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国家自然科学基金(40203007)

作品数:26 被引量:780H指数:16
相关作者:朱广伟秦伯强陈伟民张运林高光更多>>
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26 条 记 录,以下是 1-10
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Experimental study on phosphorus release from sediments of shallow lake in wave flume被引量:12
2006年
Influence of wave on sediment resuspension and nutrients release from sediments, collected from Lake Taihu and Lake Chaohu, was studied in flume experiments. Under strong-wave conditions, concentrations of suspended solids (SS), total phosphorus (TP) and dissolved total phosphorus (DTP) in overlying water were increased significantly following the sediments re-suspension. During the experiments on sediments of Lake Taihu and Lake Chaohu, TP concentrations increased 6 times and 3 times, and DTP concentration increased 100% and 70% more than it in presuspension, respectively. Concentration of soluble reactive phosphorus (SRP) of experiment on sediment of Lake Taihu increased 25%. During the massive sediment suspension, the dissolved phosphorus in pore water and much of the phosphorus adsorbed by the sediment particles were released into overlying water. The phenomena in this wave flume experiment are quite similar to the situation observed in situ of Lake Taihu. The critical wave stresses of sediment re-suspension are nearly equal. The change of concentrations of SS, TP, and SRP was the same as that in situ situation.This study showed that concentrations of TP and SRP in lake water could be increased significantly by wave disturbance. Phosphorus release was significantly enhanced by wave disturbance at the beginning of massive sediment re-suspension, but decreased later.
SUN Xiaojing,ZHU Guangwei, LUO Liancong & QIN Boqiang Nanjing Institute of Geography & Limnology, Chinese Academy of Sciences, Nanjing 210008, China
关键词:SHALLOWWAVEWAVEFLUME
不同风浪条件下太湖梅梁湾光合有效辐射的衰减被引量:29
2005年
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.
张运林秦伯强陈伟民胡维平高光朱广伟罗潋葱
关键词:悬浮物真光层深度
Direct evidence of phosphorus outbreak release from sedi-ment to overlying water in a large shallow lake caused by strong wind wave disturbance被引量:48
2005年
Concentration variations of suspended solids (SS), total phosphorus (TP), dissolved total phosphorus (DTP), dissolved reactive phosphorus (SRP), and algae available phosphorus (AAP) in overlying water were ob- served during the coldest week in a year in Lake Taihu, a large shallow lake in China. Water samples at different water depths were collected with wind speeds of 8, 12, 0 and 0 m/s on 23, 24, 26 and 30 January 2004, respectively. On 23 Janu- ary 2004, SS concentration increased to 258 mg/L with a wind speed of 8 m/s lasting for 1 h. SS concentration kept increasing and reached to 507 mg/L when the strong wind lasted for 24 h and the peak value of wind-speed reached to 12 m/s on 24 January 2004. On 26 January 2004, SS concen- tration decreased to 51 mg/L with the wind speed smaller than 2 m/s lasting for about half a day. Then after five con- tinuous waveless days, SS concentration decreased to 21 mg/L on 30 January 2004. The observed results confirmed that sediments in Lake Taihu would be intensively suspended if the surface wind speed is greater than 8 m/s, and the mag- nitude of SS would increase with increasing wind-speed. Coupled with the intensive sediment suspending, concentra- tions of TP, DTP and SRP on 23 January were 0.210, 0.048 and 0.035 mg/L, respectively. And they were 0.299, 0.054 and 0.026 mg/L on 24 January, which were significantly higher than those on 26 and 30 January. SRP concentration on 23 January was twice as high as that observed on 30 January. It indicates that the strong wind may result in an outbreak re- lease of phosphorus. Moreover, AAP contents in suspended solids were 132, 97 and 226 mg/kg on 23, 24 and 26 January, respectively. Therefore, it could be estimated that this strong wind process resulted in 987 t of TP, 80 t of SRP and 167 t of AAP releasing from sediments into overlying water. Since such strong wind process is frequent in the area of Lake Taihu, dynamical release driven by wind-induced wave dis- turbance may be the main mode for internal release of phosphorus. It
ZHUGuangwei QINBoqiang GAOGuang
关键词:藻类植物
太湖水体中胶体磷含量初探被引量:11
2006年
为了探明太湖水体中胶体磷含量,更深入认识营养盐在大型浅水湖泊中的循环过程和机理,分别从太湖的梅梁湾和贡湖湾两个不同类型的湖区采集水样,利用切向流超滤方法分离出胶体物质,对太湖水体中胶体磷含量进行了初步研究.结果表明:太湖水体春季胶体磷含量在0.017-0.029 mg/L间,其中梅梁湾藻型湖区胶体磷含量范围是0 023- 0.029 mg/L,贡湖湾草型湖区胶体磷含量在0.017-0.022 mg/L间.梅梁湾水体胶体磷占总磷比例平均为28.6%;而贡湖湾胶体磷占总磷比例平均达到39.3%.梅梁湾水体真溶解态磷含量显著高于贡湖湾水体,达贡湖湾的4倍.与澳大利亚的17个湖泊相比,太湖属胶体磷含量偏低的湖泊,但相对于海洋的研究结果,太湖胶体磷含量明显偏高.
