Study on the Deformation of Filling Bodies in a Loess Mountainous Area Based on InSAR and Monitoring Equipment

被引:5
作者
Wu, Yuming [1 ]
Lan, Hengxing [1 ,2 ]
机构
[1] Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, State Key Lab Resources & Environm Informat Syst, Beijing 100101, Peoples R China
[2] Changan Univ, Coll Geol Engn & Geomat, Xian 710054, Peoples R China
基金
中国国家自然科学基金;
关键词
InSAR; loess; in situ; deformation; land creation; MALAN LOESS; COLLAPSE MECHANISM; LAND CREATION; LANZHOU; PLATEAU; CHINA; LANDSLIDE; COMPRESSIBILITY; DISPLACEMENT; GROUNDWATER;
D O I
10.3390/land11081263
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Several land-creation projects, such as the Lanzhou New Area (LNA), have been undertaken in China as part of the Belt and Road Initiative to bring more living space to the local people in loess areas. However, undisturbed loess and remolded loess have different mechanical characteristics, which may influence the stability of the filling process. Therefore, we monitored the deformation through InSAR and field monitoring to investigate the deformation characteristics and their causes. We obtained the horizontal and vertical displacements, internal deformation, water content, and pressure, according to the air-space-ground integrated monitoring technique. The results show that stress and deformation increase rapidly during construction. Deformation in different places is different during the winter: (1) for vertical displacement, uplift is present in the cut area, settlement is present in the fill area, and heterogeneity is evident in other areas; (2) for horizontal displacement, the expansion state is present in the filling area and the compression state is present at the boundary. Laboratory tests show that the difference in soil compression properties is one of the reasons for these deformation characteristics. Additionally, the difference in volumetric water content and permeability coefficient may trigger different mechanical properties on both sides of the boundary. All the evidence indicates that the boundary region is critical for filling projects. It is also necessary to install monitoring equipment to observe deformation. When abnormal deformations appear, we should take measures to control them.
引用
收藏
页数:17
相关论文
共 67 条
[1]  
[Anonymous], 2016, Agisoft PhotoScan User Manual: Professional Edition, Version 1.3
[2]  
[Anonymous], 1990, BS 1377
[3]   Investigating Subsidence in the Bursa Plain, Turkey, Using Ascending and Descending Sentinel-1 Satellite Data [J].
Aslan, Gokhan ;
Cakir, Ziyadin ;
Lasserre, Cecile ;
Renard, Francois .
REMOTE SENSING, 2019, 11 (01)
[4]   Formation and collapse of metastable particle packings and open structures in loess deposits [J].
Assallay, AM ;
Rogers, CDF ;
Smalley, IJ .
ENGINEERING GEOLOGY, 1997, 48 (1-2) :101-115
[5]   COLLAPSE MECHANISM IN PARTLY SATURATED SOIL [J].
BARDEN, L ;
MCGOWN, A ;
COLLINS, K .
ENGINEERING GEOLOGY, 1973, 7 (01) :49-60
[6]   Quantitative Assessment of Vertical and Horizontal Deformations Derived by 3D and 2D Decompositions of InSAR Line-of-Sight Measurements to Supplement Industry Surveillance Programs in the Tengiz Oilfield (Kazakhstan) [J].
Bayramov, Emil ;
Buchroithner, Manfred ;
Kada, Martin ;
Zhuniskenov, Yermukhan .
REMOTE SENSING, 2021, 13 (13)
[7]  
Bennett M.J, 1994, SUBSURFACE INVESTIGA
[8]   D-InSAR monitoring of ground deformation related to the dewatering of construction sites. A case study of Glories Square, Barcelona [J].
Botey i Bassols, Joan ;
Vazquez-Sune, Enric ;
Crosetto, Michele ;
Barra, Anna ;
Gerard, Pierre .
ENGINEERING GEOLOGY, 2021, 286
[9]  
Carter M., 1996, HKIE T, V3, P1, DOI [10.1080/1023697X.1996.10667690, DOI 10.1080/1023697X.1996.10667690]
[10]  
CHARLES JA, 1991, NATO ADV SCI I E-APP, V200, P73