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5 results for “Geophone”

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zenodo36/100

Geophone data in the Rutor proglacial area (Valle d'Aosta, Italy)

<p>Geophone data (PASI S.r.l.&nbsp;4.5 Hz, vertical) collected along the Rutor proglacial stream, Valle d&#39;Aosta (N 45.667063, E 7.001157 WGS84). Geophones are installed at different distances from the channel (Geo1 at 3 m, Geo2 at 6 m, Geo3 at 8 m). Raw seismic data are recorded at a sampling rate of 200 Hz, with a&nbsp;Amplifier Gain = 16. Time synchronization is provided by a GPS. The dataset&nbsp;is composed of the timestamp in UTC (dd-mmm-yyyy HH:MM) and aggregated data computed&nbsp;as the mean of the absolute values of the raw data calculated on a 1-min time window (in counts). Raw data at 200 Hz are recorded with a DATA-CUBE&sup3;, a&nbsp;3-channel, 24-bit seismic data recorder.&nbsp;The signal input range of the DATA-CUBE&sup3; is &plusmn; 2.048V = 4.096Vpp.&nbsp;For 24-bit ADC this equals 0.000 000 244 140 625V per count at gain 1.</p>

opencc-by-4.0Mar 2023View details →
zenodo32/100

Rayleigh wave H/V and phase velocity measurements of "3D Shear Wave Velocity Model of Salt Lake Valley via Rayleigh Wave Ellipticity Across a Temporary Geophone Array"

<p>This file includes Rayleigh wave H/V and phase velocity measurements of the paper &quot;3D Shear Wave Velocity Model of Salt Lake Valley via Rayleigh Wave Ellipticity Across a Temporary Geophone Array&quot; in journal The Seismic Record by Qicheng Zeng, Fan-Chi Lin, and Amir A. Allam. Detailed desciption in README in the zip file.</p>

opencc-by-4.0May 2022View details →
zenodo16/100

Geophone plate data from the Sulden/Solda basin (South Tyrol, Italy) 2014-2020

<p>This dataset contains the post-processing of 7 years of seismic data collected through geophone plates installed at the monitoring station of Stilfserbr&uuml;cke - Ponte Stelvio (South Tyrol, Italy) in the framework of the AQUASED project (<a href="http://www.mountain-eering.com/wp/mountain-eering/i-nostri-servizi/ricerca-e-sviluppo/studio-aquased/">http://www.mountain-eering.com/wp/mountain-eering/i-nostri-servizi/ricerca-e-sviluppo/studio-aquased/</a>) and analyzed in the paper &ldquo;Bedload fluxes in a glacier-fed river at multiple temporal scales&rdquo; by Coviello et al. (2022). The monitoring station is located in the Sulden/Solda basin (130 km<sup>2</sup>). Eight geophone plates are equipped with 10-Hz vertical geophones, which continuously measure the vibration induced by the impact of bedload at a sampling frequency of 5 kHz. The 8 geophone plates are installed along the cross section and extends for 4 m, corresponding to half of the channel width (8 m) from the mid-channel (ch 1) to the right bank (ch 8), and are fixed on a check dam with a cantilevered metal structure. From the raw seismic data, the following signal metrics have been extracted and constitute the dataset: the impulses (Imp/min) calculated with four different thresholds (0.01, 0.04, 0.16, 0.32 V), the maximum amplitude (V), the main frequency (Hz) and the integral of the squared amplitude (V<sup>2</sup>) over 1-min time window. This dataset provides the above-mentioned signal metrics for the period 2014 to 2020, separated per plate (from DB_aquased_ch1.dat to DB_aquased_ch8.dat).</p>

restrictedSep 2022View details →
zenodo16/100

z-component of geophone for OBS3

<p>Z component of geophone for OBS 3 for the turbidity current Flow 1 (10th October), which can be compared to ADCP M2 mooring data (E.g., Figure 2) . Measurements sampled at 1 kHz. Data is provided in .mseed format.&nbsp;</p>

restrictedcc-by-4.0Jul 2024View details →
zenodo16/100

z-component of geophone for OBS1

<p>Z component of geophone for OBS 1 for the two canyon-flushing turbidity currents (Flow 10, 14th - 17th January and Flow 11, 8-9th March). Measurements sampled at 1 kHz. Data is provided in .mseed format.&nbsp;</p>

restrictedcc-by-4.0Jul 2024View details →

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