SESAR: 10.58052/IE118008A

Field

Value

IGSN

10.58052/IE118008A

Name

Cov_flux_140

Other Name(s)

Not Provided

External Parent Name

Not Provided

External Parent Object Type

Not Provided

Publish Date

2026-10-01

Last Updated

2026-10-01

Field

Value

Object Type

General sample types > Individual sample

General Material Type

Non-volcanic gas

Material Types

Not Provided

Field Name

Fluids from the Eastern Carpathians

Sample Description

Diffuse soil CO2 degassing

Age (min)

Not Provided

Age (max)

Not Provided

Age Description

Not Provided

Geological Age

Not Provided

Geological Unit

Not Provided

Sample Size

Not Provided

Purpose

Flux quantification

Field

Value

Latitude

45.851108

Longitude

26.172011

Latitude End

Not Provided

Longitude End

Not Provided

Easting

5077838.073490819

Northing

435715.2089034513

UTM Zone

Vertical Datum

Not Provided

Depth (min)

Not Provided

Depth (max)

Not Provided

Depth Scale

Not Provided

Elevation

Not Provided

Elevation End

Not Provided

Navigation Type/Location Method

Not Provided

Locality

Covasna

Locality Description

Not Provided

Location Description

Not Provided

Primary Location Name

Not Provided

Primary Location Type

Not Provided

Continent

Not Provided

Country

Romania

Province

Not Provided

County

Not Provided

City/Township

Not Provided

Field

Value

Current Archive

Not Provided

Current Archive Contact

Not Provided

Original Archive

Not Provided

Original Archive Contact

Not Provided

Availability

Not Provided

Field

Value

Cruise/Field Program

Not Provided

Platform

Not Provided

Launch Platform

Not Provided

Launch Label

Not Provided

Collectors

Institution: Babeș-Bolyai University (Babeș-Bolyai Tudományegyetem)

Location: Cluj-Napoca, Romania

Individual: Kis, Boglárka-Mercedesz

Location: Romania

Sampling Method

Accumulation chamber

Sampling Method Detail

The accumulation chamber method measures diffuse soil gas flux by placing an open-bottomed chamber (accumulation chamber) of known volume and basal area on the ground and circulating its air through an infrared detector. As soil gas collects inside, the CO₂ concentration rises. The flux is calculated from the initial linear rate of increase (dC/dt), scaled by the chamber's volume-to-area ratio and corrected for air pressure and temperature.

Sampling Start Date

2021-08-28

Sampling End Date

Not Provided

Sampling Date Precision

day

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