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CRBCZO -- Climate, Stable Isotopes, Well Water Levels -- White Clay Creek Transect A floodplain, Transect C -- (2012-2012)
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| Created: | Nov 19, 2019 at 3:47 a.m. (UTC) | |
| Last updated: | Dec 23, 2019 at 10:48 p.m. (UTC) | |
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Abstract
Diana Karwan, Olesya Lazareva, Donald L. Sparks, Anthony Aufdenkampe
The Christina River Basin-Critical Zone Observatory (CRB-CZO), located in the Piedmont region of Southeastern Pennsylvania and northern Delaware, is a partnership between the University of Delaware and the Stroud Water Research Center. At Transect A of the White Clay Creek Watershed (WCCW) of the CRB-CZO, the composition of soil pore-waters and stream was investigated to understand how the geochemical dynamics of Fe- and Mn- along redox gradients affect the C cycle within a floodplain aquifer.
Soil pore-water was collected with in-situ borosilicate glass samplers (50 mm long, 20 mm diameter, 1 μm pore size, Ecotech, Germany) with the attached PTFE (Teflon) tubes (3/1.5 mm i.d./o.d) to sampling bottle. Six samplers were deployed on both sides of the floodplain within a 10-40 cm thick dark organic-rich silty soil that represents a buried pre-settlement wetland soil, underlain gravel, and stream. No pore-water was extracted from the pre-settlement deposits due to unsaturated conditions. Water sampling was carried out for about 14 months (July, 2011 - September, 2012) on biweekly basis except last 2 months in order to evaluate temporal and spatial biogeochemical dynamics of floodplain aquifer under a variety of meteorological and hydrologic conditions. In total, 103 soil pore-water samples were collected and analyzed for DOC, Fe and Mn, pH, temperature, alkalinity, conductivity, major anions, major cations, δD, and δ18O.
Subject Keywords
Coverage
Spatial
Temporal
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Content
ReadMe.md
CRBCZO -- Climate, Stable Isotopes, Well Water Levels -- White Clay Creek Transect A floodplain, Transect C -- (2012)
OVERVIEW
Description/Abstract
Diana Karwan, Olesya Lazareva, Donald L. Sparks, Anthony Aufdenkampe The Christina River Basin-Critical Zone Observatory (CRB-CZO), located in the Piedmont region of Southeastern Pennsylvania and northern Delaware, is a partnership between the University of Delaware and the Stroud Water Research Center. At Transect A of the White Clay Creek Watershed (WCCW) of the CRB-CZO, the composition of soil pore-waters and stream was investigated to understand how the geochemical dynamics of Fe- and Mn- along redox gradients affect the C cycle within a floodplain aquifer. Soil pore-water was collected with in-situ borosilicate glass samplers (50 mm long, 20 mm diameter, 1 μm pore size, Ecotech, Germany) with the attached PTFE (Teflon) tubes (3/1.5 mm i.d./o.d) to sampling bottle. Six samplers were deployed on both sides of the floodplain within a 10-40 cm thick dark organic-rich silty soil that represents a buried pre-settlement wetland soil, underlain gravel, and stream. No pore-water was extracted from the pre-settlement deposits due to unsaturated conditions. Water sampling was carried out for about 14 months (July, 2011 - September, 2012) on biweekly basis except last 2 months in order to evaluate temporal and spatial biogeochemical dynamics of floodplain aquifer under a variety of meteorological and hydrologic conditions. In total, 103 soil pore-water samples were collected and analyzed for DOC, Fe and Mn, pH, temperature, alkalinity, conductivity, major anions, major cations, δD, and δ18O.
Creator/Author
Karwan, Diana L.|Lazareva, Olesya
CZOs
Christina
Contact
Olesya Lazareva, University of Delaware Environmental Institute, Newark DE , 19716 Diana L. Karwan, Department of Forest Resources, University of Minnesota, St. Paul, MN 55108
SUBJECTS
Disciplines
Biogeochemistry|Climatology / Meteorology|Geochemistry / Mineralogy|Hydrology|Soil Science / Pedology
Topics
Climate|Stable Isotopes|Well Water Levels
Keywords
Hydrology|water isotopes|White Clay Creek Watershed|Transect
Variables
pH|Temperature|Specific conductance|Alkalinity_ total|Oxygen-18|Deuterium|Water level|Calcium|Potassium|Magnesium|Manganese|Sodium|Silicon|Sulfur
Variables ODM2
Alkalinity, total|Calcium|Deuterium|Magnesium|Manganese|Oxygen-18|pH|Potassium, dissolved|Silicon|Sodium, dissolved|Specific conductance|Sulfur|Temperature|Water level
TEMPORAL
Date Start
2012-09-24
Date End
2012-12-19
SPATIAL
Field Areas
Agricultural Endmember: South Branch Doe Run|Boulton Run|Transect A
Location
White Clay Creek Transect A floodplain, Transect C
North latitude
39.867490000000004
South latitude
39.86232375
West longitude
-75.78814197
East longitude
-75.782027
REFERENCE
Citation
Karwan and Lazareva, 2012
CZO ID
2978
Award Grant Numbers
National Science Foundation, Earth Sciences Division - 0724971
Additional Metadata
| Name | Value |
|---|---|
| czos | Christina |
| czo_id | 2978 |
| citation | Karwan and Lazareva, 2012 |
| keywords | Hydrology, water isotopes, White Clay Creek Watershed, Transect |
| variables | pH, Temperature, Specific conductance, Alkalinity_ total, Oxygen-18, Deuterium, Water level, Calcium, Potassium, Magnesium, Manganese, Sodium, Silicon, Sulfur |
| disciplines | Biogeochemistry, Climatology / Meteorology, Geochemistry / Mineralogy, Hydrology, Soil Science / Pedology |
Credits
Funding Agencies
This resource was created using funding from the following sources:
| Agency Name | Award Title | Award Number |
|---|---|---|
| National Science Foundation, Earth Sciences Division | None | 0724971 |
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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