不同风浪条件下太湖梅梁湾光合有效辐射的衰减

基于2003年7月12～17日在太湖梅梁湾进行的连续6d原位水下光场观测资料,分析了不同风浪条件下光合有效辐射(PAR)的衰减和真光层深度,探讨了影响水下光合有效辐射的主导因子.结果表明,整个观测期间向下PAR衰减系数为2.63～4.71·m^-1(均值为3.63±0.47·m^-1),对应的真光层深度为0.98～1.75m(均值为1.29±0.18m),显示1.5m以下深度浮游植物、沉水植物基本上无法获取足够的太阳光能进行光合作用.从小风浪到中风浪、大风浪向下PAR衰减系数分别是2.63、3.72和4.37·m^-1,衰减系数分别增加了41%、66%.透明度、PAR衰减系数、真光层深度与悬浮物浓度存在显著性线性相关,并且与悬浮物中无机颗粒物相关性最好,而与叶绿素a、脱镁叶绿素及溶解性有机碳相关性很低.多元逐步线性回归表明,叶绿素a和溶解性有机碳最先被剔除方程,说明在梅梁湾由于风浪扰动引起悬浮物浓度的改变是影响水下光场的主导因素.     

抚仙湖叶绿素a的生态分布特征

2001年5月、8月和9月,对云南抚仙湖水体、沉积物、沉积物与水界面的叶绿素a,浮游植物的优势种类、细胞密度的分布和时空变化及其与环境因子的关系进行了研究。采用分光光度法测定叶绿素a浓度。结果表明,水体叶绿素a浓度的分布存在着明显的季节变化,真光层中的动态变化尤其显著,且光照强度对水体中叶绿素a浓度的分布起主导作用。在观测的3个不同季节中,表层叶绿素a浓度,秋季最高,平均为(2.27±0.12)μg/dm3;春季次之,为(1.85±0.20)μg/dm3;夏季最低,为(1.38±0.15)μg/dm3。分析水体中营养元素的分布特征及其与叶绿素a之间的关系,表明磷是抚仙湖浮游植物生长的主要限制因子。沉积物叶绿素a浓度的垂直分布存在明显差异,其浓度在表层和次表层较高,并随沉积深度的增加而降低;浮游植物的分析表明,硅藻门的小环藻是抚仙湖沉积物中叶绿素a的主要来源。而上覆水中叶绿素a浓度与真光层叶绿素a浓度相当的原因,则可能是由水底微型藻类的再悬浮和浮游植物的沉降聚集而导致的。     

獐子岛海域冬季分级叶绿素a的分布特征及其影响因素

于2016年1月对獐子岛海域进行了航次调查,研究了獐子岛海域浮游植物粒级结构的空间分布特征及其环境影响因素。结果表明:冬季表层总叶绿素a、小型(20μm)、微型(2~20μm)和微微型(0.45~2μm)浮游植物叶绿素a浓度的范围分别为0.24~0.92、0.15~0.58、0.09~0.46、0~0.03μg·L-1,平均叶绿素a的浓度分别为0.69、0.36、0.33、0.002μg·L-1,小型、微型和微微型浮游植物对浮游植物总量的贡献率分别为51.72%、48.01%、0.26%;底层总叶绿素a、小型、微型和微微型浮游植物叶绿素a浓度的范围分别为0.29~1.77、0.12~1.45、0.17~0.50、0μg·L-1,平均叶绿素a的浓度分别为0.78、0.43、0.34、0μg·L-1,小型、微型和微微型浮游植物对浮游植物总量的贡献率分别为52.97%、47.03%、0;从垂直分布上来看,表、底层总叶绿素a及两种粒级浮游植物(20μm、2~20μm)的浓度均差异不显著,分布较为均匀;从水平分布上来看,总叶绿素a及两种粒级浮游植物(20μm、2~20μm)浓度的表、底层空间分布趋势相近,均呈现出由獐子岛海域西北部向南部逐渐降低的趋势。RDA分析表明,温度、盐度、溶解氧、颗粒态有机物、NO2--N和NH4+-N是影响獐子岛海域冬季浮游植物粒级结构变动的重要因素。     