孙小静张战平朱广伟秦伯强
关键词:胶体太湖浅水湖泊
长江中下游浅水湖泊沉积物再悬浮对水下光场的影响研究——以龙感湖和太湖为例被引量:15
2005年
基于2003年7月在龙感湖、太湖梅梁湾以及2004年7月在太湖站栈桥的连续不同风浪条件下水下光场原位观测资料,分析风浪作用引起的沉积物再悬浮对PAR衰减,吸收系数及真光层深度的影响。结果表明,在龙感湖,小风浪、中风浪和大风浪的PAR衰减系数分别是1.74,2.02,2.45m^(-1),400~700 nm光谱衰减系数变化范围分别为0.98~2.97,1.34~3.95,1.82~5.40 m^(-1);在太湖梅梁湾,小风浪、中风浪和大风浪PAR衰减系数分别是2.63,3.72,4.37m^(-1),从小风浪到、中风浪、大风浪衰减系数分别增加了41%,66%;太湖站栈桥边PAR波段积分CDOM吸收系数在中风浪和大风浪的值分别为0.26,0.28 m^(-1),浮游植物吸收系数从中风浪到大风浪反而由0.76降低到0.49m^(-1),沉积物再悬浮引起非藻类颗粒物的吸收则由0.94增加到1.73m^(-1),增加了84%,总悬浮物颗粒物吸收由1.70增加到2.22m^(-1),增加了30.6%.非藻类颗粒物吸收对总吸收系数贡献最大,中风浪、大风浪下贡献率分别达44.14%,65.05%。龙感湖,梅梁湾,栈桥边3站点从中风浪到大风浪,PAR真光层深度分别降低0.40,0.19,0.20 m。透明度、PAR衰减系数、真光层深度与悬浮物浓度、风速、波高等均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。由此可见,在龙感湖和太湖等长江中下游浅水湖泊,风浪扰动引起悬浮物浓度的增加尤其是无机颗粒物的增加是影响水下光场的主导因素。
张运林秦伯强朱广伟高光罗潋葱陈伟民
关键词:浅水湖泊太湖漫射衰减系数悬浮物
浅水湖泊沉积物中磷的地球化学特征被引量:170
2003年
对太湖不同污染状况和生态系统状况的湖区沉积物中磷的地球化学形态及其分布进行了研究。结果发现,沉积物的理化性质和磷的化学形态一般都在表层下深5~15cm发生明显的转折;草型湖区、藻型湖区、开阔湖面的大湖区沉积物的理化性质、间隙水中的磷浓度及沉积物中磷的形态存在较大的差异。东太湖沉积物间隙水磷浓度和交换态磷含量都显著低于其他湖区;风浪扰动相对剧烈的开阔湖面湖区沉积物中磷的沉积规律也不同于梅梁湾藻型湖区和东太湖草型湖区。研究表明,浅水湖泊中水生生物状况、风浪扰动状况对沉积物中磷的地球化学行为有至关重要的影响。
朱广伟高光秦伯强张路罗潋葱
关键词:浅水湖泊沉积物地球化学富营养化太湖
风浪扰动对太湖水体悬浮物重金属含量的影响被引量:20
2006年
通过离心浓缩的方法,获取太湖梅梁湾口东岸处(即梅梁湾与贡湖湾的交界处)不同风浪条件下的悬浮颗粒物.冷冻干燥,微波消解,ICP-AES的方法测定了其中Co、Cr、Cu、Ni、Pb、Zn等重金属元素及Al、Ca、Fe、Mn等相关金属元素的含量.结果发现,小风浪(2 m/s)、中风浪(7 m/s)和大风浪(11 m/s)下:①水体总悬浮颗粒态金属的量依次大幅度增加;②单位悬浮颗粒物中各金属元素的含量在不同风浪下变化不同.Ca在小、中、大风浪下含量依次增大;Zn在小、中、大风浪下含量依次减少;Mn和Cu的含量变化趋势相同:与小风浪相比,中风浪下Mn、Cu的含量显著增大;与中风浪相比,大风浪下含量显著减少;其它元素Al、Fe、Ni、Pb、Co、Cr等在单位悬浮物中,中风浪与小风浪相比含量减少,大风浪与中风浪相比含量略微增加.研究表明:①金属元素在水体总悬浮物中的含量主要受风浪影响,但风浪对单位悬浮物中金属含量的影响则因元素而异;②除Cu、Mn、Zn外,悬浮物中重金属含量随粒径增大含量减少.
