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福州地区海湾和河口潮汐沼泽湿地秋季上覆水营养盐分布特征 被引量:10
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作者 何露露 杨平 +2 位作者 谭立山 仝川 黄佳芳 《环境科学》 EI CAS CSCD 北大核心 2019年第4期1788-1796,共9页
2015年秋季,采集福建省福州市沿海兴化湾(福州一侧)、福清湾、闽江口、敖江口和罗源湾5个海湾和河口分布的潮汐沼泽湿地的上覆水,并测定上覆水中的氮、磷营养盐浓度及其他水体理化指标,探讨不同海湾和河口潮汐沼泽湿地上覆水营养盐浓度... 2015年秋季,采集福建省福州市沿海兴化湾(福州一侧)、福清湾、闽江口、敖江口和罗源湾5个海湾和河口分布的潮汐沼泽湿地的上覆水,并测定上覆水中的氮、磷营养盐浓度及其他水体理化指标,探讨不同海湾和河口潮汐沼泽湿地上覆水营养盐浓度形成差异的原因.结果表明:①不同海湾和河口潮汐沼泽湿地上覆水中的氮、磷营养盐浓度均存在显著差异(P <0. 05),福清湾氮、磷营养盐浓度均较高,兴化湾氮营养盐浓度最低,敖江口磷营养盐浓度最低,其中福清湾上覆水营养盐浓度主要受区域水产养殖、陆源污染、地形的影响,而兴化湾主要受潮汐影响显著;②植被类型对沼泽湿地上覆水营养盐浓度有一定影响,南方碱蓬群落沼泽湿地上覆水中的氮营养盐浓度较高,互花米草群落沼泽湿地上覆水中的氮、磷营养盐浓度较低;同一海湾或河口沼泽湿地不同植物群落下上覆水中的营养盐浓度不同,且规律复杂.潮汐、地表径流、植物群落、地形、人为活动均会对海湾和河口沼泽湿地上覆水中的营养盐浓度产生重要影响. 展开更多
关键词 湿地 植物群落 上覆水 营养盐 河口/海湾 福州
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THE BIOGEOCHEMISTRY OF PHOTOSYNTHETIC PIGMENTS IN THE JIULONG RIVER ESTUARY AND WESTERN XIAMEN BAY 被引量:4
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作者 徐立 洪华生 +1 位作者 王海黎 陈伟琪 《Chinese Journal of Oceanology and Limnology》 SCIE CAS CSCD 2001年第2期164-171,共8页
High performance liquid chromatography (HPLC) analysis of photosynthetic pigments in samples from Western Xiamen Bay and the Jiulong River Estuary showed that their major carotenoids were fucoxanthin, peridinin, zeaxa... High performance liquid chromatography (HPLC) analysis of photosynthetic pigments in samples from Western Xiamen Bay and the Jiulong River Estuary showed that their major carotenoids were fucoxanthin, peridinin, zeaxanthin, violaxanthin, and diadinoxanthin. Diatoms dominated in the spring bloom, dinoflagellates in summer. Violaxanthin and chlorophyll b indicated the appearance of chrysophytes and green algae, most of which were freshwater species. The high phytoplankton biomass region was located at the inner part of the bay. Diatoms and dinoflagellates dominated phytoplankton communities, contributing to over 50% of total biomass. All the main diagnostic carotenoids were significantly (P<0.01) correlated negatively to dissolved inorganic phosphorus, suggesting that they were limited by phosphorus. The high negative linear relationship (P<0.0001) between dissolved inorganic phosphorus and peridinin (dinoflagellates indicator) implied the potential of dissolved inorganic phosphorus for triggering red tide events in this region. 展开更多
关键词 PIGMENTS CHLOROPHYLL carotenoids ESTUARY Xiamen Bay
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Short-and long-term sediment transport in western Bohai Bay and coastal areas
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作者 冯桓 张卫国 +5 位作者 贾丽 Michael P.WEINSTEIN 张秋丰 袁德奎 陶建华 俞立中 《Chinese Journal of Oceanology and Limnology》 SCIE CAS CSCD 2010年第3期583-592,共10页
Sediment cores (-40-100 cm) were collected at 12 locations in the western Bohai Bay, the Haihe River estuary, the Yongding River estuary and the Tianjin Harbor, China, during 24-26 July 2007, and analyzed for ^7Be a... Sediment cores (-40-100 cm) were collected at 12 locations in the western Bohai Bay, the Haihe River estuary, the Yongding River estuary and the Tianjin Harbor, China, during 24-26 July 2007, and analyzed for ^7Be and ^210pb activities. Due to localized hydrodynamic patterns and frequent disturbance from dredging activities, steady-state sedimentation features were not observed in this study. As demonstrated in the VBe and ^210pb profiles, the temporal and spatial variations of these radionuclides support a non-steady state depositional environment in the study area. By comparing ^7Be and ^210pb inventories in the sediments with those of the atmospheric source, we found that: 1) sediments dredged from the Tianjin Harbor or eroded from nearby estuarine and coastal areas are retained in the western Bohai Bay for relatively short intervals (several months), as reflected in the relatively high ^7Be inventories in the western Bohai Bay; 2) over the long-term (years to decades), ^210Pb inventories in the sediments imply that there is a net on-shore transport of sediments, and the sediments are mass-balanced in the entire study area. Overall, our results suggest that the sediments are retained in the estuaries and the western Bohai Bay despite local variability in sediment dynamics and disturbance due to human activities. 展开更多
关键词 Bohai Bay ESTUARY SEDIMENTATION sediment transport RADIONUCLIDE
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