太湖水体叶绿素a含量与氮磷浓度的关系

基于太湖水体1993—2002年5—9月监测资料,进行了叶绿素a含量与总氮(TN)、总磷(TP)浓度关系的分区统计分析,探讨了太湖藻类生长的TN、TP适宜浓度。结果表明:太湖叶绿素a含量与TN、TP浓度的关系存在显著的空间差异;在梅梁湾和西北区,当TN、TP浓度较低时,叶绿素a含量与TN、TP浓度呈正相关;当TN、TP浓度较高时(梅梁湾TN、TP浓度分别超过5.4和0.31mg.L-1;西北区分别超过4.5和0.27mg.L-1),叶绿素a含量与TN、TP浓度呈负相关;在湖心区和贡湖区,叶绿素a含量与TN、TP浓度呈正相关,尤其当TP浓度超过0.1mg.L-1时,叶绿素a含量随TP浓度增加而上升;在东太湖和湖东滨岸区,随TN、TP浓度的升高,叶绿素a含量变化较小;在西南区,叶绿素a含量与TN浓度无显著相关关系,与TP浓度呈正相关;太湖藻类生长的适宜浓度是TN<5.4mg.L-1,TP为0.1～0.31mg.L-1。     

太湖梅梁湾沿岸带水体生物学与光学特性

基于 1998～ 1999年周年 4季原位水下光场观测资料及中国科学院太湖湖泊生态系统研究站 1992～ 2 0 0 1年悬浮物、叶绿素 a、透明度长期历史观测资料分析了太湖梅梁湾沿岸带第 2号站点水体的生物学与光学特性 ,探讨了水下光合有效辐射(PAR)总量的日变化、垂直分布 ;光衰减系数的季节变化及光谱分布 ;影响光衰减系数的主要水色因子。结果表明 ,无论是 PAR还是光谱衰减系数其值都很高 ,其中 PAR衰减系数在 1.4 0～ 5 .30 / m间变化 ,均值为 2 .4 3± 0 .5 5 / m,秋季最大、夏季最小 ,真光层深度在 0 .87～ 3.2 9m间变化 ,均值为 1.98± 0 .4 1m;水下光谱在蓝光波段衰减最强烈 ,其次是红光、绿光 ,随着深度增加光谱成分出现绿移和红移现象 ,绿红光占得比例越来越大 ;光谱衰减系数随着波长的增加大致呈下降趋势 ,但在 6 70 nm附近有个峰值 ;基于线性相关分析发现在混浊的沿岸带水体中影响光衰减主要因子为水体中的悬浮物和有色可溶性有机物 ,叶绿素 a对 PAR衰减系数的贡献率只占到 1.5 9%～ 14 .2 1%。     

风场对太湖叶绿素a空间分布的影响

叶绿素a的浓度是水环境评价的重要参数。根据2005—2009年太湖全湖32个采样点的20次太湖采样数据,结合气象要素资料模拟的太湖风场,探求了风场对太湖叶绿素a空间分布的影响。结果表明:叶绿素a浓度的高值中心位于太湖西北侧、竺山湾以及梅梁湾流域,而太湖东南部的叶绿素a浓度较低;全太湖全年以东南风为主,南部风速较大,北部风速较弱;风场对叶绿素a的输移作用明显,在风场作用下,叶绿素向太湖西北部和北部输移,造成了该地区太湖流域叶绿素浓度普遍偏高。     

2006年夏季南黄海浮游植物叶绿素a分布特征及其环境调控机制

根据2006年夏季南黄海生态调查资料,分析了浮游植物现存量(叶绿素a)的空间分布特征及其主要环境调控机制.结果表明:南黄海浮游植物叶绿素a浓度范围为0.07～12.17 mg/m3,平均值为1.42 mg/m3;浮游植物叶绿素a平面分布呈近岸混合区高于外海层化区的特征,总体上随水体盐度和营养盐梯度的变化而变化,其中浅海陆架锋区对浮游植物有明显的聚集作用,垂直结构中层化区叶绿素次表层最大值现象明显,且最大值的深度和量值具有明显的区域差异;叶绿素a浓度与主要环境因子的相关性分析表明,在较大空间尺度上营养盐是浮游植物的主要调控因子,温度、光照和浮游动物摄食等也在一定空间和程度上对浮游植物的生长产生影响.     

