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1.北京工业大学 城市与工程安全减灾教育部重点实验室,北京 100124
2.南京工业大学 岩土工程研究所,南京 210009
LIANG Ke (1991- ), PhD, main research interest: soil dynamics, E-mail: liangk91@163.com.
Received:27 July 2022,
Published:25 December 2023
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梁珂,岳冲,周正龙等.考虑级配影响的珊瑚砂最大动剪切模量试验研究[J].土木与环境工程学报,2023,45(06):95-103.
LIANG Ke,YUE Chong,ZHOU Zhenglong,et al.Small-strain shear modulus prediction model related to grain gradation of coral sand[J].Journal of Civil and Environmental Engineering,2023,45(06):95-103.
梁珂,岳冲,周正龙等.考虑级配影响的珊瑚砂最大动剪切模量试验研究[J].土木与环境工程学报,2023,45(06):95-103. DOI: 10.11835/j.issn.2096-6717.2022.121.
LIANG Ke,YUE Chong,ZHOU Zhenglong,et al.Small-strain shear modulus prediction model related to grain gradation of coral sand[J].Journal of Civil and Environmental Engineering,2023,45(06):95-103. DOI: 10.11835/j.issn.2096-6717.2022.121.
对不同级配的南沙岛礁珊瑚砂进行共振柱试验,测试不同孔隙比
e
的珊瑚砂在20~300 kPa围压下的最大动剪切模量
G
0
,分析不均匀系数
C
u
、平均粒径
d
50
和细粒含量
F
c
对珊瑚砂
G
0
的影响,并建立珊瑚砂的
G
0
经验模型。结果表明:珊瑚砂的孔隙比
e
普遍大于陆源砂砾土;同一有效围压
σ
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https://html.publish.founderss.cn/rc-pub/api/common/picture?pictureId=50179491&type=
1.18533325
4.14866638
下,珊瑚砂的
G
0
-
e
曲线随
C
u
的增大而降低,随
d
50
的增大而升高,以
F
c
≈20%为界,随
F
c
的增大先降低后缓慢升高;陆源砂砾土的
G
0
经验模型将低估珊瑚砂的
G
0
值;
F
c
对
G
0
影响的本质是不同细粒含量的珊瑚砂具有不同的
C
u
和
d
50
,
C
u
和
d
50
对
G
0
的影响隐含了
F
c
对
G
0
的影响。基于Hardin模型给出考虑
C
u
、
d
50
影响的珊瑚砂
G
0
预测模型,并引入修正系数
A'
,以考虑颗粒类型等复杂因素的综合影响,采用不同海洋珊瑚砂的试验数据对
G
0
预测模型进行验证。
A series of resonant column tests were conducted on coral sand taken from the Nansha Islands
South China Sea with different grain gradations. The small-strain shear modulus
G
0
of the coral sands with various void ratio
e
with the confining stress of 20~300 kPa was obtained. The influence of coefficients of uniformity
C
u
mean particle size
d
50
and fines content
F
c
on
G
0
of coral sand was investigated
and the
G
0
formulation for coral sand was established. For the constant effective confining pressure
σ
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https://html.publish.founderss.cn/rc-pub/api/common/picture?pictureId=50179496&type=
https://html.publish.founderss.cn/rc-pub/api/common/picture?pictureId=50179500&type=
1.18533325
4.14866638
the curve of
G
0
-
e
moves downward as the increasing
C
u
and moves upward as the increasing
d
50
. The
G
0
firstly decreases and then increases as the increasing
F
c
and the
G
0
reaches the minimum value for
F
c
of about 20%. The
G
0
prediction equations of terrigenous sandy and gravelly soils will obviously underestimate the
G
0
value of coral sand. The influence of
F
c
on
G
0
essentially results from the change of
C
u
and
d
50
for coral sand with various
F
c
. The
G
0
prediction equation of coral sand related to
C
u
and
d
50
which implies the influence of
F
c
on
G
0
was proposed
and the correction factor
A'
related to the morphology and mineralogy of the particle form of coral sands was incorporated in the proposed
G
0
prediction equation. The validity of the
G
0
prediction equation was verified by comparing the measured and predicted
G
0
values of coral sands from different seas.
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