池俏俏朱广伟张战平秦伯强
关键词:太湖风浪扰动悬浮物重金属
风浪对太湖水体中胶体态营养盐和浮游植物的影响被引量:47
2007年
为了解不同风浪条件下太湖水中胶体态营养盐和浮游植物含量的特征,选择不同风速情况进行现场观测和采样,用切向流超滤法获取胶体,测定胶体态有机碳、氮、磷及其他形态营养盐含量.同时收集浮游植物样品,测定其密度和生物量.结果表明,在风速小于4m/s时胶体氮(CN)和胶体磷(CP)含量随风速变大而升高,而在风速大于4m/s时其含量不再升高,甚至略有降低;叶绿素a(Chl-a)、浮游植物密度、蓝藻密度和蓝藻生物量均在风速小于4m/s时随风速增大而升高,在风速大于4m/s时随风速增大而降低,说明小风浪有利于蓝藻生长或漂浮,而大风浪对其生长或漂浮不利.CN和CP含量与浮游藻类含量呈显著正相关,表明在藻类生长旺盛的夏季,太湖水中胶体氮、磷的主要来源为藻类产物.
孙小静秦伯强朱广伟张战平
关键词:风浪太湖营养盐浮游植物
太湖表层沉积物重金属元素的来源分析被引量:77
2004年
根据太湖MS岩芯重金属元素与Al的线性回归分析及元素/Al、V/Al比率散点图变化规律,讨论了太湖沉积物中重金属元素的来源特征。结果表明:20世纪20年代中期以前,重金属元素主要为自然来源;20年代中期—70年代中期,尽管沉积物中Al、Fe、Zn、Mn、V、Cr等重金属元素含量随沉积物粒度变粗而明显下降,但除Hg受到一定程度的人为污染之外,其它重金属元素仍以自然来源为主,物源有所变化;70年代末期以来,沉积物中重金属元素人为污染逐渐加重,Pb、Cu、Zn、Hg、As等元素既有流域母质来源,又受到一定程度的人为污染。
刘恩峰沈吉朱育新夏威岚朱广伟
关键词:表层沉积物太湖重金属
Phosphorus forms and bioavailability of lake sediments in the middle and lower reaches of Yangtze River被引量:12
2006年
Forms of phosphorus in sediments from 25 lakes in the middle and lower reaches of Yangtze River were analyzed by the sequential extraction procedure. Contents and spatial distrubution of algal available phosphorus (AAP) in sediments of Lake Taihu, the third largest freshwater lake of China, were also studied. Relationships between phosphorus forms in sediment and macrophytes coverage in sample sites, as well as phosphorus forms in sediments and chlorophyal contents in lake water were discussed. Exchangeable form of phosphorus (Ex-P) in surface sediments was significantly positive correlative to total phosphorus (TP), dissolved total phosphorus (DTP) and soluble reactive phosphorus (SRP) contents in the lake water. Bioavailable phosphorus (Bio-P) contents in sediments from macrophytes dominant sites were significantly lower than that in no macrophyte sites. In Lake Taihu, Ex-P content in top 3 cm sediment was highest.However, content of ferric fraction phosphorus (Fe-P) was highest in 4-10 cm. Bioavalilble phosphorus (Bio-P) contents in surface sediments positively correlated to Chlorophyll a contents in water of Lake Taihu with significant difference. Therefore, contents of Bio-P and AAP could be acted as the indicators of risks of internal release of phosphorus in the shallow lakes. It was estimated that there were 268.6 ton AAP in top 1 cm sediments in Lake Taihu. Sediment suspension caused by strong wind-induced wave disturbance could carry plenty of AAP into water in large shallow lakes like Lake Taihu.
ZHU Guangwei QIN Boqiang ZHANG Lu
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