Research Status and Prospect of Sediment Flocculation in the Yangtze River
Received date: 2025-05-23
Revised date: 2025-07-31
Online published: 2025-09-22
The research on the flocculation of viscous sediment in the Yangtze River is of great significance for the study of sediment deposition laws and pollutant distribution within the basin. Based on the on-site flocculation observation data in the Yangtze River Basin, the spatio-temporal variation characteristics and main influencing factors of flocculation in the Yangtze River are analyzed and summarized. Obvious fine-grained sediment flocculation phenomena are observed in the Yangtze River Basin from the Three Gorges Reservoir Area to the Yangtze River estuary. During the flood season, the particle size of flocs decreases first and then increased along the way from the reservoir area to the estuary. During the flood and dry season, the particle size ranges of flocs in the reservoir area, the middle and lower reaches of the Yangtze River, and the Yangtze River estuary are 22-58 μm, 26-98 μm, and 40-130 μm, respectively. The sedimentation velocity of flocs in both flood and dry seasons is shown to be greater in the Yangtze River estuary area than in the main stream of the middle and lower reaches of the Yangtze River and the Three Gorges Reservoir Area. Among them, the sedimentation velocity of flocs in the main stream area of the middle and lower reaches of the Yangtze River decreases along the way during the dry season. The settling velocities of flocs in the reservoir area, the middle and lower reaches of the Yangtze River, and the Yangtze River estuary range from 0.13 to 0.61 mm/s, 0.21 to 0.62 mm/s, and 0.46 to 2.32 mm/s, respectively. The main influencing factors, action modes and thresholds of flocculation in each area are summarized. Looking ahead, research on sediment flocculation in the freshwater environment of the Yangtze River Basin should be strengthened, especially in the Three Gorges Reservoir and large reservoirs in the upper reaches of the Yangtze River, as well as important lakes such as Dongting Lake and Poyang Lake, to provide theoretical references for pollution control and ecological environment protection in the Yangtze River Basin.
GUO Chao , GONG Zhi-long . Research Status and Prospect of Sediment Flocculation in the Yangtze River[J]. Journal of Changjiang River Scientific Research Institute, 0 : 20250468 . DOI: 10.11988/ckyyb.20250468
| [1] |
柴朝晖. 粘性细颗粒泥沙絮凝机理及输移模型研究[D]. 武汉: 武汉大学, 2014.
|
| [2] |
李道季, 李军, 陈吉余, 等. 长江河口悬浮颗粒物研究[J]. 海洋与湖沼, 2000, (3): 295-301.
(
|
| [3] |
郭超, 何青. 长江中下游洪枯季泥沙絮凝研究[J]. 泥沙研究, 2014, (5): 59-64.
(
|
| [4] |
左书华, 杨春松, 付桂, 等. 长江口入海水沙通量变化及其影响分析[J]. 海洋地质前沿, 2022, 38(11): 56-64.
(
|
| [5] |
水利部长江水利委员会. 长江泥沙公报2023[R]. 武汉: 水利部长江水利委员会, 2024.
Changjiang Water Resources Commission. Changjiang Sediment Bulletin 2023[R]. Wuhan: Changjiang Water Resources Commission, 2024. ) (in Chinese)
|
| [6] |
李九发, 戴志军, 刘启贞, 等. 长江河口絮凝泥沙颗粒粒径与浮泥形成现场观测[J]. 泥沙研究, 2008, (3): 26-32.
(
|
| [7] |
张志忠. 长江口细颗粒泥沙基本特性研究[J]. 泥沙研究, 1996, (1): 67-73.
(
|
| [8] |
郭超, 何青, 郭磊城. 长江河口控制站泥沙絮凝特性研究[J]. 泥沙研究, 2016, (5): 60-65.
(
|
| [9] |
丁悌平, 高建飞, 石国钰, 等. 长江水中悬浮物含量与矿物和化学组成及其地质环境意义[J]. 地质学报, 2013, 87(5): 634-660.
(
|
| [10] |
简慧敏, 姚庆祯, 张经, 等. 长江流域常量元素的分布特征[J]. 长江流域资源与环境, 2010, 19(1): 93-97.
(
|
| [11] |
王琪, 于奭, 蒋萍萍, 等. 长江流域主要干/支流水化学特征及外源酸的影响[J]. 环境科学, 2021, 42(10): 4687-4697.
(
|
| [12] |
关许为, 陈英祖, 林以安, 等. 长江口泥沙絮凝体的现场显微观测[J]. 泥沙研究, 1992, (3): 54-59.
