盐度影响沉积物抗侵蚀性的环形水槽试验研究

代馨楠; 贾永刚; 张少同; 张淑玉; 张皓清; 单红仙

doi:10.16562/j.cnki.0256-1492.2019032401

盐度影响沉积物抗侵蚀性的环形水槽试验研究

1.
中国海洋大学环境科学与工程学院，青岛 266100

2.
山东省海洋环境地质工程重点试验室，青岛 266100

基金项目: 国家自然科学基金“黄河口海域盐度变化对入海泥沙沉降与固结及侵蚀过程影响研究”（41372287），“波致渗流对粉质土海床侵蚀影响的定量评价方法研究”（41807229），“基于现场原位观测的黄河水下三角洲海底滑坡启动过程与控制因素研究”（41877223）

详细信息

作者简介: 代馨楠（1994—），女，硕士研究生，主要从事河口沉积物动力响应方面的研究工作，E-mail：daixinnan0110@163.com

通讯作者: 单红仙（1965—），女，教授，主要从事河口海岸带地质灾害的研究工作，E-mail：hongxian@ouc.edu.cn

中图分类号: P736.5

收稿日期: 2019-03-24

修回日期: 2019-11-26

刊出日期: 2020-06-25

Influence of salinity on sediment erosion-resistance: evidence from annular flume studies

1.
Environmental Geotechnical Engineering Institute, Ocean University of China, Qingdao 266100, China

2.
Shandong Provincial Key Laboratory of Marine Environment and Geological Engineering, Ocean University of China, Qingdao 266100,China

More Information

Corresponding author: SHAN Hongxian, hongxian@ouc.edu.cn

Received Date: 24 March 2019

Revised Date: 26 November 2019

Publish Date: 25 June 2020

摘要

摘要:
黄河口海域盐度变化受入海径流量、海洋动力条件及气候等影响，时空变化显著。河口区盐度场的变化不仅会影响营养盐、污染物的运输，还会改变入海泥沙的沉降及固结特性，进一步影响沉积物的抗侵蚀性。为研究不同盐度环境对沉积物抗侵蚀性的影响，选用黄河三角洲沉积物进行室内循环水槽试验，模拟不同盐度条件下沉积物发生侵蚀再悬浮的过程。研究得出在本研究区盐度0～36‰范围内，黄河口细颗粒沉积物临界切应力值存在明显差异，变化范围为0.055 6～0.080 6 Pa。固结程度相同，沉积物临界切应力随盐度的增加呈对数增长特征，在盐度小于9‰的条件下，黄河口细颗粒沉积物抗侵蚀性受盐度环境变化的影响尤为明显；固结程度不同，随着固结时间的推移，盐度环境的增加对沉积物临界切应力的促进作用减小。
- 盐度 /
- 细粒沉积物 /
- 侵蚀 /
- 临界切应力
Abstract:
The temporal and spatial change of salinity field in the Yellow River estuary is affected by runoff, ocean dynamics and climate. It influences not only the transportation of nutrients and pollutants, but also the deposition and consolidation of sediments, and so that the erosion-resistance of the sediments. In order to study the effect of salinity on the erosion-resistance of sediments, the sediments from the Yellow River estuary were used to carry out in-door annular flume experiments to simulate the process of sediment erosion and resuspension under different salinity conditions. The results show that the critical shear stress of fine sediments in the Yellow River estuary varies significantly in the salinity range of 0～36‰, and may be up to 0.055 6～0.080 6 Pa. Under same consolidation degree, the critical shear stress is logarithmically proportional to the increase in salinity, especially the salinity is less than 9‰. Under different consolidation degree, however, the effect of salinity on the critical shear stress of sediments decreases with the consolidation time.
- salinity /
- fine-grained sediments /
- erosion /
- critical shear stress

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图 1 黄河水下三角洲底层盐度场分布（2017.07）

Figure 1.

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图 2 环形水槽（a）及水槽试验系统（b）土槽侧视图，冲刷过程产生凹坑（c）

Figure 2.

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图 3 沉积物超孔隙水压力的消散曲线

Figure 3.

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图 4 不同盐度条件下悬浮泥沙浓度随近底切应力的时间演变图（5 h）

Figure 4.

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图 5 不同盐度条件下悬浮泥沙浓度随近底切应力的时间演变图（24 h）

Figure 5.

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图 6 不同盐度环境下近底切应力与悬浮泥沙浓度关系（5 h）

Figure 6.

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图 7 不同盐度环境下近底切应力与悬浮泥沙浓度关系（24 h）

Figure 7.

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图 8 沉积物临界切应力分布图

Figure 8.

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表 1 不同盐度环境近底切应力分布

Table 1. Near-bottom shear stress distribution under different salinity conditions

阶段	档位	流速/（m·s⁻¹）	盐度/‰	水体密度/（g·cm⁻³）	切应力/Pa
Ⅰ	1	0.16	0	1.000	0.029 2
			4	1.003	0.029 3
			9	1.007	0.029 4
			18	1.014	0.029 6
			27	1.021	0.029 8
			36	1.028	0.030 0
Ⅱ	2	0.21	0	1.000	0.050 3
			4	1.003	0.050 3
			9	1.007	0.050 6
			18	1.014	0.050 9
			27	1.021	0.051 3
			36	1.028	0.051 6
	3	0.22	0	1.000	0.055 2
			4	1.003	0.055 3
			9	1.007	0.055 5
			18	1.014	0.055 9
			27	1.021	0.056 3
			36	1.028	0.056 7
Ⅲ	4	0.28	0	1.000	0.089 4
			4	1.003	0.089 8
			9	1.007	0.090 6
			18	1.014	0.091 2
			27	1.021	0.091 5
			36	1.028	0.091 8
	5	0.29	0	1.000	0.095 9
			4	1.003	0.096 2
			9	1.007	0.096 5
			18	1.014	0.097 1
			27	1.021	0.097 8
			36	1.028	0.098 5

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表 2 不同盐度条件下沉积物临界切应力 (5 h)

Table 2. Critical shear stress of sediments under different salinity conditions (5 h)

盐度/‰	0	4	9	18	27	36
临界侵蚀切应力/Pa	0.055 6	0.065 7	0.067 0	0.068 3	0.068 9	0.069 3

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表 3 不同盐度条件下沉积物临界切应力 (24 h)

Table 3. Critical shear stress of sediments under different salinity conditions (24 h)

盐度/‰	0	4	9	18	27	36
临界侵蚀切应力/Pa	0.069 5	0.077 9	0.079 5	0.080 1	0.080 3	0.080 6

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