太湖典型草、藻型湖区紫外辐射的衰减及影响因素分析

2004年4月通过野外原位观测和实验室测定相结合的方法对东太湖和梅梁湾典型草、藻型湖区紫外辐射光谱衰减及影响因素进行了研究。结果表明,320nm(UV-B)、380nm(UV-A)的衰减系数在6.33~19.59m-1、3.41~13.64m-1间变化,对应的1%表面光强穿透深度分别为0.24~0.73m、0.35~1.35m,到达湖面的99%UV-B辐射在0.5m左右表层水就衰减完毕,东太湖和梅梁湾紫外辐射衰减系数存在明显的湖区差异;溶解性有机碳(DOC)的浓度在6.60~17.17mg/L间变化,其均值为(9.99±2.48)mg/L;375nm波长处CDOM吸收系数为1.78~6.25m-1,均值为(3.70±1.10)m-1;在短波部分CDOM吸收与DOC浓度存在显著性相关,相关性大致随波长降低而增加,320nm处的线性关系式:ad320=0.885DOC 2.182;紫外辐射衰减主要受制于水体中的CDOM浓度,衰减系数与DOC浓度、CDOM吸收系数存在显著性相关,340nm处的关系式分别为:Kd340=0.82 1.05DOC、Kd340=1.98 1.49ad340。在太湖紫外辐射衰减还要受悬浮物和叶绿素a浓度的影响,衰减系数与DOC、叶绿素a和悬浮物浓度多元回归的结果明显要高于单独与DOC浓度或CDOM吸收系数的回归结果。     

印度洋南赤道流区水体叶绿素a的分布及粒级结构

根据2010年4—5月印度洋南赤道流区的综合环境调查资料,对印度洋南赤道流区叶绿素a浓度分布和浮游植物的粒级结构等进行了分析. 结果表明,调查海区水体层化明显,表层水温较高,营养盐浓度较低。调查海区东部测站的数据显示该区域可能受到来自印度尼西亚贯穿流和南爪哇流的影响,有高温低盐的特点。叶绿素a浓度在该海区的分布具有以下特点：（1）表层叶绿素a浓度在整个调查海区虽然普遍较低（平均为（0.1220.052） mg/m3）,但具有明显的空间区域化特征：印度洋南赤道流区中部,叶绿素a浓度较低,站位间分布均匀;东部叶绿素a浓度相对较高,不同测站叶绿素a浓度差异明显.（2）整个调查区域叶绿素a浓度垂直分布具有明显的单峰结构,其最大值分布在60—80m水层,位于营养盐跃层内.（3）叶绿素a的粒级结构分析结果显示,pico级份的浮游植物对叶绿素a的贡献占主导地位,平均为75%,nano级份的贡献平均为20%,net级份对叶绿素a的贡献最小,平均仅有5%. 对比本次调查和在其它海区的研究,表明印度洋南赤道流区属于典型的低纬度寡营养海区,低的营养盐浓度（特别是NO3-浓度）是该海区浮游植物生长的主要限制因素之一.     

香溪河官庄坪库湾叶绿素a 及初级生产力的分布特征

2005年2月—4月对三峡库区香溪河进行了定点初级生产力及相关影响因子的研究,分析了官庄坪库湾叶绿素a含量和初级生产力的时空分布特征。结果表明,叶绿素a含量、初级生产力在各水层的变化具有相同的周期性,均存在5个峰值,平均每个周期为7—10d左右,但两者不同步。官庄坪测站的真光层深度为10m左右,介于湖泊与海洋之间,光补偿点为4—5m。初级生产力最大值出现在水下0.5m处,并沿物理深度逐渐降低;叶绿素a含量最大值则出现在水下2m处。水温的垂直变化在后期差异明显,各水层日平均水温增量(ΔT/d)与平均毛初级生产、净初级生产存在极显著的相关性。     

