[1] 王开荣.黄河调水调沙对河口及其三角洲的影响和评价[J].泥沙研究,2005(6):29-33.
[2] Yang Z S,Milliman J D,Liu J P,el al.Yellow River's water and sediment discharge decreasing steadily[J].EOS,1998,79:589-592.
[3] Xu J.Sediment flux to the sea as influenced by changing human activities and precipitation:example of the Yellow River[J].China Endronmental Management,2005,31(8):328-341.
[4] 王厚杰,杨作升,毕乃双.2005年黄河调水调沙期间河口入海主流的快速摆动[J].科学通报,2005,50(23):2656-2662.
[5] Yang Z S,Wang Z X,Zhang A F,et al.Distribution and movement of suspended matter in Sumlner in Laizhou Bay,The Gulf of Bohai[J].J Ocean Uni Qingdao,1989,4(1):49-66.
[6] 江文胜,王厚杰.莱州湾悬浮泥沙分布形态及其与底质分布的关系[J].海洋与湖沼,2005,36(2):97-103.
[7] Jiang W S,Pohlmann T.A modeling study of SPM transport in the Bohai Sea[J].J Marine System,2000,24(3/4):175-200.
[8] 范兆木,郭永盛.黄河三角洲沿岸遥感动态分析图集[M].北京:海洋出版社,1992.123.
[9] 叶超青.黄河流域环境演变与水沙运行规律研究[M].济南:山东科技出版社,1994.220.
[10] 杨守业,李从先.长江与黄河沉积物元素组成及地质背景[J].海洋地质与第四纪地质,1999,19(2):19-26.
[11] 胡国华,赵沛伦,肖翔群.黄河泥沙特性及对水环境的影响[J].水利水电技术,2004,35(8):17-20.
[12] 范德江,杨作升,王文正.长江、黄河中碳酸盐组成及差异[J].自然科学进展,2002,12(1):60-64.
[13] 文启忠.中国黄土地球化学[M].北京:科学出版社,1988.28.
[14] 张龙军,张向上,王晓亮,等.黄河口有机碳的时空输运特征及其影响因素的分析[J].水科学进展,2007,18(5):674-682.
[15] Cauwet G,Mackenzie F T.Carbon inputs and distribution in estuaries of turbid rivers:the Yangtze and Yellow rivers(Chin)[J].Marine Chemistry,1993,43-235-246.
[16] Zhang S,Gan W B,Ittekkot V.Organic matter in large turbid rivers:the Huanghe and its estuary[J].Marine Chemistry,1992,38:53-68.
[17] 蔡德陵.黄河与长江河口区有机碳的同位素地球化学[A].张经.中国主要河口的生物地球化学研究[C].北京:海洋出版社,1996.160-187.
[18] Riley J P,Skirrow G,Parsons T R.Particulate organic carbon in the sea[J].Chemical Oceanography,1975,2:365-383.
[19] 万修全,鲍献文,吴德星,等.渤海夏季潮致-风生-热盐余流的数值诊断计算[J].海洋与湖沼,2004,35(1):41-44.