| 滦河下游河道及三角洲地貌的近期演化 |
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| 引用本文： | 黎刚,殷勇.滦河下游河道及三角洲地貌的近期演化[J].地理研究,2010,29(9):1606-1615. |
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| 作者姓名： | 黎刚 殷勇 |
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| 作者单位： | 南京大学海岸与海岛开发教育部重点实验室,南京,210093 |
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| 基金项目： | 国家自然科学基金项目 |
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| 摘 要： | 自20世纪80年代滦河上中游大型水库的修建以及下游农业用水量的激增,滦河下游水沙锐减。至桃林口水库修建后,滦河入海水量减至5.96亿m3/a,下泻泥沙减至2.43万t/a,滦河断流趋势日益严重。本文选择1979年至2007年多期遥感影像,探讨在大规模水资源开发影响下滦河下游河道及三角洲地貌的演化。结果表明:20世纪90年代以后滦河下游水沙量的大幅减少直接导致下游河道萎缩。由于上游水库的拦截以及下游河道搬运能力下降,入海泥沙量大幅减少几至断绝,致使滦河三角洲主汊道1984年改道后并未发育形成新的三角洲叶瓣,入海汊道由多汊萎缩为单汊,三角洲逐渐转入全面侵蚀阶段。
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| 关 键 词： | 水库 断流 滦河河道 三角洲 |
| 收稿时间： | 2010-01-05 |
| 修稿时间： | 2010-03-24 |
Recent geomorphological evolution of downstream channel and delta of Luanhe River |
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| LI Gang,YIN Yong.Recent geomorphological evolution of downstream channel and delta of Luanhe River[J].Geographical Research,2010,29(9):1606-1615. |
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| Authors: | LI Gang YIN Yong |
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| Institution: | Key Laboratory of Coast and Island Development of the Ministry of Education, Nanjing University, Nanjing 210093, China |
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| Abstract: | Big dams built across Luanhe River since the 1980s caused great decrease of freshwater and sediment discharges. After Taolinkou Reservoir was built in 1998, the average freshwater decreased to 596×106 m3/a, and the sediment discharges reduced to 24.3×103 t/a. The period of zero flow has prolonged in recent years. Based on remote sensing images from 1979 to 2007, the hydrological changes of the Luanhe River have greatly influenced the development of downstream channel and delta. In a few years after the construction of Panjiakou and Daheiting reservoirs, the downstream channel was cut deeply and eroded widely. But since the 1990s, huge water transfer and irrigation water from the Luanhe River has made the flow in the lower Luanhe River decrease greatly. According to the remote sensing images of 1991, 2000 and 2004, the width of the lower channel became obviously narrower due to the reduction of the river flow. The main channel was 3 to 5 km wide around Macheng in 1979, while the width decreased to less than 100 m in 2004. Although the curving cut-off took place in 1991-2000, the migration of the channel has been limited within the old channel. After 2000, the zero flow happened frequently and the curving cut-off almost ceased. Most point bars inside the Luanhe artificial levee have been reclaimed for farmlands and woodlands. In recent years, the frequent zero flow has deteriorated the river water quality. Based on the remote sensing images of 1979, 1991, 2000 and 2007, the main branch of the Luanhe Estuary in 1979 was abandoned in 1984 and changed its path to Xiaotaiwan. The new main branch kept the single path from then on. Because of the great decrease of the peak flood flow, the width of the estuarine branch became narrower from 1979 to 2007 and the width has decreased to less than 100 m recently. Since the Daheiting and Panjiakou reservoirs were built in 1984, the Luanhe Delta front has stopped growing because most sediment was trapped by the dams. Two segments of the Luanhe Delta were eroded severely. One segment was located around Puochuanmen and the average erosion rate of the sand spit was 29 m/a in recent 28 years. The other was the south flank of the Luanhe Delta, and the average recession rate was 30 m/a in 1979-1991, 24 m/a in 1991-2000, and 27 m/a in 2000-2007, respectively. The severity of recent deltaic erosion was related to the history of the abandoned river branches. |
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| Keywords: | reservoir zero flow downstream channel of the Luanhe River the Luanhe Delta |
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