Global identifier:
Doi(
"10.1594/PANGAEA.940914",
)
DataMeasurements(
DataMeasurements {
domain: Unspecified,
station: None,
measured_variables: [
"Binary Object",
"DATE/TIME",
"DEPTH, sediment/rock",
"Sample comment",
],
methods: [],
},
)
Comment: The source borehole (SB) was equipped with a borehole sparker SBS42 (http://geotomographie.de/assets/equipment/Productsheet-SBS42.pdf) generating a highly repeatable signal. The sparker was moved from 13 - 8 m depth connected to an impulse generator IPG5000 (http://geotomographie.de/assets/equipment/Productsheet-IPG800+5000.pdf) that operates at 5 kV for high voltage power supply. Two hydrophone strings (BHC5 - http://geotomographie.de/assets/equipment/Productsheet-BHC5.pdf) with 17/24 hydrophones of small diameter were mounted to receiver borehole 1 (RB1) and receiver borehole 2 (RB2) accordingly from 8 - 13 m depth with a spacing of 1 m between each hydrophone. The first set of shots was released at 13 m depth and the sparker was pulled up with a shot increment of 1 m. In both receiver boreholes we recorded and stacked 10 (5 regular + 5 repetetive) shots for each depth during the baseline measurement and every monitoring cycle. Our sampling intervall was 20.833 µs and the recording length covered 30 ms.
Tags: TestUM-Aquifer ? Wittstock/Dosse ? electrical conductivity ? methane gas injection ? relative hydraulic conductivity ? seismic crosshole ?
Region: Wittstock, Brandenburg, Germany
Bounding boxes: 12.504137° .. 12.50418° x 53.193463° .. 53.193492°
License: cc-by/4.0
Language: Englisch/English
Issued: 2022-02-10
Modified: 2024-04-20
Time ranges: 2019-04-29 - 2020-05-05
Accessed 1 times.