基于GOCI影像的湖泊悬浮物浓度分类反演

悬浮物直接影响到光在水体中的传播,进而影响着水生生态环境,最终决定了湖泊的初级生产力。传统的遥感反演估算模型大多是针对某一湖区进行统一建模,忽视了不同区域水体光学性质的复杂差异性,并且传统的传感器时间分辨率和空间分辨率受到一定限制。针对太湖、巢湖、滇池、洞庭湖4个湖区利用两步聚类法将高光谱模拟到GOCI影像上的波段进行分类,将水体类型分为三类,第一类水体为悬浮物主导的水体,第二类水体为悬浮物和叶绿素a共同主导的水体,第三类水体为叶绿素a主导的水体。针对不同类型水体的光学特征,分别构建了悬浮物浓度反演模型,结果表明第一类水体可以利用B7/B4,第二和第三类水体可以利用B7/(B8+B4)作为波段组合因子对悬浮物浓度进行模型构建。精度验证结果表明,分类建模后第一类和第三类水体悬浮物浓度估算精度都得到了较明显提高,第一类水体RMSE降低了9.19mg/L,MAPE降低了3%,第三类水体RMSE降低了5.63 mg/L,MAPE降低了13.97%,第二类水体精度稍有降低。最后将反演模型应用于2013年5月13日的GOCI影像,可知整体而言太湖西南部地区悬浮物浓度较高,东北部地区悬浮物浓度较低,并且从9:00到15:00,太湖南部悬浮物浓度较高的区域在逐渐缩小。     

Oil pollution status expressed as the fraction of dissolved and dispersed petroleum hydrocarbons

Four coastal ecosystems with contrasting characteristics were sampled in Costa Rica (2000-2002). Oil pollution status, expressed as the fraction of dissolved/dispersed petroleum hydrocarbons related to chrysene equivalents, was determined by the molecular fluorescence analytical technique. A total of 130 water samples were taken, from the Caribbean (Moín Bay), and from the Pacific (Bahía Culebra, Gulf of Nicoya and Dulce Gulf). On one occasion, seven samples along the Puntarenas estuary were also analysed. In Moín the mean and standard deviation were 0.10 microg x L(-1) +/- 0.18 micro x L(-1), ranging from non detectable (nd) to 0.65 microg x L(-1). For the Pacific ecosystems the total range was from nd to 0.37 microg x L(-1). In Bahia Culebra no fluorescence signals were obtained. In the Gulf of Nicoya the mean and standard deviation were 0.04 microg x L(-1) +/- 0.09 microg x L(-1), from nd to 0.33 microg x L(-1). Values in Dulce Gulf were 0.05 microg x L(-1) +/- 0.11 microg x L(-1), from nd to 0.37 microg x L(-1). Along the Puntarenas estuary the range was 0.17 to 5.91 microg x L(-1), with a mean of 1.21 microg x L(-1) and a standard deviation of +/- 2.10 microg x L(-1). The four coastal ecosystems had concentrations below the 10 microg x L(-1) limit for polluted oceanic areas. The Puntarenas estuary reflects the influence of antropogenic activities from and around the City of Puntarenas. These levels are considered low for inshore waters.     

Lake Topography and Wind Waves Determining Seasonal-Spatial Dynamics of Total Suspended Matter in Turbid Lake Taihu,China: Assessment Using Long-Term High-Resolution MERIS Data

Multiple comprehensive in situ bio-optical investigations were conducted from 2005 to 2010 and covered a large variability of total suspended matter (TSM) in Lake Taihu to calibrate and validate a TSM concentration estimation model based on Medium Resolution Imaging Spectrometer (MERIS) data. The estimation model of the TSM concentration in Lake Taihu was developed using top-of-atmosphere (TOA) radiance of MERIS image data at band 9 in combination with a regional empirical atmospheric correction model, which was strongly correlated with the in situ TSM concentration (r ² = 0.720, p<0.001, and n = 73). The relative root mean square error (RRMSE) and mean relative error (MRE) were 36.9% and 31.6%, respectively, based on an independent validation dataset that produced reliable estimations of the TSM concentration. The developed algorithm was applied to 50 MERIS images from 2003 to 2011 to obtain a high spatial and temporal heterogeneity of TSM concentrations in Lake Taihu. Seasonally, the highest and lowest TSM concentrations were found in spring and autumn, respectively. Spatially, TSM concentrations were high in the southern part and center of the lake and low in Xukou Bay, East Lake Taihu. The lake topography, including the water depth and distance from the shore, had a significant effect on the TSM spatial distribution. A significant correlation was found between the daily average wind speed and TSM concentration (r ² = 0.685, p<0.001, and n = 50), suggesting a critical role of wind speed in the TSM variations in Lake Taihu. In addition, a low TSM concentration was linked to the appearance of submerged aquatic vegetation (SAV). Therefore, TSM dynamics were controlled by the lake topography, wind-driven sediment resuspension and SAV distribution.     

