关于黄河与河套古湖河湖关系演变的假说性分析

荣朝和

北京交通大学学报(社会科学版) ›› 2024, Vol. 23 ›› Issue (3) : 161-174.

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北京交通大学学报(社会科学版) ›› 2024, Vol. 23 ›› Issue (3) : 161-174.
专题研究

关于黄河与河套古湖河湖关系演变的假说性分析

  • 荣朝和
作者信息 +

A Hypothetical Analysis of the Evolution of the River-lake Relationship between the Yellow River and Ancient Hetao Lake: The Enlightenment to the Ecological Governance of the Inner Mongolia Section of the Yellow River

  • RONG Chao-he
Author information +
文章历史 +

摘要

黄河曾经在流经河套盆地过程中形成吉兰泰、乌兰布和、巴彦淖尔、呼包4个古湖,且在高湖面时期连成统一的“河套古大湖”,其后4湖分离并分别演绎了自己的河湖关系。在研习前人相关成果基础上,通过建立整体假说性解释框架,试图按照历史顺序与逻辑顺序统一的要求对该河段河湖关系的演变过程进行重建,并为与之相关的生态系统的治理提供借鉴。研究认为:主河道构建是黄河主动实施填湖、建堤、造槽并“甩湖”的过程与结果;冲积扇是黄河填湖的主要模式,而冲积扇顶附近凸起则是湖口淤塞、移动并最终筑成黄河自然堤的主要原因;巴彦木仁与磴口两地控制点对形成鄂尔多斯一侧黄河主河道起到了关键性作用;黄河西派在高湖面期间从巴彦木仁湖口注入吉兰泰-乌兰布和古湖,与从北面入湖的黄河水共同促成贺日木西尼古砂嘴及其延伸砂脊生长,并在低湖面期将这两个湖分离。基于对所述黄河历史过往的认识,须尽可能立足高效集成利用有限水资源这一观念,将减灾与适度重造沿河湖泊和绿洲结合,营建可持续的内蒙古段黄河生态体系。

Abstract

In the process of flowing through the Hetao Basin, the Yellow River once formed four ancient lakes: Jilantai Lake, Ulanbuhe Lake, Bayannur Lake and Huhe-Baotou Lake. In the period of high lake level, the four lakes formed a unified “Ancient Hetao Lake”, after that the four lakes separated and developed their own river-lake relationship respectively. This paper fully studies the previous achievements and establishes an overall hypothesis explanation framework to reconstruct as far as possible the evolution process of the river-lake relationship in Inner Mongolia section, which is unified in historical and logical order, and provides reference for the governance of related ecosystems. The study shows the following findings: The construction of the main river channel was the process and result of the proactive lake filling, dike building, trough building and “getting rid of lake” by Yellow River; Alluvial fans were the main mode of lake filling for the Yellow River, and the bulges near the apex of alluvial fans were the main cause for lake entrance silting and moving and the final formation of the natural dike of the Yellow River; The two control points, Bayanmuren and Dengkou, play key roles in forming the main channel of the Yellow River on the Ordos side; During the period of high lake level, the Western Flow of the Yellow River from the lake mouth of Bayanmuren into the Jilantai-Ulanbuhe Lake, with the river water from the north to the lake together, contributed to the growth of the ancient Herimusini sand spit and its extension sand ridge, and once separated the two latter lakes during the period of low lake level. In view of the understanding of the historical past of Yellow River, we should, based on the concept of efficient and integrated use of limited water resources where possible, build a sustainable Yellow River ecosystem in Inner Mongolia by combining disaster mitigation with the moderate reconstruction of lakes and oases along the river.

关键词

黄河 / 内蒙古河段 / 河套古湖 / 河湖关系 / 构建主河道 / 生态治理

Key words

Yellow River / Inner Mongolia section / ancient Hetao Lake / river-lake relationship / construct the main channel of river / eco-governance

引用本文

导出引用
荣朝和. 关于黄河与河套古湖河湖关系演变的假说性分析[J]. 北京交通大学学报(社会科学版). 2024, 23(3): 161-174
RONG Chao-he. A Hypothetical Analysis of the Evolution of the River-lake Relationship between the Yellow River and Ancient Hetao Lake: The Enlightenment to the Ecological Governance of the Inner Mongolia Section of the Yellow River[J]. Journal of Beijing Jiaotong University(Social Sciences Edition). 2024, 23(3): 161-174
中图分类号: P53    X321   

