衡水地区咸水层沉积物粒度及氘氧同位素的古气候指示

牛宏; 梁杏; 李静; 马斌; 葛勤

doi:10.3799/dqkx.2016.041

衡水地区咸水层沉积物粒度及氘氧同位素的古气候指示

doi: 10.3799/dqkx.2016.041

牛宏^1,,
梁杏^1,2, ,,
李静¹,
马斌¹,
葛勤¹

1.
中国地质大学环境学院，湖北武汉 430074
2.
中国地质大学湿地演化与生态恢复湖北省重点实验室，湖北武汉 430074

基金项目:

国家自然科学基金 41272258

国家自然科学基金 U1403282

国家重点基础研究发展计划“973”项目 2010CB428802

详细信息

作者简介:
牛宏(1988-)，男，博士研究生，主要研究水文地质方向. E-mail: nrg880607@126.com

通讯作者:
梁杏, E-mail: xliang@cug.edu.cn

中图分类号: P532
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出版历程
- 收稿日期: 2015-09-13
- 刊出日期: 2016-03-15

Paleoclimate Instruction of Sediment Grain Size and Deuterium-Oxygen Isotope in Saline Stratum of Hengshui

Niu Hong^1
,,
Liang Xing^{1,2
, ,},
Li Jing¹,
Ma Bin¹,
Ge Qin¹

1.
School of Environmental Studies, China University of Geosciences, Wuhan 430074, China
2.
Key Laboratory of Wetland Evolution & Ecological Restoration, China University of Geosciences, Wuhan 430074, China

摘要

摘要: 衡水地区的咸水层特征一直备受关注.为了探讨咸水层分布区的沉积环境与咸水形成期的古气候特征，利用钻孔(深度130 m)采集了衡水地区咸水层沉积物，进行了沉积物粒度和粘性土孔隙水氘氧同位素测试.沉积物粒度标准偏差显示，剖面上由深至浅，沉积时期水动力呈由弱到强再到弱的变化趋势，其中水动力强段为90~65 m，为厚层砂砾层.孔隙水TDS和δ¹⁸O特征显示在6 m以上受到大气降水和人类活动的影响，并且主要是以淡水灌溉影响为主.剖面上粘性土孔隙水的δ¹⁸O在130~90 m平均值为-11.5‰，65~29 m平均值为-12.1‰，23~0 m为-10.6‰，而下部淡水含水层地下水δ¹⁸O为-9.8‰，上部咸水含水层地下水δ¹⁸O为-8.2‰，粘性土孔隙水δ¹⁸O明显偏负于含水层的地下水，反映保存记录了古气候信息.130~90 m，δ¹⁸O先增大后减小反映温度先升高后降低；65~29 m，δ¹⁸O反映温度偏低的气候特征；23~0 m，δ¹⁸O相对比较稳定，总体偏正，反映了全新世为一个相对较为稳定但较高的温度.
- 衡水 /
- 沉积物粒度 /
- 粘性土孔隙水 /
- 氘氧同位素 /
- 古气候
Abstract: The characteristics of saline stratum in Hengshui have always been concerned. In order to discuss the paleoenvironment and the paleoclimate in Hengshui area, grain size and pore water stable isotope (δD, δ¹⁸O) of clay collected from Hengshui saline stratum(thickness of 130 m) by drilling were analyzed. The standard deviation of sediment grain size shows that the hydrodynamic strength changed from weak to strong and then to weak, there is a deep gravel layer in 90-65 m, which reflects a strong hydrodynamic strength and a humid clime. The TDS and δ¹⁸O reflect the affect of atmospheric precipitation and human irrigation above 6 m, specially for the human irrigation. The mean value of δ¹⁸O at depth of 130-90 m is -11.5‰, and it is -12.1‰ and -10.6‰ at depth of 65-29 m and 23-0 m. The δ¹⁸O of aquifer at 90-65 m is -9.8‰, and -8.2‰ of 29-23 m. The δ¹⁸O of clay pore water is negative compared with the aquifer groundwater, reflecting that the clay pore water saves paleoenvironment information. The δ¹⁸O at depth of 65-29 m firstly increases and than decreases reflecting the temperature firstly increases and than decreases; the δ¹⁸O at depth of 65-29 m reflects a low temperature; the δ¹⁸O at depth of 23-0 m is relatively stable, but is positive overall, indicating a warm climate in Holocene.
- Hengshui /
- sediment grain size /
- clay pore water /
- deuterium-oxygen isotopes /
- paleoclimate

