Using 3-C uphole survey technique to survey P-wave and S-wave velocity on surface

被引:0
|
作者
Li, Gui-Hua [1 ]
Zhu, Guang-Ming [1 ]
机构
[1] Department of Geology and Environmental Engineering, Xi'an University of Science and Technology, Xi'an 710054, China
关键词
D O I
暂无
中图分类号
学科分类号
摘要
In order to provide accurate model of near-surface P- and S-wave velocity and thickness, in the continent scientific drilling sites in N area of the northeast of Jiangsu Province, China, the three different surveying methods of 3-C uphole survey for near-surface surveying were used: 1. shooting by dynamite on surface and receiving by 3-C geo-phones in the hole; 2. shooting by using hammer on the surface to hammer at sleeper laterally and receiving by 3-C geophones in the hole; 3. shooting by dynamite in the hole and receiving simultaneously by τ geophone, 3-C geophones and VSP wavelet 3-C geophones on surface. The paper described in detail the acquisition, equipment and processing methods of 3-C uphole surveying data in these three different surveying methods and gained the following knowledge: the reliable first breaks of P-wave can be picked up in vertical components shooting by dynamite on the surface, but the first breaks of S-wave are difficult to be accurately picked up by using horizontal components; the S/N ratio in SH-wave data of horizontal components shooting by hammer on the surface hammering at sleeper laterally is higher, but S/N ratio of the first breaks of P-wave in vertical components is not high; the reliable first breaks of P-wave can be picked up in vertical components shooting in the hole and receiving on the surface, the S-wave arrivals can be observed in horizontal components, but there are multiple group of events before and after S-wave arrivals that makes difficult to recognize true S-wave, nevertheless, using waveform feature or dynamic feature in horizontal components can identify the depth position of layered S-wave velocity. The accurate near-surface information, the P-and S-wave static corrections needs were gained by interpretation of uphole surveying data in the work area. At meantime, some suggestions about equipments and surveying methods of next 3-C uphole survey technique are also presented in the paper.
引用
收藏
页码:160 / 165
相关论文
共 50 条
  • [1] AVO inversion using P- to S-wave velocity ratio and P-wave velocity
    Chen F.
    Zong Z.
    Yang Y.
    Gu X.
    Geophysics, 2022, 87 (04)
  • [2] P-WAVE AND S-WAVE VELOCITY STRUCTURE IN D'' REGION
    MONDT, JC
    TRANSACTIONS-AMERICAN GEOPHYSICAL UNION, 1977, 58 (09): : 912 - 912
  • [3] Characteristics of velocity ratio of p-wave and s-wave for anisotropic rocks
    College of Civil Engineering, Fuzhou University, Fuzhou 350002, China
    不详
    Yanshilixue Yu Gongcheng Xuebao, 2006, 10 (2023-2029):
  • [4] Amplitude-variation-with-offset inversion using P- to S-wave velocity ratio and P-wave velocity
    Chen, Fubin
    Zong, Zhaoyun
    Yang, Yaming
    Gu, Xingyu
    GEOPHYSICS, 2022, 87 (04) : N63 - N74
  • [5] Description of SU(3) s-wave and p-wave baryons
    Furuichi, M
    Shimizu, K
    Takeuchi, S
    MODERN PHYSICS LETTERS A, 2003, 18 (2-6) : 362 - 365
  • [6] 3-DIMENSIONAL P-WAVE AND S-WAVE VELOCITY STRUCTURE BELOW UNZEN VOLCANO
    OHMI, S
    LEES, JM
    JOURNAL OF VOLCANOLOGY AND GEOTHERMAL RESEARCH, 1995, 65 (1-2) : 1 - 26
  • [7] S-WAVE AND P-WAVE STRENGTH FUNCTIONS
    KRUEGER, TK
    MARGOLIS, B
    NUCLEAR PHYSICS, 1961, 28 (04): : 578 - &
  • [8] 3-DIMENSIONAL P-WAVE AND S-WAVE VELOCITY STRUCTURES OF SOUTHERN PERU AND THEIR TECTONIC IMPLICATIONS
    CUNNINGHAM, PS
    ROECKER, SW
    HATZFELD, D
    JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH AND PLANETS, 1986, 91 (B9): : 9517 - 9532
  • [9] P-WAVE AND S-WAVE CRUSTAL VELOCITY OF THE LAKE VANERN AREA, SW SWEDEN
    GREEN, CM
    STUART, GW
    GEOPHYSICAL JOURNAL-OXFORD, 1988, 92 (03): : 533 - 533
  • [10] P-wave and S-wave velocity structure of northern Cascadia margin gas hydrates
    Dash, Ranjan
    Spence, George
    GEOPHYSICAL JOURNAL INTERNATIONAL, 2011, 187 (03) : 1363 - 1377