JP2017193841A - Ground estimation method - Google Patents
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Abstract
【課題】地盤の特性の推定精度を高める。【解決手段】地表面の下方に硬質基盤を有する地盤の卓越振動数を推定する地盤推定方法であって、水平x方向の常時微動と、水平x方向と直交する水平y方向の常時微動と、鉛直方向の常時微動とを、水平x方向及び水平y方向を水平面内で回転させた複数の角度位置で測定する常時微動測定工程と、複数の角度位置毎に、水平x方向の常時微動、水平y方向の常時微動、鉛直方向の常時微動からそれぞれスペクトルHx、スペクトルHy、スペクトルVを算出するスペクトル算出工程と、各々の角度位置におけるスペクトルHxとスペクトルHy、又は、Hx/Vスペクトル比とHy/Vスペクトル比から形状が最も似ている角度位置を求め、当該角度位置のスペクトルHx、スペクトルHy、スペクトルVに基づいて地盤の卓越振動数を推定する卓越振動数推定工程とを有する。【選択図】図7An object of the present invention is to improve the accuracy of estimating ground characteristics. A ground estimation method for estimating a dominant frequency of ground having a hard basement below the ground surface, comprising constant microtremors in the horizontal x direction, constant microtremors in the horizontal y direction orthogonal to the horizontal x direction, A constant slight movement measurement step of measuring the vertical constant slight movement at a plurality of angular positions in which the horizontal x direction and the horizontal y direction are rotated in the horizontal plane; A spectrum calculation step of calculating spectrum Hx, spectrum Hy, and spectrum V from microtremors in the y direction and normal microtremors in the vertical direction, respectively; a dominant frequency estimating step of obtaining an angular position with the most similar shape from the V spectrum ratio, and estimating the dominant frequency of the ground based on the spectrum Hx, spectrum Hy, and spectrum V of the angular position; [Selection drawing] Fig. 7
Description
本発明は、地盤推定方法に関する。 The present invention relates to a ground estimation method.
地盤は地震時でなくとも常に小さく揺れている(常時微動)。この常時微動を測定し、その測定結果から地盤の特性を検出できることが知られている。例えば、特許文献1では、水平2成分(x、y)と鉛直成分(z)の常時微動から地盤の卓越周期(換言すると卓越振動数)を算出している。 The ground always shakes slightly even when it is not in an earthquake (fine tremor). It is known that this microtremor can be measured and the characteristics of the ground can be detected from the measurement result. For example, in Patent Document 1, the ground period (in other words, the dominant frequency) is calculated from the constant fine movement of the two horizontal components (x, y) and the vertical component (z).
しかしながら、上記の方法は地表面下の硬質基盤が傾いていないことを前提としており、硬質基盤が傾いている場合は、地盤の特性(卓越振動数など)を安定して検出できなくなるという問題があった。 However, the above method is based on the premise that the hard base below the ground surface is not tilted. If the hard base is tilted, there is a problem that the characteristics of the ground (such as dominant frequency) cannot be detected stably. there were.
本発明は、上記のような従来の問題に鑑みなされたものであって、その目的は、地盤の特性の検出精度を高めることにある。 The present invention has been made in view of the above-described conventional problems, and an object of the present invention is to increase detection accuracy of ground characteristics.
上記目的を達成するための主たる発明は、地表面の下方に硬質基盤を有する地盤の卓越振動数を推定する地盤推定方法であって、水平x方向の常時微動と、前記水平x方向と直交する水平y方向の常時微動と、鉛直方向の常時微動とを、前記水平x方向及び前記水平y方向を水平面内で回転させた複数の角度位置で測定する常時微動測定工程と、前記複数の角度位置毎に、前記水平x方向の常時微動、前記水平y方向の常時微動、前記鉛直方向の常時微動からそれぞれスペクトルHx、スペクトルHy、スペクトルVを算出するスペクトル算出工程と、各々の角度位置における前記スペクトルHxと前記スペクトルHy、又は、Hx/Vスペクトル比とHy/Vスペクトル比から形状が最も似ている角度位置を求め、当該角度位置の前記スペクトルHx、前記スペクトルHy、前記スペクトルVに基づいて前記地盤の卓越振動数を推定する卓越振動数推定工程と、を有することを特徴とする地盤推定方法である。
本発明の他の特徴については、本明細書及び添付図面の記載により明らかにする。
A main invention for achieving the above object is a ground estimation method for estimating a dominant vibration frequency of a ground having a hard base below the ground surface, wherein the fine movement in the horizontal x direction is orthogonal to the horizontal x direction. A microtremor measurement step for measuring microtremors in the horizontal y direction and microtremors in the vertical direction at a plurality of angular positions obtained by rotating the horizontal x direction and the horizontal y direction in a horizontal plane, and the plurality of angular positions. A spectrum calculation step for calculating a spectrum Hx, a spectrum Hy, and a spectrum V from the fine movement in the horizontal x direction, the fine movement in the horizontal y direction, and the fine movement in the vertical direction, respectively, and the spectrum at each angular position. An angular position having the most similar shape is determined from Hx and the spectrum Hy, or an Hx / V spectral ratio and a Hy / V spectral ratio, and the spectral position of the angular position is determined. Torr Hx, the spectral Hy, a ground estimation method characterized by having a predominant frequency estimation step of estimating the number of dominant frequency of the ground on the basis of the spectrum V.
Other features of the present invention will become apparent from the description of the present specification and the accompanying drawings.
本発明によれば、地盤の特性の検出精度を高めることができる。 ADVANTAGE OF THE INVENTION According to this invention, the detection precision of the characteristic of a ground can be improved.
