LLC VOW 02 (2017-02-03 to 2020-11-03)
Download: llc_vow_02_20170203_20201103-3.xlsx
This resource is part of the Living Lakes Canada Upper Columbia Basin Groundwater Monitoring Program, and contains a groundwater monitoring record for LLC VOW 02 from 2017-02-03 to 2020-11-03. Water levels are reported in meters below ground surface.
Resource metadata
| Field | Value |
| Data last updated | March 16, 2021 |
| Metadata last updated | March 12, 2021 |
| Created | March 12, 2021 |
| Format | XLSX |
| License | CC-BY-NC-SA-4.0 |
| Data collection info | Continuous (Hourly since 2018-07-19, 0.5 hour interval prior to 2018-07-19) water level data were collected with a HOBO U20 water level data logger. The water level is determined by continuously collecting the absolute pressure of the water column above a sensor, compensating it for atmospheric pressure, and calibrating it with reference water levels that are collected manually. The atmospheric pressure is measured by a HOBO U20 level logger (0- 4m range) that is installed in the airspace at the top of the wellhead. Manual water level level measurements were collected using either a Heron or Solinst water level tape (sounding tape). |
| Data processing | Data compensation and water level referencing were completed using HOBOWare Pro software. For the conversion of pressure to water level, the water density of freshwater is adjusted for water temperature. Pressures are converted to water level based on manual water level readings using a water level tape. The pressure data were reviewed to ensure they are within the factory calibrated range of the sensor. Manual and logger data were compared to identify potential instrument drift. The differences between the manual measurements (5) and the data logger were all less than 2.5 cm. |
| Data type | lab |
| Datastore active | False |
| Datastore contains all records of source file | False |
| Has views | True |
| Hash | 9c30c26b8e120c3ed8e47ae55215fe2e |
| Header row | 1 |
| Id | f85b757f-feb8-4049-99ea-54c45f27e21e |
| Load status | Table was successfully loaded: 45596 rows |
| Mimetype | application/vnd.openxmlformats-officedocument.spreadsheetml.sheet |
| Package id | faa8fd9d-0942-4c1e-9b81-d813474d67ae |
| Position | 0 |
| Resource citation | Living Lakes Canada Upper Columbia Basin Groundwater Monitoring Program. (2021) LLC VOW 02 (2017-02-03 to 2020-11-03). Columbia Basin Water Hub. (Resource) Creston. (DOI). |
| Resource data disclaimer | No warranty or guarantee exists that the information is accurate, complete, current, or suitable for any purpose. The individual user must confirm the accuracy of the data and whether it will be appropriate for their purpose themselves. |
| Resource location | Creston, S Goat River Road |
| Size | 1 MiB |
| State | active |
| Url type | upload |
| Waterhub certified | Certified |
| Waterhub grade | Technical Research Grade |
| Citation (Required) | Living Lakes Canada Upper Columbia Basin Groundwater Monitoring Program. (2021) LLC VOW 02 (2017-02-03 to 2020-11-03). Columbia Basin Water Hub. (Resource) Creston. (DOI). |
| Resource Location | Creston, S Goat River Road |
| Data Collection Information | Continuous (Hourly since 2018-07-19, 0.5 hour interval prior to 2018-07-19) water level data were collected with a HOBO U20 water level data logger. The water level is determined by continuously collecting the absolute pressure of the water column above a sensor, compensating it for atmospheric pressure, and calibrating it with reference water levels that are collected manually. The atmospheric pressure is measured by a HOBO U20 level logger (0- 4m range) that is installed in the airspace at the top of the wellhead. Manual water level level measurements were collected using either a Heron or Solinst water level tape (sounding tape). |
| Data Processing | Data compensation and water level referencing were completed using HOBOWare Pro software. For the conversion of pressure to water level, the water density of freshwater is adjusted for water temperature. Pressures are converted to water level based on manual water level readings using a water level tape. The pressure data were reviewed to ensure they are within the factory calibrated range of the sensor. Manual and logger data were compared to identify potential instrument drift. The differences between the manual measurements (5) and the data logger were all less than 2.5 cm. |
| Data Disclaimer | No warranty or guarantee exists that the information is accurate, complete, current, or suitable for any purpose. The individual user must confirm the accuracy of the data and whether it will be appropriate for their purpose themselves. |
| Water Hub Data Grade | Technical Research Grade |
| Date of Most Recent Water Hub QA/QC | |
| Data type | Laboratory Results |
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