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自记水管倾斜仪的倾斜潮观测
引用本文:刘长恩,邓世榜,杨军. 自记水管倾斜仪的倾斜潮观测[J]. 地球物理学报, 1985, 28(5): 502-509
作者姓名:刘长恩  邓世榜  杨军
作者单位:1. 浙江省地震局;2. 徐州市地震办公室;3. 国家地震局分析预报中心
摘    要:我们利用WSQ-1型自记水管倾斜仪在江苏省徐州市琵琶山山洞(34°20'N,117°20'E)对倾斜潮进行了观测.仪器钵体安装在埋入基岩的不锈钢支承棒上,仪器方位为NE117.15°及NE20.50°,格值分别为0.9744ms/mm及0.9429ms/mm.利用维涅第科夫方法对88天(1982年4月至6月)的观测资料进行了调和分析,得到了上述二方位上观测值的主要波群结果.本文还对使用水管倾斜仪进行倾斜潮观测的一些问题进行了讨论.

关 键 词:水管倾斜仪  倾斜潮  水平摆倾斜仪  调和分析  水管仪  中误差  琵琶  半日波  观测精度  气压差  
收稿时间:1983-08-01

OBSERVATIONS OF TILT TIDES BY USE OF WATER TUBE TILTMETER
LIU CHANG-EN,DENG SHI-BANG,YANG JUN. OBSERVATIONS OF TILT TIDES BY USE OF WATER TUBE TILTMETER[J]. Chinese Journal of Geophysics, 1985, 28(5): 502-509
Authors:LIU CHANG-EN  DENG SHI-BANG  YANG JUN
Affiliation:1. Seismological Bureau of Zhejiang Province;2. Seismological Office of Xuzhou, Jiangsu Province;3. Centre of Analysis and Prediction, State Seismological Bureau
Abstract:WSQ-1 Automatic-Recording Water Tube Tiltmeter was used to observe tilt tides in a tunnel at Pipa Hill in Xuzhou, Jiangsu Province (34°20′N, 117°20′E). The tilt-meter is installed in NE 117.15° and 20.50° azimuths, and its end reservoirs are set up on stainless steel piers which were placed on the bedrock. The values of scale division of WSQ-1 are 0.9744 ms/mm and 0.9429 ms/mm. Venedikov's method has been used to analyse the observed data for 88 days (April to June 1982). The preliminary results of the principal wave groups in 117.15°azimuth are given as following:GAMME PHASE LAG SPHGROUP COEFFICIENT SD (deg) (deg)Q1 0.742 0.0690 22.7 5.32O1 0.802 0.0144 10.6 1.03K1 0.744 0.0093 8.76 0.712N2 0.629 0.0566 -3.86 5.14N2 0.660 0.0124 3.53 1.08M2 0.671 0.00257 2.72 0.22S2 0.682 0.0055 -1.16 0.46Some problems about observation of tilt tides using water tube tiltmeter are discussed.
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