与土壤C、C/N、C/P及环境因子的相关性较强,P养分损失率与土壤C、N、P含量及其化学计量比和环境因子的相关性较弱。土壤C、N、P含量及其化学计量比与环境因子的相关性较强。     

白洋淀水陆交错带对陆源营养物质的截留作用初步研究

在白洋淀进行的野外实验结果表明水陆交错带中的芦苇群落和群落间的小沟都能有效地截留来自府河的陆源营养物质,其中,在植被２９０ｍ长的小沟对地表径流总Ｎ和总Ｐ的截留分别为４２和６５％;４ｍ芦苇根区土壤对地表下径流总Ｎ和总Ｐ的截留率分别为６４和９２％。被截留比率最大的是无机态的正磷酸根态磷和铵态氮。     

Changes of nitrogen and phosphorus loads to European seas

During the last decades human activity has altered the natural cycle of nitrogen and phosphorus on a global scale, producing significant emissions to waters. In Europe, the amount of nutrients discharged from rivers to coastal waters as well as the effects of mitigation measures in place are known only partially, with no consistent temporal and spatial cover. In this study, we quantify the loads and concentration of nitrogen and phosphorus discharged in the European seas over the period 1985–2005, and we discuss their impact on coastal ecosystems. To support our analysis, a catchment database covering the whole of Europe was developed together with data layers of nutrients diffuse and point sources, and the statistical model green was used to estimate the annual loads of nitrogen and phosphorus discharged in all European seas. The results of this study show that during the last 20 years, Europe has discharged 4.1–4.8 Tg yr^?1 of nitrogen and 0.2–0.3 Tg yr^?1 of phosphorus to its coastal waters. We show that beside the North Sea and part of the Baltic Sea, annual nutrient exports have not changed significantly, in spite of the implementation of measures to reduce nutrient sources, and that the N : P ratio has increased steadily, especially in the North, Mediterranean and Atlantic seas. The response of river basins to changes in inputs was not linear, but influenced by climatic variations and nutrients previously accumulated in soils and aquifers. An analysis of the effects of European environmental policies shows that measures to reduce phosphorus were more successful that those tackling nitrogen and that policies aimed at point sources were more effective or more effectively implemented than those controlling pollution from diffuse sources. The increase of the N : P ratio could fuel eutrophication in N‐limited coastal ecosystems, reducing biodiversity and the ecosystem's resilience to future additional anthropogenic stress, such as climate change.     

黄土丘陵沟壑区退耕地土壤养分因子对植被恢复的贡献

为了探求各土壤养分因子对植被恢复贡献的大小．利用因子分析(Factor analysis)对黄土高原丘陵沟壑区退耕地植被恢复中的土壤养分进行了多元统计分析,定量研究了土壤养分环境对植被恢复的作用。结果表明：住所选取的6个土壤养分因子中,土壤有机质、有效N、全P和速效P对植被恢复的贡献较大．是限制该地区植被恢复的主导因素,其它养分因子的贡献相对较小。根据土壤养分因子间的相关系数,土壤有机质与全N和有效N呈显著相关。因此,在评价土壤养分因子对植被恢复贡献大小时．选取土壤有机质、氮和磷的含量作为评价指标,不但节省了时间和财力,而且有助于植被恢复的快速评价。     

中小型土壤动物组成对复垦铜尾地土壤养分的影响

通过盆钵生物试验研究了中小型土壤动物不同类群的组成对复垦铜尾矿废弃地土壤养分的影响。整个培养试验根据需求对不同中小型土壤动物组合设置四个处理措施,每种措施分为有无凋落物两种水平,即:(1)无土壤动物(Re),无土壤动物+凋落物(Re+Li)(2)跳虫(Co),跳虫+凋落物(Co+Li)(3)跳虫+蜱螨类(Co+Ac),跳虫+蜱螨类+凋落物(Co+Ac+Li)(4)中小型土壤动物(剔除大型土壤动物Me),中小型土壤动物+凋落物(Me+Li)。另设一组对照(CK)处理,并于培养实验开始前完成测定,作为本底值。分析表明,土壤p H随着中小型土壤动物类群的增加而降低,最低值出现在Me和Me+Li处理,且二者之间无显著性差异;对照(CK)处理下的各养分含量均显著低于其他各处理,各处理中有机质、有效磷和水解性氮的含量的最大值均出现Me+Li处理,且与其他各处理呈极显著差异(P0.01);土壤全磷含量最大值出现在Re和Me+Li处理,最低值出现在Co+Li处理且之间呈显著差异(P0.05);土壤全氮含量最大值出现在Co+Ac和Me+Li处理,最低值出现在Co+Ac+Li处理且彼此间也呈显著差异(P0.05)。相关分析表明,有机质与有效磷以及全氮与水解性氮之间相关性达到极显著正相关关系(r=0.886,r=0.898),有机质与全氮及水解性氮分别呈现显著正相关关系(r=0.735,r=0.780),全氮与有效磷(r=0.782)以及有效磷与水解性氮(r=0.755)也呈现显著正相关关系。p H与有机质呈现显著负相关关系(r=-0.782),全磷与有机质、全氮、有效磷、水解性氮均无相关关系。     

Nutrient limitation of phytoplankton in solar salt ponds in Shark Bay,Western Australia

The aim of this research was to examine nutrient limitation of phytoplankton in solar salt ponds of varying salinity at Useless Inlet in Western Australia. These ponds use solar energy to evaporate seawater for the purpose of commercial salt production. A combination of techniques involving water column nutrient ratios, comparisons of nutrient concentrations to concentration of magnesium ions and bioassays were used in the investigation. Comparisons of changes in dissolved inorganic nitrogen to phosphorus ratios and concentrations of dissolved inorganic nutrients against changes in concentrations of the conservative cation Mg²⁺ indicated that phytoplankton biomass was potentially nitrogen limited along the entire pond salinity gradient. Nutrient addition bioassays indicated that in low salinity ponds, phytoplankton was nitrogen limited but in high salinity ponds, phosphorus limited. This may be due to isolation of phytoplankton in bioassay bottles from in situ conditions as well as to changes in phytoplankton species composition between ponds, and the variable availability of inorganic and organic nutrient sources. The differences in limiting nutrient between methods indicate that phytoplankton cells may be proximally limited by nutrients that are not theoretically limiting at the pond scale. Dissolved organic nutrients constituted a large proportion of total nutrients, with concentrations increasing through the pond sequence of increasing salinity. From the change in nutrient concentrations in bioassay bottles, sufficient dissolved organic nitrogen may be available for phytoplankton uptake in low salinity ponds, potentially alleviating the dissolved inorganic nitrogen limitation of phytoplankton biomass. Guest Editors: J. John & B. Timms Salt Lake Research: Biodiversity and Conservation—Selected Papers from the 9th Conference of the International Society for Salt Lake Research