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| 1 | Relationship between petroleum hydrocarbon and plankton in a mesocosm experiment显示文摘A mesocosm experiment was carried out from May 26 to June 1, 1998 at the location of 30’52’N, 122’36’E, the Changjiang Estuary, in order to measure the influence of petroleum hydrocar- bon to the ecosystem, furthermore, to estimate the environmental capacity. In the experiment, it is found that the petroleum hydrocarbon can, in some degree, enhance the growth of diatom, but inhibit the growth of dinoflagellate. In general, the petroleum hydrocarbon can inhibit the growth of both Phytoplankton and zooplankton, and can the inhibit the growth of total plankton (including phytoplankton and zooplankton) as well. A kinetic model was presented to estimate the uptake/release rate constants of petroleum hydrocarbon by plankton, and thereafter, the uptake and release rate constants (k1, k2), bioconcentration factor (BCF) as well as the petroleum bydrocarbon influenced influenced uptake and release rate constants of nutrients by phytoplankton (kup, krel) were obtained. The results imply that the bioconcentration of petroleum hydrocarbon by plankton is fairly large and petroleum hydrocarbon caused no significant influence on the uptake of N- NO3, but significant influence on that of P -PO4. In addition, the application of kinetic model for the bioconcentration of volatile organic toxic compound by organism suggests that the uptake of petroleum hydrocarbon by plankton was an important process for the environmental capacity of petroleum hydrocarbon. | Shi Xiaoyong, Wang Xiulin, Han Xiurong, Jiang Yu Zhu Mingyuan, Chen Shang, Koshikawa Hiroshi (1. Ocean University of Qingdao, Qingdao 266003, China 2. First Institute of Oceanology, Qingdao 266061, China 3. National Institute for Environmental Studies, Ja | 2001 | Acta Oceanologica Sinica2001，20，2： | 12 |
| 2 | Preliminary study on assessment of nutrient transport in the Taihu Basin based on SWAT modeling显示文摘With the Taihu Basin as a study area, using the spatially distributed and mechanism-based SWAT model, preliminary simulations of nutrient transport in the Taihu Basin during the period of 1995~2002 has been carried out. The topography, soil, meteorology and land use with industrial point pollution discharge, the loss of agricultural fertilizers, urban sewerage, and livestock drainages were all considered in the boundary conditions of the simulations. The model was calibrated and validated against water quality monitoring data from 2001 to 2002. The results show that the annual total productions of nitrogen (TN) and phosphorus (TP) into Lake Taihu are 40000t and 2000t respectively. Nutrient from the Huxi Region is a major resource for Lake Taihu. The non-point source (surface source) pollution is the main form of catchment sources of nutrients into Lake Taihu,occupied TN 53% and TP 56% respectively. TN and TP nutrients from industrial point pollution discharge are 30% and 16%, and sewerage in both forms of point source and non-point source are TN 31% and TP 47%. Both the loss of agricultural fertilizers and livestock drainages from the catchment should be paid more attention as an important nutrient source. The results also show that SWAT is an effective model for the simulation of temporally and spatially nutrient changes and for the assessment of the trends in a catchment scale. | LAI Geying, YU Ge & GUI Feng Nanjing Institute of Geography & Limnology, Chinese Academy of Sciences, Nanjing 210008, China The Graduate School of the Chinese Academy of Sciences, Beijing 100039, China Key Lab of Poyang Lake Ecological Environment and Resource Development, Jiangxi Normal University, Nanchang 330027, China | 2006 | Science China Earth Sciences2006，49，z1： | 11 |
| 3 | Variation characteristics of heavy metals and nutrients in the core sediments of Taihu Lake and their pollution history显示文摘The sedimentary environment change, trophic evolution and heavy metals pollution history of the northern Taihu Lake in the last 100 years are studied according to the sedimentary geochemical proxies of the core sediments, such as grain size, nutrients, heavy metals, diatom, etc. The nutrients in the sediments depended mainly on the lake internal circulation and the heavy metals were from natural geogenic sources before the 1920s, which were not influenced by human activities generally, and grain size was one of the key factors influencing heavy metals content in the sediments.The alternation of manner and strength of human activities in Taihu Lake catchment before and after the 1920s made the lake sediments coarser, and hence heavy metals and TP content decreased contrasted with that before the 1920s. TP content in sediments and water increased from the 1950s to late 1970s due to anthropogenic pollutants discharge, and the lake belonging to mesotrophic state.TN and TOC content and C/N ratio increased due to the increasing external pollutants into Taihu Lake by human activities, TP content also increased obviously in water and sediments, and the diatom association was dominated by eutrophic species since the late 1970s, indicating the eutrophication state of Taihu Lake in this period. Meanwhile the increasing in heavy metals content, such as Cu, Mn,Ni, Pb and Zn, and their proportion of valid fractions in the sediments indicates that they all result from human pollutants since the late 1970s. The heavy metals in the surface sediments have certain potential biological toxicity due to the higher SEM/AVS ratio. | LIU Enfeng SHEN Ji LIU Xingqi ZHU Yuxin WANG Sumin | 2006 | Science China Earth Sciences2006，49，z1： | 11 |