本明細書及び添付図面の記載により、少なくとも以下の事項が明らかとなる。
地表面の下方に硬質基盤を有する地盤の卓越振動数を推定する地盤推定方法であって、水平x方向の常時微動と、前記水平x方向と直交する水平y方向の常時微動と、鉛直方向の常時微動とを、前記水平x方向及び前記水平y方向を水平面内で回転させた複数の角度位置で測定する常時微動測定工程と、前記複数の角度位置毎に、前記水平x方向の常時微動、前記水平y方向の常時微動、前記鉛直方向の常時微動からそれぞれスペクトルHx、スペクトルHy、スペクトルVを算出するスペクトル算出工程と、各々の角度位置における前記スペクトルHxと前記スペクトルHy、又は、Hx/Vスペクトル比とHy/Vスペクトル比から形状が最も似ている角度位置を求め、当該角度位置の前記スペクトルHx、前記スペクトルHy、前記スペクトルVに基づいて前記地盤の卓越振動数を推定する卓越振動数推定工程と、を有することを特徴とする地盤推定方法が明らかとなる。
このような地盤推定方法によれば、基盤の傾きに関わらず、地盤の特性(卓越振動数)の検出精度を高めることができる。
At least the following matters will become apparent from the description of the present specification and the accompanying drawings.
A ground estimation method for estimating a dominant vibration frequency of a ground having a hard base below a ground surface, the horizontal fine movement in the horizontal x direction, the fine movement in the horizontal y direction perpendicular to the horizontal x direction, and the vertical fine movement A fine movement measurement step for measuring fine movement at a plurality of angular positions obtained by rotating the horizontal x direction and the horizontal y direction in a horizontal plane, and a fine movement in the horizontal x direction for each of the plurality of angular positions; A spectrum calculating step for calculating spectrum Hx, spectrum Hy, and spectrum V from the fine movement in the horizontal y direction and the fine movement in the vertical direction, respectively, and the spectrum Hx and the spectrum Hy or Hx / V at each angular position. An angular position having the most similar shape is obtained from the spectral ratio and the Hy / V spectral ratio, and the spectrum Hx, the spectrum Hy, and the spectrum at the angular position are obtained. A predominant frequency estimation step of estimating the number of dominant frequency of the ground on the basis of the vector V, ground estimating method characterized by having become apparent.
According to such a ground estimation method, it is possible to improve the detection accuracy of the ground characteristics (dominant frequency) regardless of the inclination of the base.
かかる地盤推定方法であって、前記水平x方向及び前記水平y方向の回転角度は90度未満であることが望ましい。
このような地盤推定方法によれば、無駄な測定をせずに済む。
In this ground estimation method, it is desirable that the rotation angle in the horizontal x direction and the horizontal y direction is less than 90 degrees.
According to such a ground estimation method, unnecessary measurement is not required.
かかる地盤推定方法であって、前記卓越振動数推定工程では、前記スペクトルHxと前記スペクトルHyの相乗平均を前記スペクトルVで除算して前記H/Vスペクトル比を算出し、当該H/Vスペクトル比が最も大きくなる振動数を前記卓越振動数としてもよい。 In this ground estimation method, in the dominant frequency estimation step, the H / V spectrum ratio is calculated by dividing the geometric mean of the spectrum Hx and the spectrum Hy by the spectrum V to calculate the H / V spectrum ratio. The frequency at which becomes the largest may be the dominant frequency.
かかる地盤推定方法であって、前記卓越振動数推定工程では、前記スペクトルHxと前記スペクトルHyの2乗和平方根を前記スペクトルVで除算して前記H/Vスペクトル比を算出し、当該H/Vスペクトル比が最も大きくなる振動数を前記卓越振動数としてもよい。 In this ground estimation method, in the dominant frequency estimation step, the square root sum of the spectrum Hx and the spectrum Hy is divided by the spectrum V to calculate the H / V spectrum ratio, and the H / V The frequency with the largest spectral ratio may be the dominant frequency.
また、地表面の下方に硬質基盤を有する地盤の前記硬質基盤の傾斜方向を推定する地盤推定方法であって、水平x方向の常時微動と、前記水平x方向と直交する水平y方向の常時微動と、鉛直方向の常時微動とを、前記水平x方向及び前記水平y方向を水平面内で回転させた複数の角度位置で測定する常時微動測定工程と、前記複数の角度位置毎に、前記水平x方向の常時微動、前記水平y方向の常時微動、前記鉛直方向の常時微動からそれぞれスペクトルHx、スペクトルHy、スペクトルVを算出するスペクトル算出工程と、各々の角度位置における前記スペクトルHxと前記スペクトルHy、又は、Hx/Vスペクトル比とHy/Vスペクトル比の形状が最も似ている角度位置の45度回転方向、あるいは、各々の角度位置における前記スペクトルHxと前記スペクトルHy、又は、前記Hx/Vスペクトル比と前記Hy/Vスペクトル比の形状が最も異なる角度方向を求めることに基づいて前記硬質基盤の傾斜方向を推定する傾斜方向推定工程と、を有することを特徴とする地盤推定方法が明らかとなる。 Also, a ground estimation method for estimating a tilt direction of the hard base of a ground having a hard base below the ground surface, the micro tremor in the horizontal x direction and the micro tremor in the horizontal y direction perpendicular to the horizontal x direction. And a microtremor measurement step for measuring microtremors in the vertical direction at a plurality of angular positions obtained by rotating the horizontal x direction and the horizontal y direction in a horizontal plane, and the horizontal x at each of the plurality of angular positions. A spectrum calculation step of calculating a spectrum Hx, a spectrum Hy, and a spectrum V from the continuous fine movement in the direction, the fine movement in the horizontal y direction, and the fine movement in the vertical direction, respectively, and the spectrum Hx and the spectrum Hy at each angular position, Or 45 degree rotation direction of the angular position where the shape of the Hx / V spectral ratio and Hy / V spectral ratio is most similar, or the front in each angular position An inclination direction estimating step of estimating an inclination direction of the hard base based on obtaining an angular direction in which the shapes of the spectrum Hx and the spectrum Hy or the Hx / V spectrum ratio and the Hy / V spectrum ratio are most different from each other; A ground estimation method characterized by having
このような地盤推定方法によれば、地盤の特性(基盤の傾斜の方向又は傾斜に垂直な方向)の検出精度を高めることができる。 According to such a ground estimation method, it is possible to improve the detection accuracy of the characteristics of the ground (the direction of inclination of the base or the direction perpendicular to the inclination).
