JP5587101B2 - Method for estimating seismic motion at locations where seismometers are not installed - Google Patents

Method for estimating seismic motion at locations where seismometers are not installed Download PDF

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JP5587101B2
JP5587101B2 JP2010193138A JP2010193138A JP5587101B2 JP 5587101 B2 JP5587101 B2 JP 5587101B2 JP 2010193138 A JP2010193138 A JP 2010193138A JP 2010193138 A JP2010193138 A JP 2010193138A JP 5587101 B2 JP5587101 B2 JP 5587101B2
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seismometer
ground
installation
seismometers
motion
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直泰 岩田
俊六 山本
将宏 是永
俊太 野田
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Railway Technical Research Institute
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Description

本発明は、地震計の新設・移設後の地震動を推定することにより、地震警報の出力状況を推定することができ、新設・移設の効果を定量的に把握することができる、地震計が設置されていない地点における地震動の推定方法に関するものである。 The present invention can estimate the output status of the earthquake warning by estimating the seismic motion after the new installation / relocation of the seismometer , and quantitatively grasp the effect of the new installation / relocation. It relates to a method for estimating seismic motion at a location that is not .

図2は地震の概略過程を示す模式図である。   FIG. 2 is a schematic diagram showing an outline process of an earthquake.

この図において、101は震源、102は基盤、103は表層地盤、104は地表である。   In this figure, 101 is the epicenter, 102 is the base, 103 is the surface ground, and 104 is the ground.

震源101で地震が発生すると(震源過程A)、地震動は基盤102を介して伝播し(伝播過程B)、表層地盤103で増幅されて(増幅過程C)、最終的に震動Dとして地表104に現れる。   When an earthquake occurs in the epicenter 101 (seismic process A), the ground motion propagates through the base 102 (propagation process B), is amplified by the surface ground 103 (amplification process C), and finally becomes ground motion 104 as the ground motion D. appear.

従来、評価対象地点の地震の被害推定方法の提案がなされている(下記特許文献1参照)。また、常時微動のH/Vスペクトル比を用いた地震動推定法の提案がなされている(下記非特許文献1参照)。   Conventionally, an earthquake damage estimation method at an evaluation target point has been proposed (see Patent Document 1 below). In addition, a ground motion estimation method using a constant tremor H / V spectrum ratio has been proposed (see Non-Patent Document 1 below).

特開2008−249485号公報JP 2008-249485 A

土木学会論文集,No.675/I−55,pp.261−272,2001.4JSCE Proceedings, No. 675 / I-55, pp. 261-272, 2001.4

しかしながら、地震計の新設や移設を行う場合、地盤調査などは行われているが、地震計設置後の地震動の特性がどのようなものであるかを推定することは行われていない。   However, when a seismometer is newly installed or moved, ground surveys have been carried out, but it has not been estimated what the characteristics of the seismic motion after the seismometer is installed.

本発明は、上記状況に鑑みて、地盤調査結果を有効に利用して地震計の新設や移設を行った後の地震動の推定を的確に行い、鉄道や道路などへの警報出力を地震計を新設や移設する前に把握することができる、地震計の新設や移設を行った後の地震動の推定方法を提供することを目的とする。   In view of the above situation, the present invention accurately uses the ground survey results to accurately estimate seismic motion after newly installing or moving seismometers, and outputs alarm outputs to railways and roads. The purpose is to provide a method for estimating seismic motion after a new seismometer is installed or moved, which can be grasped before the new installation or move.

本発明は、上記目的を達成するために、
〔1〕地震計が設置されていない地点における地震動の推定方法において、互いに近接する地震計設置箇所と地震計設置予定箇所とにおける地震動の増幅特性をそれぞれ常時微動のH/Vスペクトルから予め求めておき前記地震計設置箇所および前記地震計設置予定箇所の基盤が共通であり、この基盤から入力する地震動が共通である場合、前記地震計設置箇所および前記地震計設置予定箇所のH/Vスペクトルの比を地盤増幅度として、前記地震計設置予定箇所の地震動S Y (f)を前記地震計設置箇所の地震動S X (f)に前記地盤増幅度Rを乗ずることにより推定することを特徴とする。
In order to achieve the above object, the present invention provides
[1] In the method of estimating the ground motion at the point where seismometer is not installed, is previously obtained from the H / V spectra Microtremor respective amplification characteristics of the ground motion at the seismometers installation locations and seismometers planned installation place close to each other In addition, when the bases of the seismometer installation location and the seismometer installation planned location are common and the seismic motion input from this base is common, the H / V spectrum of the seismometer installation location and the seismometer installation planned location characterized in a ratio as site amplification degree R, to estimate by multiplying said ground amplification factor R to ground motion S Y (f) of the seismometers placed planned portion to ground motion S X (f) of the seismometer locations And

