Checking for non-preferred file/folder path names (may take a long time depending on the number of files/folders) ...
This resource contains some files/folders that have non-preferred characters in their name. Show non-conforming files/folders.
This resource contains content types with files that need to be updated to match with metadata changes. Show content type files that need updating.
SSHCZO -- Geology, Soil Water -- Infiltrometer - Shale Hills & Missed Grouse -- Shale Hills -- (2013-2013)
| Authors: |
|
|
|---|---|---|
| Owners: |
|
This resource does not have an owner who is an active HydroShare user. Contact CUAHSI (help@cuahsi.org) for information on this resource. |
| Type: | Resource | |
| Storage: | The size of this resource is 158.7 KB | |
| Created: | Nov 19, 2019 at 6:26 a.m. | |
| Last updated: | Dec 23, 2019 at 11:58 p.m. | |
| Citation: | See how to cite this resource | |
| Content types: | Single File Content |
| Sharing Status: | Public |
|---|---|
| Views: | 1653 |
| Downloads: | 22 |
| +1 Votes: | Be the first one to this. |
| Comments: | No comments (yet) |
Abstract
Infiltrometer data were collected from 5-6 sites around the infiltration experiments. Map is provided in the spreadsheet file. IN2-W Turf Tec double ring infiltrometer was used. Inner ring diameter is 0.06 m. Steady state tests were performed by measuring the amount of infiltration after a fixed time. For the transient method the infiltration amount was recorded every minute. Water was added (amount recorded) when necessary to keep the float within the recording interval. Multiple depths were tested when possible (10, 20 30 cm).
Subject Keywords
Coverage
Spatial
Temporal
| Start Date: | |
|---|---|
| End Date: |
Content
ReadMe.md
SSHCZO -- Geology, Soil Water -- Infiltrometer - Shale Hills & Missed Grouse -- Shale Hills -- (2013)
OVERVIEW
Description/Abstract
Infiltrometer data were collected from 5-6 sites around the infiltration experiments. Map is provided in the spreadsheet file. IN2-W Turf Tec double ring infiltrometer was used. Inner ring diameter is 0.06 m. Steady state tests were performed by measuring the amount of infiltration after a fixed time. For the transient method the infiltration amount was recorded every minute. Water was added (amount recorded) when necessary to keep the float within the recording interval. Multiple depths were tested when possible (10, 20 30 cm).
Creator/Author
Toran, Laura
CZOs
Shale Hills
Contact
Laura Toran, Temple University, ltoran@temple.edu
Subtitle
Level 1 - Quality-controlled Data
SUBJECTS
Disciplines
Hydrology
Topics
Geology|Soil Water
Subtopic
Infiltrometer - Shale Hills & Missed Grouse
Keywords
Infiltration experiment|Shale Hills|Missed Grouse|geophysical monitoring
Variables
Time|level (mm)
Variables ODM2
Water depth
TEMPORAL
Date Start
2013-10-13
Date End
2013-11-30
SPATIAL
Field Areas
Susquehanna Shale Hills Critical Zone Observatory
Location
Shale Hills
North latitude
40.66593819
South latitude
40.6637321
West longitude
-77.90747404
East longitude
-77.90100215
REFERENCE
Citation
The following acknowledgment should accompany any publication or citation of these data: Logistical support and/or data were provided by the NSF-supported Shale Hills Susquehanna Critical Zone Observatory.
CZO ID
4828
Additional Metadata
| Name | Value |
|---|---|
| czos | Shale Hills |
| czo_id | 4828 |
| citation | The following acknowledgment should accompany any publication or citation of these data: Logistical support and/or data were provided by the NSF-supported Shale Hills Susquehanna Critical Zone Observatory. |
| keywords | Infiltration experiment, Shale Hills, Missed Grouse, geophysical monitoring |
| subtitle | Level 1 - Quality-controlled Data |
| variables | Time, level (mm) |
| disciplines | Hydrology |
How to Cite
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
Comments
There are currently no comments
New Comment