かかる地盤推定方法であって、複数の地点において前記傾斜方向推定工程を実行して前記硬質基盤の傾斜方向を推定することが望ましい。 In this ground estimation method, it is preferable that the inclination direction estimation process is executed at a plurality of points to estimate the inclination direction of the hard base.
このような地盤推定方法によれば、硬質基盤の傾斜方向をより確実に求めることができる。 According to such a ground estimation method, the inclination direction of the hard base can be obtained more reliably.
===第1実施形態===
<<卓越振動数について>>
<常時微動について>
大地(地盤)は地震時でなくとも常に小さく揺れている。一般に、周期1秒よりも短周期の揺れは人間活動による人工的な振動源が原因であり、それよりも長周期の揺れは波浪や気圧変化などの自然現象が原因であると考えられている。これらの小さな振動は常時微動と呼ばれる。
=== First Embodiment ===
<< About the dominant frequency >>
<Regarding microtremor>
The ground (ground) is always shaking slightly, even during an earthquake. In general, fluctuations shorter than 1 second are caused by artificial vibration sources caused by human activities, and longer periods are caused by natural phenomena such as waves and atmospheric pressure changes. . These small vibrations are called microtremors.
この常時微動を測定することにより、地震時の地盤の揺れ易さなどの特性を検出することができる。また、測定したデータを解析することにより、地盤構造(どのような固さの層構成になっているかなど)の推定を行うこともできる。 By measuring this microtremor, characteristics such as the ease of shaking of the ground during an earthquake can be detected. In addition, by analyzing the measured data, it is possible to estimate the ground structure (how hard the layer structure is).
図1は、常時微動の測定方法の概略説明図である。また、図2は、各方向の揺れ(常時微動)の測定結果の一例を示す図である。図2の横軸は時間、縦軸は揺れの大きさを示している。 FIG. 1 is a schematic explanatory diagram of a method for measuring microtremors at all times. Moreover, FIG. 2 is a figure which shows an example of the measurement result of the shake (always fine movement) of each direction. In FIG. 2, the horizontal axis indicates time, and the vertical axis indicates the magnitude of shaking.
微動を測る際は、図1のように微動計10を地盤1の地面1a(地表面に相当)に設置する。なお、地盤1の地面1aの下方には、硬い層の基盤3(硬質基盤に相当)が存在している。 When measuring the fine movement, the fine movement meter 10 is installed on the ground 1a (corresponding to the ground surface) of the ground 1 as shown in FIG. A hard base 3 (corresponding to a hard base) exists below the ground 1a of the ground 1.
微動計10は、高感度の地震計である。微動計10には、水平2成分(x方向、y方向)と鉛直成分(z方向)との3成分のセンサーとロガー(記録装置)とが一体に設けられている。図1において、微動計10は、x方向の正が東(負が西)、y方向の正が北(負が南)、z方向の正が上(負が下)となるように地面1a上に配置されている。そして微動計10は、x方向、y方向、z方向の各成分の揺れの大きさ(変位、速度、加速度など)を同時に計測し記録する。これにより、図2のように各方向の微動(常時微動)が測定される。例えば、地盤1の東西の揺れ(微動)は、微動計10のx方向(図2の3つの図のうちの一番上の図)の成分として測定される。 The microtremor meter 10 is a highly sensitive seismometer. The microtremor meter 10 is integrally provided with a three-component sensor of two horizontal components (x direction and y direction) and a vertical component (z direction) and a logger (recording device). In FIG. 1, the microtremor meter 10 has a ground 1a such that the positive in the x direction is east (negative is west), the positive in the y direction is north (negative is south), and the positive in the z direction is upward (negative is down). Is placed on top. The microtremor meter 10 simultaneously measures and records the magnitude (displacement, velocity, acceleration, etc.) of the shaking of each component in the x, y, and z directions. Thereby, as shown in FIG. 2, fine movement in each direction (always fine movement) is measured. For example, the east-west shaking (fine movement) of the ground 1 is measured as a component in the x direction (the uppermost figure of the three figures in FIG. 2) of the fine movement meter 10.
<H/Vスペクトル比について>
1地点において観測した微動の3成分観測記録のうち、水平動のスペクトル(H)を上下(鉛直)動のスペクトル(V)で除算したスペクトル比をとることにより、振動源の影響を受けない安定した結果が得られるといわれている。このスペクトル比はH/Vスペクトル比と呼ばれており、地盤1が揺れやすい振動数(卓越振動数)を推定するのに利用されている。
<About H / V spectral ratio>
Of the three-component observation records of microtremors observed at one point, a stable ratio that is not affected by the vibration source is obtained by taking the spectrum ratio obtained by dividing the horizontal motion spectrum (H) by the vertical (vertical) motion spectrum (V). It is said that the result will be obtained. This spectral ratio is called the H / V spectral ratio, and is used to estimate the frequency at which the ground 1 is likely to shake (dominant frequency).
図1のように微動計10を地面1aに設置し、x、y、zの3成分の常時微動を記録する場合、H/Vスペクトル比の計算の手順は以下のようになる。 As shown in FIG. 1, when the microtremor meter 10 is installed on the ground 1a and the constant tremor of the three components x, y and z is recorded, the procedure for calculating the H / V spectrum ratio is as follows.
図3A〜図3Cは、H/Vスペクトル比の算出の手順を示す概略説明図である。 3A to 3C are schematic explanatory diagrams illustrating a procedure for calculating the H / V spectrum ratio.
まず、観測された各成分(x、y、z)の微動データ(図3A)を周波数分析する。これにより、図3Bに示すようにx方向、y方向、z方向の各スペクトルが得られる。なお、図3Bの各図の横軸は振動数(Hz)、縦軸は振幅の大きさを示している。次に、水平動(xおよびy)のスペクトルを上下動(z)のスペクトルで除算する。この時、H/Vスペクトル比の計算式は以下の式などの方法がある。 First, frequency analysis is performed on the fine movement data (FIG. 3A) of each observed component (x, y, z). Thereby, as shown to FIG. 3B, each spectrum of x direction, y direction, and z direction is obtained. 3B, the horizontal axis indicates the frequency (Hz), and the vertical axis indicates the amplitude. Next, the horizontal motion (x and y) spectrum is divided by the vertical motion (z) spectrum. At this time, the calculation formula of the H / V spectrum ratio includes a method such as the following formula.