Nickel-induced changes in lipid peroxidation, antioxidative enzymes, and metal accumulation in Lemna gibba

In this study, an experiment was carried out to study the process of stress adaptation in Lemna gibba grown under nickel stress (0-20 mg Ni L(-1)). The results showed that Ni concentrations in plants increased with increasing Ni supply levels and reached a maximum of 142.82 mg.kg1 DW at 0.5 mg x L(-1) Ni treatments. The level of photosynthetic pigments (Chl a, Chi b, and total Chl) and soluble proteins increased upon exposure to high Ni concentrations. At the same time, the level of malondialdehyde (MDA) increased with increasing Ni concentration. These results suggested an alleviation of stress that was presumably the results of antioxidants such as superoxide dismutase (SOD), catalase (CAT) which generally increased linearly with increasing Ni levels. In addition, the proline content in L. gibba increased with increasing nickel levels. Our present work concluded that Lemna gibba has a high level of nickel tolerance and accumulation. We also found that moderate nickel treatment (0.05-5 mg x L(-1)) alleviated oxidative stress in plants, while the addition of higher amounts of nickel (10-20 mg x L(-1)) could cause an increasing generation of ROS, which was effectively scavenged by the antioxidative system. Therefore, L. gibba may be used as a phytoremediator in moderately polluted aquatic ecosystems.     

再生水用于地下回灌过程中有机物的迁移和去除

人工地下水回灌是解决我国水资源短缺的有效途径之一.在实验室利用土壤柱系统,考查了回灌过程中有机物的迁移和去除.二级处理出水经活性碳吸附后进入土壤柱系统,土壤柱系统对TOC、UV-254和BOD₅的去除率分别为44%、34.36%和95%,并且大部分有机物是在土壤表层0～0.5 m被去除的.进水TOC浓度为9～11 mg·L^-1时,回灌过程中TOC浓度随土壤柱深度的变化符合指数方程：C=10e^-0.6934h(R²=0.8697). 用该方程可以较好地预测土壤柱出水中的TOC浓度.     

Primary production dynamics of dominant hydrophytes in Lake Provala (Serbia)

The objective of this investigation was to analyze the primary production of the dominant hydrophytes by monitoring levels of organic matter and organic carbon and estimating photosynthetic potential via the total chlorophyll content. The survey was conducted in Lake Provala (Serbia) throughout the peak vegetation period of the year 2000. The contents of organic matter and organic carbon for Myriophyllum spicatum L. were 105.11 g m⁻² and 73.66 g m⁻², Nymphoides peltata (Gmel.) Kunt. were 95.51 g m⁻² and 45.26 g m⁻² and Ceratophyllum demersum L. were 52.17 g m⁻² and 29.75 g m⁻². Chlorophyll A (Chl a) and chlorophyll A+B (Chl a+b) pigments ranged from 1.54 mg g⁻¹(Chl a) and 2.1 mg g⁻¹(Chl a+b) in M. spicatum to 5.27 mg g⁻¹(Chl a) and 7.53 mg g⁻¹(Chl a+b) in C. demersum. At full leaf out, the latter aquatic plants exceeded 50% cover of the open water surface. All species achieved maximum growth in June, but significant differences in growth dynamics were observed. At the end of the vegetation period, these plants sink to the bottom and decompose     

Seasonal changes in the structure of the anoxygenic phototrophic bacterial community in Lake Mogilnoe, a relict lake on Kil'din Island in the Barents Sea