本発明によれば、新設・移設後の地震動を推定することにより、地震警報の出力状況等を推定することができ、新設・移設の効果を定量的に把握することができる。   According to the present invention, it is possible to estimate the output status of an earthquake warning, etc. by estimating the seismic motion after the new installation / relocation, and quantitatively grasp the effects of the new installation / relocation.

例えば、地震計を増設することにより、鉄道や道路などの運転規制回数がどの程度増加するか、あるいは、地震計を移設することにより、運転規制回数がどの程度減少するかを見積もることができる。   For example, it is possible to estimate how many times the number of operation restrictions on railways, roads, and the like increases by installing more seismometers, or how much the number of operation restrictions decreases by moving seismometers.

本発明の実施例を示す地震計が設置されていない地点における地震動の推定方法の模式図である。It is a schematic diagram of the estimation method of the ground motion in the point where the seismometer which shows the Example of this invention is not installed. 地震動の伝播過程を概略的に示す模式図である。It is a schematic diagram which shows roughly the propagation process of an earthquake motion.

本発明の地震計が設置されていない地点における地震動の推定方法は、互いに近接する地震計設置箇所と地震計設置予定箇所とにおける地震動の増幅特性をそれぞれ常時微動のH/Vスペクトルから予め求めておき前記地震計設置箇所および前記地震計設置予定箇所の基盤が共通であり、この基盤から入力する地震動が共通である場合、前記地震計設置箇所および前記地震計設置予定箇所のH/Vスペクトルの比を地盤増幅度として、前記地震計設置予定箇所の地震動S Y (f)を前記地震計設置箇所の地震動S X (f)に前記地盤増幅度Rを乗ずることにより推定する。 Method of estimating ground motion at the point where seismometer is not installed in the present invention, obtained in advance from the H / V spectra Microtremor respective amplification characteristics of the ground motion at the seismometers installation locations and seismometers planned installation place close to each other In addition, when the bases of the seismometer installation location and the seismometer installation planned location are common and the seismic motion input from this base is common, the H / V spectrum of the seismometer installation location and the seismometer installation planned location Is the ground amplification degree R , and the ground motion S Y (f) at the location where the seismometer is scheduled to be installed is estimated by multiplying the ground motion S X (f) at the location where the seismometer is installed by the ground amplification degree R.

以下、本発明の実施の形態について詳細に説明する。   Hereinafter, embodiments of the present invention will be described in detail.

図1は本発明の実施例を示す地震計が設置されていない地点における地震動の推定方法の模式図である。   FIG. 1 is a schematic diagram of a method for estimating seismic motion at a point where a seismometer is not installed according to an embodiment of the present invention.

この図において、1は地震動が入力する基盤、2は表層地盤、3は地表、4は地震計が設置されている地表3の場所(SiteX)、5は地震計が設置されていない地表3の場所(SiteY)である。   In this figure, 1 is the base where earthquake motion is input, 2 is the surface ground, 3 is the ground, 4 is the location of the surface 3 where the seismometer is installed (SiteX), 5 is the surface 3 where the seismometer is not installed It is a place (SiteY).

互いに近接する地震計設置箇所としてのSiteXと地震計設置予定箇所としてのSiteYとにおける地震動は、
X (f)=B(f)×GX (f)
Y (f)=B(f)×GY (f)
基盤1から入力する地震動が共通の場合、
X (f)/SY (f)=GX (f)/GY (f)=R
このとき、R(f)=GY (f)/GX (f)をSiteXとSiteYのH/Vスペクトルの比として事前に求めておくことにより、SY (f)=SX (f)×Rとして求めることができる。
The seismic motion at SiteX as the seismometer installation location and SiteY as the seismometer installation location close to each other is
S X (f) = B (f) × G X (f)
S Y (f) = B (f) × G Y (f)
When the ground motion input from the base 1 is common,
S X (f) / S Y (f) = G X (f) / G Y (f) = R
At this time, R (f) = G Y (f) / G X (f) is obtained in advance as the ratio of the H / V spectrum of SiteX and SiteY, so that S Y (f) = S X (f) XR can be obtained.