ここで、Hx、Hy、Vは、それぞれ、水平直交2成分(x、y)及び鉛直成分(z)の微動のフーリエスペクトルである。また、式1は、水平動のスペクトルHをスペクトルHxとスペクトルHyの相乗平均とする場合の式であり、式2は、水平動のスペクトルHをスペクトルHxとスペクトルHyの2乗和平方根とする場合の式である。
これにより、図3Cに示すようにH/Vスペクトル比が得られる。
Here, Hx, Hy, and V are fine-spectrum Fourier spectra of a horizontal orthogonal two component (x, y) and a vertical component (z), respectively. Equation 1 is an equation in the case where the horizontal motion spectrum H is the geometric mean of the spectrum Hx and the spectrum Hy, and Equation 2 is the horizontal motion spectrum H being the square sum of squares of the spectrum Hx and the spectrum Hy. Is the expression of the case.
Thereby, the H / V spectral ratio is obtained as shown in FIG. 3C.
また、図4Aは、図1の状態で測定されたHx/Vスペクトル比、及び、Hy/Vスペクトル比の一例を示す図であり、図4Bは、そのときのH/Vスペクトル比を示す図である。なお、Hx/Vスペクトル比とは水平x成分のスペクトルHxと鉛直z成分のスペクトルVとの比であり、Hy/Vスペクトル比とは水平y成分のスペクトルHyと鉛直z成分のスペクトルVとの比である。 4A is a diagram showing an example of the Hx / V spectral ratio and Hy / V spectral ratio measured in the state of FIG. 1, and FIG. 4B is a diagram showing the H / V spectral ratio at that time. It is. The Hx / V spectral ratio is the ratio between the horizontal x component spectrum Hx and the vertical z component spectrum V. The Hy / V spectral ratio is the horizontal y component spectrum Hy and the vertical z component spectrum V. Is the ratio.
図4AではHx/Vスペクトル比の形状とHy/Vスペクトル比の形状が似ている(卓越振動数が同じ値である)。そして、これらの各成分のスペクトルから得られるH/Vスペクトル比(図4B)の卓越振動数も、図4Aの卓越振動数と同じ値になっている。 In FIG. 4A, the shape of the Hx / V spectral ratio is similar to the shape of the Hy / V spectral ratio (the dominant frequency is the same value). The dominant frequency of the H / V spectrum ratio (FIG. 4B) obtained from the spectra of these components is also the same value as the dominant frequency of FIG. 4A.
このようにH/Vスペクトル比を求める際に、水平動のスペクトルHは水平x成分(スペクトルHx)および水平y成分(スペクトルHy)を合わせて考えており、この求め方は、地層が成層(x方向の微動≒y方向の微動)であることを前提としている。しかしながら、実際には図5のように基盤3(固い層)が傾斜している場合がある。なお、図5は、基盤3が傾斜している場合の状態を示す図である。図5では、基盤3が南北方向に傾いており、北側は浅く、南側は深くなっている。また、図5において微動計10は図1と同じ向きに置かれている。 Thus, when obtaining the H / V spectral ratio, the horizontal motion spectrum H is considered by combining the horizontal x component (spectrum Hx) and the horizontal y component (spectrum Hy). It is assumed that fine movement in the x direction≈fine movement in the y direction. However, actually, the base 3 (hard layer) may be inclined as shown in FIG. In addition, FIG. 5 is a figure which shows a state in case the base | substrate 3 inclines. In FIG. 5, the base 3 is inclined in the north-south direction, the north side is shallow and the south side is deep. In FIG. 5, the microtremor meter 10 is placed in the same direction as in FIG.
図6Aは図5の状態で測定されたHx/Vスペクトル比、及び、Hy/Vスペクトル比の一例を示す図であり、図6Bは、そのときのH/Vスペクトル比を示す図である。 6A is a diagram showing an example of the Hx / V spectral ratio and the Hy / V spectral ratio measured in the state of FIG. 5, and FIG. 6B is a diagram showing the H / V spectral ratio at that time.
図5のように基盤3が傾斜している場合、図6Aに示すようにx方向のスペクトルHxとy方向のスペクトルHyとが大きく異なる(卓越振動数が一致しない)ことがある。この場合、スペクトルHxとスペクトルHyをそのまま用いてH/Vスペクトル比を算出するとH/Vスペクトル比のピークが不明確になり、安定した卓越振動数を求めることができなくなるおそれがある(地盤1の特性の検出精度が低下するおそれがある)。 When the base 3 is inclined as shown in FIG. 5, the spectrum Hx in the x direction and the spectrum Hy in the y direction may be greatly different (the dominant frequencies do not match) as shown in FIG. 6A. In this case, if the H / V spectrum ratio is calculated using the spectrum Hx and the spectrum Hy as they are, the peak of the H / V spectrum ratio becomes unclear, and it may not be possible to obtain a stable dominant frequency (ground 1). The detection accuracy of the characteristics may be reduced).
そこで、本実施形態では、地盤1の特性(具体的には卓越振動数)の検出精度を高めるようにしている。 Therefore, in this embodiment, the detection accuracy of the characteristics (specifically, the dominant frequency) of the ground 1 is increased.
<<本実施形態の卓越振動数の測定方法>>
図7は、本実施形態における卓越振動数の測定方法の概略説明図である。なお、本実施形態において微動計10は、各種のデータやプログラムを記憶する記憶部及び各種の演算を行う演算処理部を備えたコンピュータ(不図示)と通信可能に接続されており、常時微動の測定以外の処理は、当該コンピュータにて行う。
<< Measurement method of the dominant frequency of this embodiment >>
FIG. 7 is a schematic explanatory diagram of a method for measuring the dominant frequency in the present embodiment. In the present embodiment, the microtremor meter 10 is communicably connected to a computer (not shown) provided with a storage unit for storing various data and programs and an arithmetic processing unit for performing various calculations. Processing other than measurement is performed by the computer.
