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Created: | Nov 19, 2019 at 6:44 a.m. | |
Last updated: | Dec 24, 2019 at 12:04 a.m. | |
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Content types: | Single File Content |
Sharing Status: | Public |
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Abstract
To quantify “truly dissolve” phases of solute concentrations, groundwater and stream water samples collected at the Shale Hills Critical Zone observatory were filtered a sequence of filters with different pore sizes (1μm, 0.45 μm, 0.22 μm, 100KDa, and sometimes 1 KDa). Approximately 1L of water samples were taken at the Shale Hills CZO. The samples were retrieved to the laboratory within an hour and were filtered at the laboratory. The samples were filtered:
Filter pore size filter material filter manufacture filtration method
1μm Cellulose nitrate membrane filters Whatman vacuum filtration
0.45 μm Polyethersulfone membrane filter Pall Corporation vacuum filtration
0.22 μm Polyethersulfone membrane filter Pall Corporation vacuum filtration
100KDa Regenerated Cellulose filter EMD Millipore ultra-filtration
1KDa Regenerated Cellulose filter EMD Millipore ultra-filtration
The filtrates were acidified (1% v/v) using Optima Nitric acid. Major cations and silica were analyzed on an inductively coupled plasma–optical emission spectrometer (ICP– OES).
Subject Keywords
Coverage
Spatial
Temporal
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Additional Metadata
Name | Value |
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czos | Shale Hills |
czo_id | 5273 |
citation | The following acknowledgment should accompany any publication or citation of these data: Logistical support and/or data were provided by the NSF-supported Susquehanna Shale Hills Critical Zone Observatory. |
keywords | groundwater chemistry, stream water chemistry, sequential filtration |
subtitle | Level 1 - Quality Controlled Data |
variables | rundate, #, location, date, depth, filter size, filter number, Al (ug/mL), Ba (ug/mL), Ca (ug/mL), Fe (ug/mL), K (ug/mL), Mg (ug/mL), Mn (ug/mL), Na (ug/mL), Ni (ug/mL), P (ug/mL), Si (ug/mL), Sr (ug/mL), Ti (ug/mL), Zn (ug/mL) |
disciplines | Geochemistry / Mineralogy, Water Chemistry |
How to Cite
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
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