このように、地震計の新設・移設後の地震動を推定することにより、地震警報の出力状況等を推定することができ、新設・移設の効果を定量的に把握することができる。例えば、地震計を増設することにより、鉄道や道路などの運転規制回数がどの程度増加するか、あるいは、地震計を移設することにより、運転規制回数がどの程度減少するかを見積もることができる。   Thus, by estimating the seismic motion after the new installation / relocation of the seismometer, it is possible to estimate the output status of the earthquake warning and to quantitatively grasp the effects of the new installation / relocation. For example, it is possible to estimate how many times the number of operation restrictions on railways, roads, and the like increases by installing more seismometers, or how much the number of operation restrictions decreases by moving seismometers.

なお、地震計設置箇所および地震計設置予定箇所の基盤が共通であるか否かは、文献やインターネット等により予め調査しておく。   In addition, whether the bases of the seismometer installation location and the seismometer installation planned location are common is investigated in advance by literature or the Internet.

また、互いに近接する地震計設置箇所の距離は、基盤1に入力する地震動が同一の範囲として定めることができる。したがって、基盤1に入力する地震動が同一の範囲が広い場合には、数km〜10数kmに及ぶ距離となることもある。   Further, the distance between the seismometer installation locations that are close to each other can be determined as the same range of the seismic motion input to the base 1. Accordingly, when the ground motion input to the base 1 has a wide range, the distance may reach several kilometers to several tens of kilometers.

なお、本発明は上記実施例に限定されるものではなく、本発明の趣旨に基づき種々の変形が可能であり、これらを本発明の範囲から排除するものではない。   In addition, this invention is not limited to the said Example, Based on the meaning of this invention, a various deformation | transformation is possible and these are not excluded from the scope of the present invention.

本発明の地震計が設置されていない地点における地震動の推定方法は、地盤調査結果を有効に利用して地震計を新設や移設した後の地点における地震動の推定を的確に行い、鉄道や道路などへの警報出力を地震計を新設や移設する前に把握することができる。 The method for estimating the ground motion at a point where the seismometer of the present invention is not installed is an effective method for estimating ground motion at a point after the seismometer is newly installed or relocated by effectively using the ground survey results, such as railways and roads. Can be grasped before the seismometer is newly installed or moved.

1 地震が発生する基盤
2 表層地盤
3 地表
4 地震計が設置されている地表の場所(SiteX)
5 地震計が設置されていない地表の場所(SiteY)
1 Base where earthquake occurs 2 Surface layer 3 Ground surface 4 Location of the surface where the seismometer is installed (SiteX)
5 Location on the surface of the earth where no seismometer is installed (SiteY)

Claims (1)

互いに近接する地震計設置箇所と地震計設置予定箇所とにおける地震動の増幅特性をそれぞれ常時微動のH/Vスペクトルから予め求めておき前記地震計設置箇所および前記地震計設置予定箇所の基盤が共通であり、この基盤から入力する地震動が共通である場合、前記地震計設置箇所および前記地震計設置予定箇所のH/Vスペクトルの比を地盤増幅度として、前記地震計設置予定箇所の地震動S Y (f)を前記地震計設置箇所の地震動S X (f)に前記地盤増幅度Rを乗ずることにより推定することを特徴とする地震計が設置されていない地点における地震動の推定方法。 Is previously obtained amplification characteristic of ground motion from H / V spectra Microtremor respectively in the seismometers installation locations and seismometers planned installation place close to each other, the foundation of the seismometers installation site and the seismometer installation planned portion common If the seismic motion input from this base is common, the seismic motion S at the location where the seismometer is planned to be installed is defined as the ground amplification factor R as the ratio of the H / V spectrum at the location where the seismometer is installed and the location where the seismometer is planned to be installed. A method for estimating seismic motion at a point where no seismometer is installed , wherein Y (f) is estimated by multiplying the ground motion S X (f) at the seismometer installation location by the ground amplification degree R.
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