本実施形態では、図7に示すように微動計10を数度おきに回転させて測定する。つまり、x方向、y方向、及び、z方向の各常時微動を、x方向とy方向を水平面で回転させた複数の角度位置で測定する(常時微動測定工程に相当)。 In the present embodiment, measurement is performed by rotating the microtremor meter 10 every several degrees as shown in FIG. That is, the microtremors in the x direction, the y direction, and the z direction are measured at a plurality of angular positions obtained by rotating the x direction and the y direction on the horizontal plane (corresponding to the microtremor measurement step).
例えば、図に示すようにx方向が東、y方向が北を向いた状態(x0、y0)から、微動計10を上から見て時計回りに(x1、y1)→(x2、y2)→(x3、y3)と回転させる。そして、各角度位置の水平2成分と鉛直成分の常時微動を測定する。 For example, as shown in the figure, from the state (x 0 , y 0 ) where the x direction is east and the y direction is north, (x 1 , y 1 ) → (x 2 , y 2 ) → (x 3 , y 3 ). Then, the fine movement of the two horizontal components and the vertical component at each angular position is measured.
コンピュータは、各角度位置で測定した常時微動のデータを受信し、これらを周波数分析してx方向、y方向、z方向の各スペクトル(スペクトルHx、スペクトルHy、スペクトルV)を算出する(スペクトル算出工程に相当)。なお、本実施形態では、微動計10自体を回転させているが、x方向とy方向の水平2成分のデータを数度おきに回転させて解析してもよい。 The computer receives microtremor data measured at each angular position, and frequency-analyzes them to calculate each spectrum in the x, y, and z directions (spectrum Hx, spectrum Hy, spectrum V) (spectrum calculation). Equivalent to the process). In the present embodiment, the microtremor meter 10 itself is rotated. However, data of two horizontal components in the x and y directions may be rotated and analyzed every several degrees.
次に、角度位置ごとにHx/Vスペクトル比と、Hy/Vスペクトル比を求め、各々の角度位置におけるHx/Vスペクトル比とHy/Vスペクトル比の形状が最も一致する方向(角度位置)を見つける。なお、xとyは正負記録しているため、90度回すと0度の場合のスペクトルと同じ結果となる。つまり、回転の角度は90度未満でよい。これにより無駄な測定をせずに済む。 Next, the Hx / V spectral ratio and the Hy / V spectral ratio are obtained for each angular position, and the direction (angular position) in which the shape of the Hx / V spectral ratio and Hy / V spectral ratio at each angular position most closely matches is determined. locate. Since x and y are recorded as positive and negative, turning 90 degrees gives the same result as the spectrum at 0 degree. That is, the rotation angle may be less than 90 degrees. This eliminates unnecessary measurement.
図8A〜図8Dは、微動計10を水平面で(x方向、y方向について)回転させた場合の、Hx/Vスペクトル比と、Hy/Vスペクトル比の形状の変化を示す図である。図8Aは(x0、y0)、図8Bは(x1、y1)、図8Cは(x2、y2)、図8Dは(x3、y3)における形状をそれぞれ示している。 8A to 8D are diagrams showing changes in the shape of the Hx / V spectral ratio and the Hy / V spectral ratio when the microtremor meter 10 is rotated in the horizontal plane (about the x direction and the y direction). 8A shows the shape at (x 0 , y 0 ), FIG. 8B shows the shape at (x 1 , y 1 ), FIG. 8C shows the shape at (x 2 , y 2 ), and FIG. 8D shows the shape at (x 3 , y 3 ). .
これらの図からわかるように、回転に応じてx方向とy方向の形状が変化している。例えば図の場合、図8Cの角度位置(x2、y2)になったときにHx/Vスペクトル比とHy/Vスペクトル比の形状が概ね一致している。 As can be seen from these figures, the shapes in the x direction and the y direction change according to the rotation. For example, in the case of the figure, when the angle position (x 2 , y 2 ) in FIG. 8C is reached, the shapes of the Hx / V spectral ratio and the Hy / V spectral ratio substantially coincide.
このように、Hx/Vスペクトル比とHy/Vスペクトル比の形状が最も似ている角度位置を求め、その角度位置のデータ(スペクトルHx、スペクトルHy、スペクトルV)を用いて、前述した式1又は式2によりH/Vスペクトル比を求める。そして、H/Vスペクトル比が最も大きくなる振動数を卓越振動数と推定する(卓越振動数推定工程に相当)。これにより、基盤3が傾斜していても安定した卓越振動数を求めることができる。 In this way, the angle position where the shapes of the Hx / V spectrum ratio and the Hy / V spectrum ratio are most similar is obtained, and using the data of the angle position (spectrum Hx, spectrum Hy, spectrum V), the above-described formula 1 Alternatively, the H / V spectral ratio is obtained by Equation 2. Then, the frequency at which the H / V spectrum ratio is the largest is estimated as the dominant frequency (corresponding to the dominant frequency estimation step). Thereby, even if the base | substrate 3 inclines, the stable dominant frequency can be calculated | required.
なお、本実施形態では、Hx/Vスペクトル比とHy/Vスペクトル比の形状を比較することで角度位置を決定しているが、各々の角度位置におけるスペクトルHxとスペクトルHyの形状から最も似ている角度位置を求めてもよい。また、本実施形態では、コンピュータが角度位置を求めているが、例えば作業員が形状を目視することによって角度位置を決めてもよい。 In the present embodiment, the angle position is determined by comparing the shapes of the Hx / V spectral ratio and the Hy / V spectral ratio, but it is most similar to the shape of the spectrum Hx and the spectrum Hy at each angular position. The angular position may be obtained. In this embodiment, the computer determines the angular position. However, for example, the worker may determine the angular position by viewing the shape.