(
|
| [13] |
林以安, 李炎. 长江口絮凝聚沉特征与颗粒表面理化因素作用:Ⅰ悬浮颗粒絮凝沉降特征[J]. 泥沙研究, 1997, 22(1):42-48.
(
|
| [14] |
程江, 何青, 王元叶. 利用LISST观测絮凝体粒径、有效密度和沉速的垂线分布[J]. 泥沙研究, 2005, (1): 33-39.
(
|
| [15] |
唐建华. 长江口及其邻近海域粘性细颗粒泥沙絮凝特性研究[D]. 上海: 华东师范大学, 2007.
|
| [16] |
杨天, 杨世伦, 杨海飞, 等. 悬浮絮凝体特征及其影响因子的综合作用——以长江口内河槽和口门最大浑浊带为例[J]. 华东师范大学学报(自然科学版), 2017, (4): 149-159.
(
|
| [17] |
王诗妮, 蒋雪中, 何青. 长江口不同河段表层细颗粒泥沙絮凝特性[J]. 泥沙研究, 2017, 42(2): 47-53.
(
|
| [18] |
唐建华, 何青, 王元叶, 等. 长江口浑浊带絮凝体特性[J]. 泥沙研究, 2008, (2): 27-33.
(
|
| [19] |
|
| [20] |
陈锦山, 何青, 郭磊城. 长江悬浮物絮凝特征[J]. 泥沙研究, 2011, (5): 11-18.
(
|
| [21] |
李云中, 江玉姣. 三峡水库坝前泥沙絮凝沉降实证分析[J]. 水利水电快报, 2019, 40(2): 62-65,72.
(
|
| [22] |
李文杰, 张凌越, 杨胜发, 等. 三峡库区泥沙絮凝临界条件现场测量[J]. 水科学进展, 2019, 30(1): 76-83.
(
|
| [23] |
何芳娇, 吉祖稳, 王党伟, 等. 三峡水库泥沙絮凝特征及影响因素分析[J]. 人民长江, 2016, 47(14): 31-35,45.
(
|
| [24] |
程江, 何青, 夏小明. 长江口徐六泾悬浮细颗粒泥沙絮凝体特性[J]. 海洋与湖沼, 2007, (4): 304-313.
(
|
| [25] |
郭超. 粘性泥沙絮凝沉降过程与控制机制研究[D]. 上海: 华东师范大学, 2018.
|
| [26] |
李文杰, 马浩平, 杨胜发, 等. 三峡库区细颗粒泥沙淤积及一维数值模拟研究[J]. 应用基础与工程科学学报, 2021, 29(2): 251-260.
(
|
| [27] |
郭超, 何青, 郭磊城, 等. 紊动对黏性细颗粒泥沙絮凝沉降影响的试验研究[J]. 泥沙研究, 2019, 44(2): 18-25.
(
|
| [28] |
柴朝晖, 方红卫, 王茜, 等. 水流和电解质对黏性泥沙絮凝沉降影响试验[J]. 水科学进展, 2017, 28(2): 285-292.
(
|
| [29] |
万远扬, 吴华林, 顾峰峰. 长江口细颗粒泥沙沉降速度室内试验研究[J]. 人民长江, 2014, 45(1): 98-101.
(
|
| [30] |
关许为, 陈英祖, 杜心慧. 长江口絮凝机理的试验研究[J]. 水利学报, 1996, (6): 70-74,80.
(
|
| [31] |
张宇卓, 张根广, 李青, 等. 基于电解质浓度参数的泥沙沉速公式研究[J]. 泥沙研究, 2020, 45(3): 1-7,45.
(
|
| [32] |
王保栋. 河口细颗粒泥沙的絮凝作用[J]. 黄渤海海洋, 1994, (1): 71-76.
(
|
| [33] |
刘启贞, 李九发, 徐灿华, 等. 盐度和腐殖酸共同作用下的长江口泥沙絮凝过程研究[J]. 海洋学报(中文版), 2008, (3): 140-147.
(
|
| [34] |
|
| [35] |
刘洁, 张智超, 李霞, 等. 三峡水库微塑料与悬沙的聚集特性及作用机制[J]. 湖泊科学, 2025, 37(1): 149-158.
(
|
| [36] |
|
| [37] |
丁武泉, 李强, 李航. 表面电位对三峡库区细颗粒泥沙絮凝沉降的影响[J]. 土壤学报, 2010, 47(4): 698-702.
(
|
/
| 〈 |
|
〉 |