Geopsy: H/V and Spectrum Toolboxes: Processing Tab
Contents
Use
This toolbox tab contains the smoothing and taper parameters for H/V or Spectrum curves and the way the horizontal components are processed to compute the H/V spectral ratio, described in two sections:
- the Parameters section (For H/V and Spectrum tools)
- the Horizontal components section (For H/V tool only)
Parameters section
This section is divided in three parts:
Smoothing
Type of smoothing applied to the windows. During the computing of H/V or Spectrum, the Fourier spectra can be smoothed (it is strongly recommended) in the goal to clarify the global aspect of the curves.
For the Spectrum computation, the Fourier spectrum from each selected time window is smoothed and then the averaged curve is computed.
For the H/V computation, the horizontal Fourier spectra (NS and EW) are first combined and then the smoothing is applied on the merged horizontal Fourier spectrum and on the vertical Fourier spectrum.
Four smoothing methods are evailable:
- Konno and Ohmachi[1] smoothing. This smoothing use a constant bandwidth in a logarithmic scale and is strongly recommended because this smoothing function preserves the different number of points at low and high frequency. This smoothing is controlled by a smoothing constant varying in-between 0 and 100. A constant of 0 gives a very strong smoothing, when a constant of 100 a very soft smoothing, more details;
- Constant smoothing. This smoothing function has a triangular shape centered on the current frequency and its width is equal to "Band width" given by the user. This band width varies from 0 (soft smoothing) to 100 (strong smoothing);
- Proportional smoothing. This smoothing function has a triangular shape and its width depends upon the current frequency. The half width is defined by percentage*frequency. The value of "percentage" cannot be greater or equal to 100% (strong smoothing).
- No smoothing. This can be sometime useful to have a rough idea about Fourier spectra;
The Smoothing constant spin box is used to give the smoothing constant value.
Taper
Check the box to apply a cosine taper on both sides of the selected time windows.
A taper is used to minimize the border effects due to the extraction of a window so as to improve its properties in the frequency domain. The use of a taper is strongly recommended so as to avoid the creation of spurious frequencies.
The taper width is adjusted in the spin box.
Filter
When the box is checked a high-pass filter is applied along the entire record of each component before selecting the stable time windows. This procedure is used to avoid spurious frequencies due to the effect of a strong low frequency content.
Checking this option is recommended when the signal has a strong low frequency content with respect to the frequency of interest, e.g. shallow site next to a shore line, or recording under windy condition. In such case, cutting the signal into short time windows may strongly distort the spectrum, and even using the minimum window length criteria according to the SESAME guidelines [2] (i.e. 10 times the corresponding period for the minimum frequency of interest) may not be enough to ensure a reliable H/V estimation.
This option should be used with caution. As the signal is high-pass filtered, the results below the chosen cut-off frequency could be somewhat flaky, and the cut-off frequency must be much lower than the frequency of interest.
Horizontal components section (only available for HV toolbox)
This section is devoted to indicate how the H/V has to be computed. There are 3 different methods that can be applied.

Squared average
The H/V is computed as followed:
- The Fourier amplitude spectrum is computed for each window of each component (N, E and Z);
- The horizontal average spectrum is computed by a combination of horizontal spectra for each window, following the formula
- The horizontal (averaged) and vertical spectra of each window are smoothed;
- The horizontal to vertical ratio (H/V) is computed for each window;
- The H/V is computed by averaging all H/V coming from individual windows.
Total horizontal energy
The H/V is computed as followed:
- The Fourier amplitude spectrum is computed for each window of each component (N, E and Z)
- The horizontal average spectrum is computed by a combination of horizontal spectra for each window, following the formula
- The horizontal (averaged) and vertical spectra of each window are smoothed
- The horizontal to vertical ratio (H/V) is computed for each window
- The H/V is computed by averaging all H/V coming from individual windows.
Directional energy
Here, the H/V is calculated along a given direction, 0° is assumed to be the North direction and 90° the East direction. From the North-South and the East-West signals, a new (and single) signal is computed geometrically. This new signal is assumed to be the horizontal signal. The direction in which the H/V will be calculated is given in a spin box allowing changes in the direction between 0° and 180°. If the user wants to compute in a direction between 180° and 360°, due to symetry the user should take the symetrical direction: wanted direction-180°. If the user wants a 220° direction, it should be entered 40° in the spin box.
- The Fourier amplitude spectrum is computed for each window of each component (recomputed horizontal and vertical)
- The horizontal (recomputed) and vertical spectra of each window are smoothed
- The horizontal to vertical ratio (H/V) is computed for each window
- The H/V is computed by averaging all H/V coming from individual windows.
Load parameters and Start section
The section at the bottom of the Time tab comprises two buttons.
- The Load parameters button is used to load parameters from previous H/V or spectrum processing stored in a name.log file (example).
- Press the Start button to start H/V or Spectrum processing.
If no window selection has been performed, a pup-up window appears.
Simply click on the Yes button and processing will follow its way with the current Toolbox parameters.
To perform user's windowing, click on the No button.
References
- ↑ Konno K. and T. Ohmachi, 1998. Ground motion characteristics estimated from spectral ratio between horizontal and vertical components of microtremors. Bull. seism. Soc. Am., 88-1, 228-241.
- ↑ Guidelines for the implementation of the H/V spectral ratio technique on ambient vibrations measurements, processing and interpretation, [1], 62 pages, April 2005