以上説明したように、本実施形態では、地面1aの下方に基盤3を有する地盤1の卓越振動数を推定する際に、水平2成分(x方向及びy方向)を水平面内で回転させた複数の角度位置で、x方向、y方向、z方向の常時微動を測定している。そして、各常時微動からそれぞれ、水平x方向のスペクトルHxと、水平y方向のスペクトルHyと、鉛直方向のスペクトルVとを算出している。そして、各々の角度位置におけるHx/Vスペクトル比とHy/Vスペクトル比から形状が最も似ている角度位置を求め、当該角度位置のスペクトルHx、スペクトルHy、スペクトルVを用いて地盤1の卓越振動数を推定している。 As described above, in the present embodiment, when estimating the dominant frequency of the ground 1 having the base 3 below the ground 1a, a plurality of horizontal two components (x direction and y direction) are rotated in the horizontal plane. At this angular position, microtremors in the x, y, and z directions are constantly measured. Then, from each microtremor, a spectrum Hx in the horizontal x direction, a spectrum Hy in the horizontal y direction, and a spectrum V in the vertical direction are calculated. Then, an angular position having the most similar shape is obtained from the Hx / V spectral ratio and the Hy / V spectral ratio at each angular position, and the dominant vibration of the ground 1 is obtained using the spectrum Hx, the spectrum Hy, and the spectrum V at the angular position. Estimate the number.
これにより、基盤3の傾斜の有無にかかわらず、安定した卓越振動数を求めることができ、地盤1の特性(卓越振動数)の検出精度を高めることができる。 Thereby, irrespective of the presence or absence of the inclination of the base | substrate 3, the stable dominant frequency can be calculated | required and the detection precision of the characteristic (dominant frequency) of the ground 1 can be improved.
===第2実施形態===
前述の実施形態では、地盤1の特性として卓越振動数を算出していたが、第2実施形態では、地盤1の基盤3の傾き(傾斜)の方向を求める。
=== Second Embodiment ===
In the above-described embodiment, the dominant frequency is calculated as the characteristic of the ground 1, but in the second embodiment, the direction of the inclination (inclination) of the base 3 of the ground 1 is obtained.
すなわち、x方向のスペクトルHxとy方向のスペクトルHy(又は、Hx/Vスペクトル比とHy/Vスペクトル比)の異なる原因が基盤3の傾斜による影響であると考えると、基盤3の傾斜方向およびその直角方向で計測した場合が最もスペクトルの違いが大きくなると推察される。逆に、基盤3の傾斜の影響を対称に受ける方向(つまり傾斜方向から45度回転した角度位置)で測定するとスペクトルHxとスペクトルHy(または、Hx/Vスペクトル比とHy/Vスペクトル比)が最も近くなると推察される。 That is, if the cause of the difference between the spectrum Hx in the x direction and the spectrum Hy in the y direction (or the Hx / V spectral ratio and the Hy / V spectral ratio) is due to the tilt of the base 3, the tilt direction of the base 3 and It is assumed that the difference in spectrum is the largest when measured in the perpendicular direction. Conversely, when measured in a direction that is symmetrically affected by the tilt of the substrate 3 (that is, an angular position rotated 45 degrees from the tilt direction), the spectrum Hx and spectrum Hy (or Hx / V spectrum ratio and Hy / V spectrum ratio) are obtained. Presumed to be closest.
図9A〜図9D、及び、図10A〜図10D図は、基盤3の傾斜の方向と微動計10の角度位置(x方向、y方向)との関係の説明図である。ここでは第1実施形態(図5、図7)と同様に、傾斜の方向は南北方向であり、北側では基盤3が浅く、南側では基盤3が深くなっている。 9A to 9D and FIGS. 10A to 10D are explanatory diagrams of the relationship between the inclination direction of the base 3 and the angular position (x direction, y direction) of the microtremor meter 10. Here, as in the first embodiment (FIGS. 5 and 7), the direction of inclination is the north-south direction, the base 3 is shallow on the north side, and the base 3 is deep on the south side.
図9A〜図9Dは、x方向又はy方向の何れか一方が傾斜方向に対して垂直になっている場合の図である。すなわち、x方向とy方向の一方が傾斜の方向(南北方向)に垂直であり、他方が傾斜の方向に平行になっている。この場合、x方向とy方向とにおいて、基盤3の傾斜の影響の受け方が最も異なり、スペクトルの違いが大きくなる。 9A to 9D are diagrams in a case where one of the x direction and the y direction is perpendicular to the tilt direction. That is, one of the x direction and the y direction is perpendicular to the tilt direction (north-south direction), and the other is parallel to the tilt direction. In this case, the way of receiving the influence of the inclination of the base 3 is most different between the x direction and the y direction, and the difference in spectrum becomes large.
図10A〜図10Dは、x方向とy方向が、傾斜方向に対して共に45度になっている場合の図である。この場合、xとyとにおいて基盤3の傾斜の影響を同様に受けることになる。すなわち、xとyのスペクトルが概ね一致するようになる。 10A to 10D are diagrams in the case where the x direction and the y direction are both 45 degrees with respect to the tilt direction. In this case, x and y are similarly affected by the inclination of the base 3. That is, the spectra of x and y are approximately the same.
なお、図9Aと図9C、図9Bと図9D、及び、図10Aと図10C、図10Bと図10Dはそれぞれ波のデータは正負反転した波形となり、スペクトル(振動数ごとの揺れの大きさ)は同一となる。 9A and 9C, FIG. 9B and FIG. 9D, and FIG. 10A and FIG. 10C, FIG. 10B and FIG. 10D, respectively, the wave data are inversion waveforms, and the spectrum (the magnitude of fluctuation for each frequency) Are the same.
以上のことより、x方向のスペクトルHxとy方向のスペクトルHy(または、Hx/Vスペクトル比、及び、Hy/Vスペクトル比)が概ね一致した方向(図8Cの状態)から45度回転した方向が基盤3の傾斜方向、又は、傾斜に垂直な方向であるとわかる。 From the above, the direction rotated 45 degrees from the direction in which the spectrum Hx in the x direction and the spectrum Hy in the y direction (or Hx / V spectral ratio and Hy / V spectral ratio) substantially coincide (state of FIG. 8C). Is the inclination direction of the substrate 3 or the direction perpendicular to the inclination.
