Groundwater chemistry in the riparian zone of Caribou-Poker Creeks Research Watershed, Alaska, 2003

Groundwater was sample from wells in the riparian zone of a high permafrost (C3) and low permafrost watershed (C2) in Caribou-Poker Creeks Research Watershed in interior Alaska. Each sample was measured for a suite of solutes (anions, cations, dissolved organic carbon, total dissolved nitrogen, cond...

Full description

Bibliographic Details
Other Authors: JeremyJones
Format: Dataset
Language:unknown
Published: Bonanza Creek LTERBoreal Ecology Cooperative Research Unit University of Alaska FairbanksP.O. Box 756780 FairbanksAK99775USA907-474-6364907-474-6251 2006
Subjects:
dissolved organic carbon
water chemistry
watersheds
ammonium
groundwater
Caribou-Poker Creeks Research Watershed
permafrost
Alaska
Online Access:http://hdl.handle.net/10255/dryad.18049
http://metacat.lternet.edu/knb/metacat/knb-lter-bnz.147.8/xml
id ftdryad:oai:v1.datadryad.org:10255/dryad.18049
record_format openpolar
spelling ftdryad:oai:v1.datadryad.org:10255/dryad.18049 2023-05-15T15:53:35+02:00 Groundwater chemistry in the riparian zone of Caribou-Poker Creeks Research Watershed, Alaska, 2003 JeremyJones The tributary basins of Caribou Creek are all arbitrarily designated with a "C". The C2 basin is the sub-basin with the least amount of permafrost of the CPCRW sub-basins. As such, it has been often been studied intensively in conjunction with C3, the sub-basin with the greatest amount of permafrost. The basin trends to the south, with well-drained slopes and permafrost-underlain treeless muskeg in valley bottom. Although an extensive fire history has not been done, there was probably a stand-replacing fire early in this century (ca. 1925), with some large white spruce stands that survived from the earlier vegetation. -147.603928 W -147.5713145 E 65.15876438 N 65.14329713 S 2003-05-01 to 2003-08-31 2003-05-01 to 2003-08-31 2006-01-01 text/plain http://hdl.handle.net/10255/dryad.18049 http://metacat.lternet.edu/knb/metacat/knb-lter-bnz.147.8/xml unknown Bonanza Creek LTERBoreal Ecology Cooperative Research Unit University of Alaska FairbanksP.O. Box 756780 FairbanksAK99775USA907-474-6364907-474-6251 http://metacat.lternet.edu/knb/metacat/knb-lter-bnz.147.8/xml knb-lter-bnz.147.8 http://hdl.handle.net/10255/dryad.18049 Access to Data While metadata will be freely available to those requesting it, the data manager will assure that any restrictions on access to data sets in the database will be enforced. Data will not be released without proper permission first being obtained from the investigator who generated the data. Use of data Researchers should receive adequate acknowledgment for the use of their data by others and should be provided with copies of publications using their data. Users of data from the data base must be aware that data is not to be sold or redistributed.Citing Bonanza Creek LTER DatasetsIt is considered a matter of professional ethics to acknowledge the work of other scientists. Thus, the Data User will properly cite the Data Set in any publications or in the metadata of any derived data products that were produced using the Data Set. dissolved organic carbon water chemistry watersheds ammonium groundwater dataset 2006 ftdryad 2020-01-01T14:38:04Z Groundwater was sample from wells in the riparian zone of a high permafrost (C3) and low permafrost watershed (C2) in Caribou-Poker Creeks Research Watershed in interior Alaska. Each sample was measured for a suite of solutes (anions, cations, dissolved organic carbon, total dissolved nitrogen, conductivity, pH). To analyze spatial and temporal patterns of solutes in riparian groundwater and to determine calculate groundwater inputs to stream chemistry. Dataset Caribou-Poker Creeks Research Watershed permafrost Alaska Dryad Digital Repository (Duke University)
institution Open Polar
collection Dryad Digital Repository (Duke University)
op_collection_id ftdryad
language unknown
topic dissolved organic carbon
water chemistry
watersheds
ammonium
groundwater
spellingShingle dissolved organic carbon
water chemistry
watersheds
ammonium
groundwater
Groundwater chemistry in the riparian zone of Caribou-Poker Creeks Research Watershed, Alaska, 2003
topic_facet dissolved organic carbon
water chemistry
watersheds
ammonium
groundwater
description Groundwater was sample from wells in the riparian zone of a high permafrost (C3) and low permafrost watershed (C2) in Caribou-Poker Creeks Research Watershed in interior Alaska. Each sample was measured for a suite of solutes (anions, cations, dissolved organic carbon, total dissolved nitrogen, conductivity, pH). To analyze spatial and temporal patterns of solutes in riparian groundwater and to determine calculate groundwater inputs to stream chemistry.
author2 JeremyJones
format Dataset
title Groundwater chemistry in the riparian zone of Caribou-Poker Creeks Research Watershed, Alaska, 2003
title_short Groundwater chemistry in the riparian zone of Caribou-Poker Creeks Research Watershed, Alaska, 2003
title_full Groundwater chemistry in the riparian zone of Caribou-Poker Creeks Research Watershed, Alaska, 2003
title_fullStr Groundwater chemistry in the riparian zone of Caribou-Poker Creeks Research Watershed, Alaska, 2003
title_full_unstemmed Groundwater chemistry in the riparian zone of Caribou-Poker Creeks Research Watershed, Alaska, 2003
title_sort groundwater chemistry in the riparian zone of caribou-poker creeks research watershed, alaska, 2003
publisher Bonanza Creek LTERBoreal Ecology Cooperative Research Unit University of Alaska FairbanksP.O. Box 756780 FairbanksAK99775USA907-474-6364907-474-6251
publishDate 2006
url http://hdl.handle.net/10255/dryad.18049
http://metacat.lternet.edu/knb/metacat/knb-lter-bnz.147.8/xml
op_coverage The tributary basins of Caribou Creek are all arbitrarily designated with a "C". The C2 basin is the sub-basin with the least amount of permafrost of the CPCRW sub-basins. As such, it has been often been studied intensively in conjunction with C3, the sub-basin with the greatest amount of permafrost. The basin trends to the south, with well-drained slopes and permafrost-underlain treeless muskeg in valley bottom. Although an extensive fire history has not been done, there was probably a stand-replacing fire early in this century (ca. 1925), with some large white spruce stands that survived from the earlier vegetation.
-147.603928 W -147.5713145 E 65.15876438 N 65.14329713 S
2003-05-01 to 2003-08-31
2003-05-01 to 2003-08-31
genre Caribou-Poker Creeks Research Watershed
permafrost
Alaska
genre_facet Caribou-Poker Creeks Research Watershed
permafrost
Alaska
op_relation http://metacat.lternet.edu/knb/metacat/knb-lter-bnz.147.8/xml
knb-lter-bnz.147.8
http://hdl.handle.net/10255/dryad.18049
op_rights Access to Data While metadata will be freely available to those requesting it, the data manager will assure that any restrictions on access to data sets in the database will be enforced. Data will not be released without proper permission first being obtained from the investigator who generated the data. Use of data Researchers should receive adequate acknowledgment for the use of their data by others and should be provided with copies of publications using their data. Users of data from the data base must be aware that data is not to be sold or redistributed.Citing Bonanza Creek LTER DatasetsIt is considered a matter of professional ethics to acknowledge the work of other scientists. Thus, the Data User will properly cite the Data Set in any publications or in the metadata of any derived data products that were produced using the Data Set.
_version_ 1766388698505543680

Similar Items