| 长江水体溶解态无机氮和磷现状及长期变化特点 |
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| 引用本文： | 江 涛,俞志明,宋秀贤,曹西华,袁涌铨.长江水体溶解态无机氮和磷现状及长期变化特点[J].海洋与湖沼,2012,43(6):1067-1075. |
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| 作者姓名： | 江 涛 俞志明 宋秀贤 曹西华 袁涌铨 |
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| 作者单位： | 1. 中国科学院海洋研究所生态与环境重点实验室,青岛266071 中国科学院研究生院,北京100039
2. 中国科学院海洋研究所生态与环境重点实验室,青岛,266071 |
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| 基金项目： | 国家基金委“创新研究群体科学基金”, 41121064 号; 国家973 项目, 2010CB428706 号; 中国科学院方向性项目, KZCX2-YW-208号和国家863计划专题项目, 2008AA09Z107 号 |
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| 摘 要： | 于2006年2、5、8和11月对长江从攀枝花至河口和上游的两条支流雅砻江和嘉陵江的溶解态无机氮(NO-3-N、NO-2-N和NH+4-N)和磷酸盐(PO43--P)进行了取样调查,同时结合长江营养盐的历史数据,分析了长江水体中溶解态无机氮、磷的长期变化特点。结果表明,长江NO-3-N、NH+4-N、DIN(包括NO-3-N、NO-2-N和NH+4-N)和PO3-4-P浓度从上游到下游显示出增加趋势,但存在季节差异;NO2-N浓度总体较低,在长江中下游(武汉—南京)浓度较高。长江从上游到下游DIN通量的变化主要受径流量的影响,从上游到下游单位面积年产N量逐渐升高;PO3-4-P输送通量从上游往下游呈增加趋势,也主要受径流量控制,但从季节变化来讲,PO3-4-P的月输送通量受其浓度的控制更加明显。自20世纪60年代来,长江水体中NO3--N、NO2--N、DIN和PO3-4-P的浓度都处于缓慢上升趋势,但到80年代上升速度明显加快;不同阶段DIN和34PO-P的季节变化特点也不尽相同,反映了其来源的差异。目前,长江水体中溶解态无机氮、磷浓度与国内及国际河流相比处于中等水平。
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| 关 键 词： | 氮 磷 输送通量 长江 |
| 收稿时间： | 2011/12/31 0:00:00 |
| 修稿时间： | 2012/2/28 0:00:00 |
ANALYSIS OF DISTRIBUTION, FLUX AND LONG-TERM VARIATIONS OF DISSOLVED INORGANIC NITROGEN AND PHOSPHATE IN THE CHANGJIANG RIVER |
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| JIANG Tao,YU Zhi-Ming,SONG Xiu-Xian,CAO Xi-Hua and YUAN Yong-Quan.ANALYSIS OF DISTRIBUTION, FLUX AND LONG-TERM VARIATIONS OF DISSOLVED INORGANIC NITROGEN AND PHOSPHATE IN THE CHANGJIANG RIVER[J].Oceanologia Et Limnologia Sinica,2012,43(6):1067-1075. |
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| Authors: | JIANG Tao YU Zhi-Ming SONG Xiu-Xian CAO Xi-Hua and YUAN Yong-Quan |
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| Institution: | Key Laboratory of Marine Ecology and Environmental Sciences, Institute of Oceanology, Chinese Academy of Sciences;Graduate School of the Chinese Academy of Sciences;Key Laboratory of Marine Ecology and Environmental Sciences, Institute of Oceanology, Chinese Academy of Sciences;Key Laboratory of Marine Ecology and Environmental Sciences, Institute of Oceanology, Chinese Academy of Sciences;Key Laboratory of Marine Ecology and Environmental Sciences, Institute of Oceanology, Chinese Academy of Sciences;Key Laboratory of Marine Ecology and Environmental Sciences, Institute of Oceanology, Chinese Academy of Sciences |
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| Abstract: | The concentrations of dissolved inorganic nitrogen (NO?3-N, NO?2-N and NH+4-N) and dissolved inorganic phosphate (PO3-4-P) were investigated from Panzhihua to Shanhai in the Changjiang River and two tributaries of the upper drainage (Yalongjiang River and Jialingjiang River) during February, May, August and November in 2006. The results showed that NO?3-N, NH+4-N, DIN or PO3-4-P concentration increased from upstream to downstream while there were seasonal differences. The concentration of NO?2-N was relatively low and it was higher in the middle and lower reaches from Wuhan to Nanjing. DIN flux in the Changjiang River was mainly controlled by water discharge, however monthly PO3-4-P flux was greatly influenced by the riverine concentration of PO3-4-P when the seasonal variations were considered. The areal yields of DIN and PO3-4-P increased obviously from upstream to downstream. The concentrations of NO?3-N, NO?2-N, DIN and PO3-4-P increased steadily since 1960s and rose greatly after 1980. The seasonal variations of DIN and PO3-4-P were quite different, which suggested that they might be from different sources. Compared with other large rivers in the world, the concentrations of DIN and PO3-4-P were higher than those of the large and less disturbed world systems and lower than those of the eutrophic rivers in Europe and North America. |
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| Keywords: | Nitrogen Phosphate Nutrients flux Changjiang River |
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