よって、スペクトルHxとスペクトルHy(または、Hx/Vスペクトル比とHy/Vスペクトル比)の形状が最も似ている角度位置の45度回転方向、あるいは、各々の角度位置におけるスペクトルHxとスペクトルHy(または、Hx/Vスペクトル比とHy/Vスペクトル比)の形状が最も異なる角度方向から、基盤3の傾斜方向、及び、その直角方向(傾斜方向に垂直な方向)を推定することができる。ただし、一点の測定だけでは、傾斜方向と傾斜に直角な方向の何れかであることがわかるのみであり、基盤3の傾斜方向を確実に判断できない。 Therefore, the 45-degree rotation direction of the angular position where the shapes of the spectrum Hx and the spectrum Hy (or the Hx / V spectral ratio and the Hy / V spectral ratio) are most similar, or the spectral Hx and the spectral Hy (at each angular position) Alternatively, it is possible to estimate the tilt direction of the substrate 3 and the direction perpendicular to the tilt direction (direction perpendicular to the tilt direction) from the angle direction in which the shapes of the Hx / V spectrum ratio and the Hy / V spectrum ratio are the most different. However, only one point of measurement can be understood to be either the tilt direction or the direction perpendicular to the tilt, and the tilt direction of the substrate 3 cannot be determined reliably.
これに対し、複数(2つ以上)の地点で卓越振動数の測定をすれば、基盤3の傾斜方向をより確実に推測することができる。また、卓越振動数は、基盤3が浅いほど大きくなり、基盤3が深いほど小さくなる。よって、前述の方法で複数の地点の卓越振動数を求め、その大小を比較することで、その各地点のどこの基盤3が深いかがわかる。つまり、基盤3の傾斜方向(深さの向き)、及び、その直角方向(傾斜方向に垂直な方向)を判断することができる。 On the other hand, if the dominant frequency is measured at a plurality of (two or more) points, the inclination direction of the base 3 can be estimated more reliably. The dominant frequency increases as the base 3 is shallow, and decreases as the base 3 is deep. Therefore, by obtaining the dominant frequencies at a plurality of points by the above-described method and comparing the magnitudes, it is possible to know which base 3 is deep at each point. That is, it is possible to determine the inclination direction (depth direction) of the base 3 and the right-angle direction (direction perpendicular to the inclination direction).
図11A〜図11Cは、地盤1の特性(基盤3の傾斜方向)の推定方法についての説明図である。 11A to 11C are explanatory diagrams of a method for estimating the characteristics of the ground 1 (inclination direction of the base 3).
図11Aに示すように、この例では、基盤3の傾斜方向に対して、x方向とy方向がそれぞれ45度となっている(スペクトルHxとスペクトルHyが概ね一致する)。ただし、仮に地点P1だけで測定した場合、傾斜の方向が図に示す方向か、図に示す方向の直交方向かが判断できない。そこで、本実施形態では、地点P1と地点P2の2点で測定している。 As shown in FIG. 11A, in this example, the x direction and the y direction are 45 degrees with respect to the inclination direction of the base 3 (the spectrum Hx and the spectrum Hy substantially coincide). However, if the measurement is performed only at the point P1, it cannot be determined whether the direction of the inclination is the direction shown in the figure or the direction orthogonal to the direction shown in the figure. Therefore, in this embodiment, measurement is performed at two points, point P1 and point P2.
図11Bは、地点P1におけるH/Vスペクトル比と地点P2におけるH/Vスペクトル比を示す図である。P1の方がH/Vスペクトル比の卓越振動数が小さく、P2はH/Vスペクトル比の卓越振動数が大きい。 FIG. 11B is a diagram showing the H / V spectrum ratio at the point P1 and the H / V spectrum ratio at the point P2. P1 has a smaller H / V spectral ratio dominant frequency, and P2 has a higher H / V spectral ratio dominant frequency.
この結果から、傾斜の方向が図11Aに示す方向であり、図11Cに示すように、地点P1では基盤3が深く、地点P2では基盤3が浅くなっていることがわかる。仮に、卓越振動数が同じであると、傾斜の方向が地点P1と地点P2を結ぶ方向(図11Aに示す傾斜方向)と直交する方向であることになる。 From this result, it can be seen that the direction of inclination is the direction shown in FIG. 11A, and the base 3 is deep at the point P1 and the base 3 is shallow at the point P2, as shown in FIG. 11C. If the dominant frequency is the same, the inclination direction is a direction orthogonal to the direction connecting the points P1 and P2 (inclination direction shown in FIG. 11A).
このように、本実施形態のように複数の地点で測定することにより、基盤3の傾斜方向を推定することができる。また、この場合においても、微動計10を回転してx方向とy方向のスペクトルが概ね一致する方向を求めることで、地盤1の特性(ここでは基盤3の傾斜方向)の検出精度を高めることができる。 Thus, the inclination direction of the board | substrate 3 can be estimated by measuring in several points like this embodiment. Also in this case, the detection accuracy of the characteristics of the ground 1 (here, the inclination direction of the base 3) is improved by rotating the microtremor meter 10 to obtain a direction in which the spectra in the x direction and the y direction substantially coincide. Can do.
なお、本実施形態ではスペクトルHxとスペクトルHyの形状が最も似ている方向の45度回転方向を傾斜方向として推定していたが、スペクトルHxとスペクトルHyが最も異なる方向から傾斜方向を推定してもよい。 In this embodiment, the 45-degree rotation direction in the direction in which the spectrum Hx and the spectrum Hy are most similar is estimated as the tilt direction. However, the tilt direction is estimated from the direction in which the spectrum Hx and the spectrum Hy are the most different. Also good.
===その他の実施の形態===
以上、本発明の実施形態について説明したが、上記の実施形態は、本発明の理解を容易にするためのものであり、本発明を限定して解釈するためのものではない。また、本発明は、その趣旨を逸脱することなく、変更や改良され得るとともに、本発明にはその等価物が含まれるのはいうまでもない。例えば、以下に示すような変形が可能である。
=== Other Embodiments ===
As mentioned above, although embodiment of this invention was described, said embodiment is for making an understanding of this invention easy, and is not for limiting and interpreting this invention. Further, the present invention can be changed or improved without departing from the gist thereof, and needless to say, the present invention includes equivalents thereof. For example, the following modifications are possible.