参考文献

1 李建彪,冉勇康,郭文生. 河套盆地托克托台地湖相层研究[J]. 第四纪研究,2005,(5).
2 陈发虎,范育新,春喜,等. 晚第四纪“吉兰泰-河套”古大湖的初步研究[J]. 科学通报,2008,(10).
3 陈发虎,范育新,MadseD. B.,等. 河套地区新生代湖泊演化与“吉兰泰-河套”古大湖形成机制的初步研究[J]. 第四纪研究,2008,(5).
4 袁宝印,王振海. 青藏高原隆起与黄河地文期[J]. 第四纪研究,1995,(4).
5 谭其骧. 何以黄河在东汉以后会出现一个长期安流的局面[J]. 学术月刊,1962,(2).
6 侯仁之,俞伟超. 烏兰布和沙漠的考古发現和地理环境的变迁[J]. 考古,1973,(2).
7 耿侃,胡春元,刘佳. 吉兰泰地区第四纪湖泊的演变[J]. 干旱区资源与环境,1989,(2).
8 胡春元. 试论吉兰泰盐湖的发育与资源保护问题[J]. 内蒙古林学院学报,1998,(2).
9 贾铁飞,石蕴琮,银山. 乌兰布和沙漠形成时代的初步判定及意义[J]. 内蒙古师大学报(自然科学汉文版),1997,(3).
10 贾铁飞,赵明,包桂兰,等. 历史时期乌兰布和沙漠风沙活动的沉积学记录与沙漠化防治途径分析[J]. 水土保持研究,2002,(3).
11 牛俊杰,赵淑贞,任世芳,等. 历史时期乌兰布和沙漠北部的环境变迁[J]. 中国沙漠,1999,(3).
12 李并成. 我国历史上的沙漠化问题及其警示[J]. 求是,2002,(15).
13 春喜,陈发虎,范育新,等. 乌兰布和沙漠的形成与环境变化[J]. 中国沙漠,2007,(6).
14 范育新,陈发虎,范天来,等. 乌兰布和北部地区沙漠景观形成的沉积学和光释光年代学证据[J]. 中国科学,2010,(7).
15 王娜,春喜. 乌兰布和沙漠晚第四纪以来环境演化研究进展[J]. 中国沙漠,2022,(1).
16 林旭,刘静,刘海金.黄河形成于何时?[J/OL].地球科学,(2023-09-06)[2023-12-15]. http://kns.cnki.net/kcms/detail/42.1874.P.20230905.1644.004.html.
17 春喜. 晚第四纪吉兰泰盐湖古湖面与环境变化研究[D]. 兰州:兰州大学资源环境学院,2006.
18 孙洋. 吉兰泰盐湖DEM模型与晚第四纪湖泊演化初步研究[D]. 兰州:中国科学院寒区旱区环境与工程研究所,2006.
19 杨丽萍. 基于遥感与DEM的“吉兰泰—河套”古大湖重建研究[D]. 兰州:兰州大学资源环境学院,2008.
20 FAN Y X, CHEN F H, WEI G X, et al. Potential Water Sources for Late Quaternary Megalake Jilantai-Hetao, China, Inferred from Mollusk Shell 87Sr/ 86Sr Ratios[J]. Journal of Paleolimnology ,2010,43(3):577-587.
21 FAN Y X, WANG Y D, MOU X S, et al. Environmental Status of the Jilantai Basin, North China, on the Northwestern Margin of the Modern Asian Summer Monsoon Domain During Marine Isotope Stage 3[J]. Journal of Asian Earth Sciences, 2017,147:178-192.
22 范天来,范育新,魏国孝. 河套盆地西山咀凸起区湖相地层的发现及其测年[J]. 地理学报,2011,(5).
23 李国强. 乌兰布和沙漠钻孔岩芯记录的释光年代学和晚第四纪沙漠-湖泊演化研究[D]. 兰州:兰州大学资源环境学院,2012.
24 张复. 吉兰泰盆地MIS 3阶段沉积环境及生态环境研究[D].兰州:兰州大学地质科学与矿产资源学院,2015.
25 赵希涛,杨艳,贾云丽,等. 论晚期共和古湖时代、演化过程及其与地壳运动和黄河发育的关系[J]. 地球学报,2021,(4).
26 吴加敏,王润生,姚建华. 黄河银川平原段河道演变的遥感监测与研究[J]. 国土资源遥感,2006,(4).
27 陈耳东. 河套段黄河变迁史话[J]. 内蒙古水利,1998,(1).
28 春喜,陈发虎,范育新,等. 乌兰布和沙漠腹地古湖存在的沙嘴证据及环境意义[J]. 地理学报,2009,(3).
29 春喜,范育新,夏敦胜,等. MIS 3阶段吉兰泰古湖演化的初步研究[J]. 干旱区资源与环境,2008,(12).
30 FRANK K J, RANDALL J S. Paleowind 11,000 BP directions derived from lake spits in Northern Michigan[J]. Geomorphology, 2001, 38: 1-18.
31 马燕. 水权与地权:清代以来后套地区的土地控制与权力体系[J]. 宁夏社会科学,2020,(4).
32 梁勇,李建国,田振新. 内蒙古河套灌区:2022年黄河分凌及乌梁素海生态补水双线并行[N]. 中国水利报,2022-03-16
33 巴彦淖尔市人民政府办公室关于印发《巴彦淖尔市“十四五”水安全保障规划》的通知[EB/OL].(2022-07-01)[2023-12-15]. https://www.bynr.gov.cn/xxgk/zfxxgklm/xxgknr/ghjh_1/zxgh/202211/t20221110_488849.html

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