[1] Meybeck M. Carbon, nitrogen, and phosphorus transport by world rivers [J]. American Journal of Science, 1982, 282(4): 401-450.[2] Josette G, Leporcq B, Sanchez N, et al. Biogeochemical mass-balances (C, N, P, Si) in three large reservoirs of the Seine Basin (France) [J]. Biogeochemistry, 1999, 47(2): 119-146.[3] Syvitski J P M, V¨or¨osmarty C J, Kettner A J, et al. Impact of humans on the flux of terrestrial sediment to the global coastal ocean [J]. Science, 2005, 308: 376-380.[4] Milliman J D. Blessed dams or damned dams? [J]. Nature, 1997, 386: 325-327.[5] Zhang J, Zhang Z F, Liu S M, et al. Human impacts on the large world rivers: Would the Changjiang (Yangtze River) be an illustration? [J]. Global Biogeochemical Cycles, 1999, 13:1099-1105.[6] Kelly V J. Influence of reservoirs on solute transport: a regional-scale approach [J]. Hydrological Processes, 2001, 15: 1227-1249.[7] Nilsson C, Reidy C A, Dynesius M, et al. Fragmentation and flow regulation of the world’s large river systems [J]. Science, 2005, 308(5720): 405-408.[8] Friedl G, W¨uest A. Disrupting biogeochemical cycles-Consequences of damming [J]. Aquatic Sciences, 2002, 64(1): 55-65.[9] Humborg C, Blomqvist S, Avsam E, et al. Hydrological alterations with river damming in northern Sweden: Implications for weathering and river biogeochemistry [J]. Global Biogeochemical Cycles, 2002, 16(3): 12-1-12-13.[10] 陈庆伟, 刘兰芬, 刘昌明. 筑坝对河流生态系统的影响及水库生态调度研究[J]. 北京师范大学学报 (自然科学版), 2007, 43(5): 578-582.[11] 刘丛强, 汪福顺, 工雨春, 等. 河流筑坝拦截的水环境响应——来自地球化学的视角[J]. 长江流域资 源与环境, 2009, 18(4): 384-396.[12] 冉祥滨, 于志刚, 姚庆祯, 等. 水库对河流营养盐滞留效应研究进展[J]. 湖泊科学, 2009, 21(5):614-622.[13] 张恩仁, 张经. 三峡水库对长江N、P营养盐截留效应的模型分析[J]. 湖泊科学, 2003, 15(1): 41-48.[14] Aucour A M, Sheppard S M F, Guyomar O, et al. Use of 13C to trace origin and cycling of inorganic carbon in the Rhˆone river system [J]. Chemical Geology, 1999, 159: 87-105.[15] Barth J A C, Veizer J. Carbon cycle in St. Lawrence aquatic ecosystems at Cornwall (Ontario),Canada: seasonal and spatial variations [J]. Chemical Geology, 1999, 159: 107-128.[16] Das A, Krishnaswami S, Bhattacharva S K. Carbon isotope ratio of dissolved inorganic carbon (DIC) in rivers draining the Deccan Traps, India: sources of DIC and their magnitudes[J]. Earth and Planetary Science Letters, 2005, 236(1/2): 419-429.[17] H´elie J F, Hillaier-Marcel C, Rondeau B. Seasonal changes in the sources and fluxes of dissolved inorganic carbon through the St. Lawrence River—isotopic and chemical constraint[J]. Chemical Geology, 2002, 186: 117-138.[18] Wachniew P, R´o˙za´nki K. Carbon budget of a mid-latitude, groundwater-controlled lake: isotopic evidence for the importance of dissolved inorganic carbon recycling [J]. Geochimica et Cosmochimica Acta, 1997, 61(12): 2453-2465.[19] Wang X F, Veizer J. Respiration-photosynthesis balance of terrestrial aquatic ecosystems, Ottawa area,Canada [J]. Geochimica et Cosmochimica Acta, 2000, 64(22): 3775-3786.[20] 喻元秀, 刘丛强, 汪福顺, 等. 乌江流域梯级水库中溶解无机碳及其同位素分异特征[J]. 科学通报,2008, 53(16): 1935-1941.[21] 喻元秀, 汪福顺, 王宝利, 等. 溶解无机碳及其同位素组成特征对初期水库过程的响应——以新建水库(洪家渡) 为例[J]. 矿物学报, 2009, 29(2): 268-274.[22] 李干蓉, 刘丛强, 陈椽, 等. 猫跳河流域梯级水库夏-秋季节溶解无机碳(DIC) 含量及其同位素组成的分布特征[J]. 环境科学, 2009, 30(10): 2891-2897.[23] 李铁松, 张桥英. 嘉陵江的起源及流域自然环境研究[J]. 四川师范学院学报(自然科学版), 1996,20(2): 105-108.[24] Atekwanae A, Krishnamurthy R V. Seasonal variations of dissolved inorganic carbon and 13C of surface waters: application of a modified gas evolution technique [J]. Journal of Hydrology,1998, 205(3/4): 265-278.[25] 鲍丽然, 李晓东, 刘小龙. 嘉陵江河水主要离子化学组成的时间和空间变化特征[J]. 水利水电科技进展, 2010, 30(4): 35-40.[26] 刘丛强. 生物地球化学过程与地表物质循环——西南喀斯特流域侵蚀与生源要素循环[M]. 北京: 科学出版社, 2007: 187-192.[27] 吴起鑫, 韩贵琳, 唐杨. 三峡水库坝前水体水化学及溶解无机碳时空分布特征[J]. 环境科学学报,2012, 32(3): 654-661. |