| 4 | Transport and distribution of nutrients in anchovy spawning ground to the southern waters of Shandong Peninsula显示文摘The distribution of nutrients and the effect of side transport of nutrients on anchovy spawning ground to the southern waters of Shandong Peninsula are discussed based on the data collected in June 2000, May and June 2001. The coastal current and upwelling are the main physical processes of nutrient transport to the southern waters of Shandong Peninsula. The concentrations of nutrients, Chl-a, the density of anchovy eggs, larva and juvenile fish increase obviously where they are greatly affected by these processes, while the contents of nutrients and Chl-a, the density of anchovy eggs, larva and juvenile fish decrease significantly where these processes diminish or disappear. The investigation suggest that the side transport of nutrients by Lubei (North Shandong) coastal current in the northern area causes the Chl-a content to be high and dense anchovy eggs, larva and juvenile fish to be dense in the coastal area of the Chengshan Cape.In the southern area, the riverine input from Subei irrigation ditch with high content of nutrients inshore and upwelling in the western edge of the Huanghai Sea Cold Water offshore should be responsible for high Chl-a concentration and dense anchovy eggs, larva and juvenile fish. It is possible that these processes of nutrient transport have controlled the anchovy spawning ground to the southern waters of Shandong Peninsula. | Gao Shengquan 1,2,Lin Yi’an 1,2, Jin Mingming1,Liu Xiaoya1 1. Laboratory of Regional Oceanography, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China. 2. Laboratory of Submarine Geosciences, Hangzhou 310012,China | 2003 | Acta Oceanologica Sinica2003，22，4： | 4 |
| 5 | Vertical properties of nutrients and oxygen under temperature-salinity structure of the Bering Basin in July 1999显示文摘The China R/V Xuelong went on the first Arctic scientific cruise, and we obtained 271 hydro-chemical samples from 22 deep-sea stations in the Bering Basin in late July, 1999. Here we describe vertical properties of silicate [Si], dissolved inorganic nitrogen [DIN] or [N] (nitrate plus ammonium plus nitrite), phosphate [P] and oxygen [O2] in seawater under potential temperature-salinity structure. The seasonal stratification in the summer and the water exchanges of the North Pacific Ocean over the Bering Basin resulted in that the four layers of vertical structure with two thermoclines may be found. Vertical [Si] and [N] and [P] profiles show that the nutrients are consumed mainly in ≤50 m and the order of deficient nutrients is [Si] the first, [N] the second and [P] the third. The [N] and [P] increase with depth downward to about 500 m and then both decrease, but the [Si] increases from 150 m to 2000 m or the bottom. In ≥150 m the [O2] decreases, which is related with both [P] and [N] increasing closely. Seawater [N]:[P] ratios are 6-12 in ≤50 m, 10.5-14.3 in 100-150 m and 11.7-15.8 from 300 m to the bottom. | Jin Mingming (金明明) | 2002 | Chinese Journal of Polar Science2002，13，2： | 2 |
| 6 | EUTROPHICATION AND RED TIDES AS CONSEQUENCES OF ECONOMIC DEVELOPMENT显示文摘This paper reports the phenomena of eutrophication and red tides correlated with human activities, especially economic development. The fertilizer production in China has been accelerated since the 1970s and has approximately doubled the rate of nitrogen input into the terrestrial N cycle. While the rate of the total population growth of China maintains relatively stable the rate of population growth in cities and towns in the 1980s and 1990s was 10 times higher than ever before. As a result, the urban sewage discharge increased by 400%, which carries 1 million tons of nitrogen into the environmental waters per year. The mining of P minerals and application of P-containing fertilizers greatly enhanced the input of P into the waters. Harmful algal blooms are consequence of the eutrophication. The high frequency of algal bloom is related to the quick economic development since the 1970s and the eutrophication of environmental waters. Analysis indicates that the number of the red tide events in the China Seas roughly follows the curve of the growth rate of GDP with a time lag of about 5-6 years. The time lag is explained as the period of the cycle of accumulation, denitrification and release of the nutrients with transportation and resuspension of the sediment. | Zhao-Yin WANG1, Yongsheng WU2, and Guangqian WANG3 1 Prof., Dept. of Hydraulic Engineering, Tsinghua University & International Research and Training Center on Erosion and Sedimentation, Beijing 100084, China, Email: zywang@tsinghua.edu.cn or zywang@sun | 2001 | International Journal of Sediment Research2001，16，4： | 2 |
| 7 | Exchange fluxes of nutrients between sediment and sea water in the Bohai Sea显示文摘Investigations of sediment-water fluxes of nutrients in the Bohai Sea were carried out in September - October 1998 and April - May 1999. The exchange fluxes of nutrients between sediment and sea water were determined by incubating the core-top sediments with overlying water aerated with air. The benthic fluxes of NO3- , NO2- , NH4+ , DIN, DON and TON in the first cruise and the flux-es of NO3 , NO2- , NH4+ , DIN, DON, TDN, PO43- , DOP and TDP in the second cruise were measured. The exchange fluxes of nutrients in fall were higher than in spring. The benthic nutrient fluxes represented 15% -55% of nutrient budgets in the Bohai Sea. | Liu Sumei, Zhang Jing, Zhang Hong, Yu Jianhua 1. College of Chemistry and Chemical Engineering, Ocean University of Qingdao, Qingdao 266003, China 2. State Key Laboratory of Estuarine and Coastal Research, East China Normal University, 3663 Zhongshanbei | 2001 | Acta Oceanologica Sinica2001，20，3： | 0 |
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