An anaerobic phototrophic bacterial community in Lake Mogilnoe, a relict lake on Kil'din Island in the Barents Sea, was studied in June 1999 and September 2001. Irrespective of the season, the upper layer of the anaerobic zone of this lake had a specific species composition of sulfur phototrophic bacteria, which were dominated by the brown-colored green sulfur bacterium Chlorobium phaeovibrioides. The maximum number of phototrophic sulfur bacteria was observed in June 1999 at a depth of 9 m, which corresponded to a concentration of bacteriochlorophyll (Bchl) e equal to 4.6 mg/l. In September 2001, the maximum concentration of this pigment (3.4 mg/l) was found at a depth of 10 m. In both seasons, the concentration of Bchl a did not exceed 3 microg/l. Purple sulfur bacteria were low in number, which can be explained by their poor adaptation to the hydrochemical and optical conditions of the Lake Mogilnoe water. In June 1999, the water contained a considerable number of Pelodictyon phaeum microcolonies and Prosthecochloris phaeoasteroides cell chains, which was not the case in September 2001. A 16S rDNA-based phylogenetic analysis of pure cultures of phototrophic bacteria isolated from the lake water confirmed that the bacterial community is dominated by Chl. phaeovibrioides and showed the presence of three minor species, Thiocvstis gelatinosa, Thiocapsa sp., and Thiorhodococcus sp., the last of which is specific to Lake Mogilnoe.     

滆湖大洪港草、藻状态转换的磷阈值

以滆湖水草残存区--大洪港为对象,研究了自然条件下磷对大洪港草、藻状态转换的影响.对环境因子进行相关分析表明：总磷(TP)与叶绿素a(Chl a)、透明度(SD)呈较好的线性相关关系.主成分分析结果表明,TP、总氮(TN)是影响水质变化的主要成分,其中主成分的贡献率及最大分量来源为TP.总磷浓度的变化影响大洪港草/藻型状态的转换,大洪港冬季处于草型状态,春季从草型状态转换为草-藻中间状态,夏秋季一直维持在草-藻中间状态.系统从草型状态向藻型状态转换的湖水总磷阈值为61 μg·L^-1,从草-藻中间状态向藻型状态转换的总磷阈值为115 μg·L^-1.可通过采取削减与控制污染源、底泥疏浚、构建沉水植被区等措施来改善湖区生境,使TP浓度降低到61 μg·L^-1以下,以维持大洪港处于草型状态.     

三种农药对斑马鱼的急性毒性和生物浓缩系数

采用斑马鱼(Brachydanio rerio)为试验生物,研究了吡虫啉、三唑磷和哒螨灵的急性毒性和生物浓缩系数．通过毒性试验,获得了这3种农药对斑马鱼的24、48、72和96h LC50值．这3种农药的96h LC50值分别为281．37mg·L^-1、8．37mg·L^-1和11．66μg·L^-1．根据急性毒性数据和有关技术指南,确定生物浓缩试验浓度和持续暴露时间为14d．经0．5和5mg·L^-1吡虫啉暴露后的生物浓缩系数(BCFs)分别为1．52和0．97．经0．02和0．2mg·L^-1三唑磷暴露后的BCFs分别为9．00和8．45．经0．1和1μg·L^-1哒螨灵暴露后的BCFs分别为5600和4920．     

Secchi disk — chlorophyll relationships in a lake with highly variable phytoplankton biomass

In meseutrophic Lake Constance mean euphotic phytoplankton chlorophyll concentrations vary about 100-fold over the year. Concomitant fluctuations in euphotic depth (Z_eu) and Secchi depth (Z_s) are related to each other in a non-linear fashion that as a rough approximation can be expressed by Z_eu 5 Z_s.Secchi depth is to a great extent a function of beam attenuation of light which depends on the inherent optical properties of the water and is highly sensitive to light scattering from particles. Euphotic depth, by contrast, is a function of the vertical light attenuation coefficient which also depends on absorption and scattering, but is less sensitive to the latter than beam attenuation. Algal cells both absorb and scatter light and therefore influence Secchi depth and euphotic depth, however, in different fashions.Whenever the lake is clear due to scarce phytoplankton, scattering is small and beam attenuation only exceeds vertical light attenuation by a relatively small factor. As a consequence, the ratio of euphotic depth to Secchi depth is small (1.5–2.5). When the lake is turbid due to high algal density, enhanced scattering from algal cells and detrital particles causes beam attenuation to rise more than vertical light attenuation, thus leading to high ratios of euphotic depth to Secchi depth (3–5). The relatively close relationships between Secchi depth and chlorophyll in Lake Constance are due to (1) high influence of chlorophyll concentration on water transparency, (2) co-variation of phytoplankton and other suspended particles, and (3) limited variation of cellular chlorophyll contents.