前述の実施形態等では、常時微動の測定以外は記憶部や演算処理部を有するコンピュータで行うこことしたが、このコンピュータの機能を微動計10に設けて、微動計10のみで各処理を行うようにしてもよい。 In the above-described embodiment and the like, the computer having the storage unit and the arithmetic processing unit is used except for the measurement of the fine movement at all times. However, the function of this computer is provided in the fine movement meter 10 and each processing is performed only by the fine movement meter 10. You may do it.
1 地盤
1a 地面
3 基盤
10 微動計
1 Ground 1a Ground 3 Base 10 Microtremor meter
Claims (6)
水平x方向の常時微動と、前記水平x方向と直交する水平y方向の常時微動と、鉛直方向の常時微動とを、前記水平x方向及び前記水平y方向を水平面内で回転させた複数の角度位置で測定する常時微動測定工程と、
前記複数の角度位置毎に、前記水平x方向の常時微動、前記水平y方向の常時微動、前記鉛直方向の常時微動からそれぞれスペクトルHx、スペクトルHy、スペクトルVを算出するスペクトル算出工程と、
各々の角度位置における前記スペクトルHxと前記スペクトルHy、又は、Hx/Vスペクトル比とHy/Vスペクトル比から形状が最も似ている角度位置を求め、当該角度位置の前記スペクトルHx、前記スペクトルHy、前記スペクトルVに基づいて前記地盤の卓越振動数を推定する卓越振動数推定工程と、
を有する地盤推定方法。 A ground estimation method for estimating a dominant frequency of a ground having a hard base below the ground surface,
A plurality of angles obtained by rotating the horizontal x direction and the horizontal y direction in the horizontal plane in the horizontal x direction, the fine direction in the horizontal y direction orthogonal to the horizontal x direction, and the vertical fine movement in the horizontal plane. Microtremor measurement process that measures at position,
A spectrum calculating step for calculating a spectrum Hx, a spectrum Hy, and a spectrum V from the fine movement in the horizontal x direction, the fine movement in the horizontal y direction, and the fine movement in the vertical direction for each of the plurality of angular positions;
From the spectrum Hx and the spectrum Hy at each angular position, or an angular position having the most similar shape from the Hx / V spectral ratio and the Hy / V spectral ratio, the spectrum Hx, the spectrum Hy, A dominant frequency estimating step of estimating a dominant frequency of the ground based on the spectrum V;
A ground estimation method comprising:
前記水平x方向及び前記水平y方向の回転角度は90度未満である
ことを特徴とする地盤推定方法。 The ground estimation method according to claim 1,
The ground estimation method, wherein a rotation angle in the horizontal x direction and the horizontal y direction is less than 90 degrees.
前記卓越振動数推定工程では、
前記スペクトルHxと前記スペクトルHyの相乗平均を前記スペクトルVで除算して前記H/Vスペクトル比を算出し、当該H/Vスペクトル比が最も大きくなる振動数を前記卓越振動数とする
ことを特徴とする地盤推定方法。 The ground estimation method according to claim 1 or 2,
In the dominant frequency estimation step,
The geometric mean of the spectrum Hx and the spectrum Hy is divided by the spectrum V to calculate the H / V spectral ratio, and the frequency at which the H / V spectral ratio is the largest is the dominant frequency. The ground estimation method.
前記卓越振動数推定工程では、
前記スペクトルHxと前記スペクトルHyの2乗和平方根を前記スペクトルVで除算して前記H/Vスペクトル比を算出し、当該H/Vスペクトル比が最も大きくなる振動数を前記卓越振動数とする
ことを特徴とする地盤推定方法。 The ground estimation method according to claim 1 or 2,
In the dominant frequency estimation step,
The square root sum of the spectrum Hx and the spectrum Hy is divided by the spectrum V to calculate the H / V spectrum ratio, and the frequency at which the H / V spectrum ratio is the largest is the dominant frequency. A ground estimation method characterized by
水平x方向の常時微動と、前記水平x方向と直交する水平y方向の常時微動と、鉛直方向の常時微動とを、前記水平x方向及び前記水平y方向を水平面内で回転させた複数の角度位置で測定する常時微動測定工程と、
前記複数の角度位置毎に、前記水平x方向の常時微動、前記水平y方向の常時微動、前記鉛直方向の常時微動からそれぞれスペクトルHx、スペクトルHy、スペクトルVを算出するスペクトル算出工程と、
各々の角度位置における前記スペクトルHxと前記スペクトルHy、又は、Hx/Vスペクトル比とHy/Vスペクトル比の形状が最も似ている角度位置の45度回転方向、あるいは、各々の角度位置における前記スペクトルHxと前記スペクトルHy、又は、前記Hx/Vスペクトル比と前記Hy/Vスペクトル比の形状が最も異なる角度方向を求めることに基づいて前記硬質基盤の傾斜方向を推定する傾斜方向推定工程と、
を有することを特徴とする地盤推定方法。 A ground estimation method for estimating an inclination direction of the hard base of the ground having a hard base below the ground surface,
A plurality of angles obtained by rotating the horizontal x direction and the horizontal y direction in the horizontal plane in the horizontal x direction, the fine direction in the horizontal y direction orthogonal to the horizontal x direction, and the vertical fine movement in the horizontal plane. Microtremor measurement process that measures at position,
A spectrum calculating step for calculating a spectrum Hx, a spectrum Hy, and a spectrum V from the fine movement in the horizontal x direction, the fine movement in the horizontal y direction, and the fine movement in the vertical direction for each of the plurality of angular positions;
The spectrum Hx and the spectrum Hy at each angular position, or the 45 degree rotation direction of the angular position having the most similar shape of the Hx / V spectral ratio and the Hy / V spectral ratio, or the spectrum at each angular position An inclination direction estimating step of estimating an inclination direction of the hard base based on obtaining an angular direction in which the shapes of the Hx and the spectrum Hy or the Hx / V spectrum ratio and the Hy / V spectrum ratio are most different from each other;
A ground estimation method characterized by comprising:
複数の地点において前記傾斜方向推定工程を実行して前記硬質基盤の傾斜方向を推定することを特徴とする地盤推定方法。 The ground estimation method according to claim 5.
A ground estimation method, wherein the inclination direction estimation step is executed at a plurality of points to estimate the inclination direction of the hard base.
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