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图 1 河北平原分区及钻孔位置

据张人权等(2013)

Fig. 1. Study area and locations of the drilling

下载: 全尺寸图片幻灯片

图 2 河北平原地下水流系统示意图

据张之淦(1987)；A.扇地局部水流系统；B.浅层局部水流系统；C.区域水流系统

Fig. 2. The schematic map of groundwater flow systems in Hebei Plain

下载: 全尺寸图片幻灯片

图 4 粘性土孔隙水各参数随深度变化

五角星代表本次所测得的含水层地下水δ¹⁸O值，空心三角形和圆圈表示处于含水层中的粘性土孔隙水δ¹⁸O

Fig. 4. Parameters of clay pore water vary with depth

下载: 全尺寸图片幻灯片

图 3 沉积物粒度参数随深度变化

平均粒径上的误差棒长度表示了标准偏差的相对大小

Fig. 3. Parameters of sediment grain size vary with depth

下载: 全尺寸图片幻灯片

表 1 粘性土孔隙水δ¹⁸O、δD

Table 1. δ¹⁸O and δD of clay pore water

深度(m)	δD‰	δ¹⁸O‰
0.5	-66.8	-8.9
0.8	-68.3	-9.2
1.5	-71.1	-9.4
2.0	-65.7	-8.8
2.5	-78.1	-10.4
3.0	-77.1	-10.3
3.5	-92.4	-12.6
4.0	-70.1	-9.4
4.5	-93.6	-12.5
5.0	-69.8	-9.5
6.0	-85.8	-11.9
7.0	-86.8	-11.6
8.0	-83.3	-11.0
9.0	-93.5	-12.2
10.0	-77.4	-10.5
11.0	-65.9	-8.9
12.0	-93.5	-12.6
13.0	-85.9	-11.7
15.0	-77.3	-10.4
16.0	-71.1	-9.0
19.0	-73.6	-9.9
20.0	-93.6	-12.6
21.0	-82.6	-10.9
22.0	-70.3	-9.7
24.0	-91.5	-12.0
25.0	-89.3	-11.8
27.0	-68.9	-9.1
29.0	-80.8	-10.8
30.0	-101.9	-13.1
31.0	-93.4	-12.2
32.0	-87.9	-11.8
33.0	-76.9	-9.9
34.0	-107.8	-14.6
35.1	-75.7	-9.9
39.0	-97.2	-13.2
40.0	-74.2	-9.8
41.0	-96.7	-13.0
43.0	-90.7	-11.8
44.0	-86.1	-11.7
45.0	-84.7	-11.2
46.0	-90.3	-12.0
47.0	-95.3	-12.6
49.0	-92.1	-12.2
51.0	-79.6	-10.3
52.0	-85.7	-11.1
53.0	-96.4	-12.2
54.0	-102.8	-13.8
55.0	-86.3	-11.3
56.0	-96.0	-12.8
57.0	-96.2	-12.6
58.0	-80.3	-10.8
58.8	-88.3	-11.9
60.0	-100.0	-13.1
61.0	-104.7	-13.8
62.0	-87.1	-12.2
63.0	-90.0	-12.1
64.0	-104.5	-14.0
65.0	-88.1	-12.0
83.0	-92.3	-12.5
91.0	-94.7	-12.8
92.0	-86.7	-11.4
93.0	-91.7	-11.7
94.0	-86.1	-11.3
95.0	-95.9	-12.5
99.0	-84.7	-10.5
100.0	-88.1	-10.7
101.0	-97.6	-12.5
102.0	-90.9	-11.7
103.0	-86.4	-11.0
104.0	-94.1	-12.3
105.0	-86.8	-11.4
106.0	-80.7	-10.6
109.0	-81.0	-10.6
110.0	-87.4	-11.4
111.0	-84.6	-11.2
112.0	-82.0	-10.7
113.0	-88.9	-11.9
114.0	-83.7	-11.0
115.0	-86.3	-11.5
117.2	-82.6	-10.9
118.0	-96.7	-13.3
119.0	-84.5	-11.6
120.0	-83.5	-11.3
123.0	-84.4	-11.5
124.0	-82.5	-11.2
125.0	-87.0	-11.9
129.3	-86.8	-11.7

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