Biogeochemistry of Permafrosted/NonPermafrosted Watersheds in CPCRW: Summer 1995
Chemical measurements of groundwater, soil water and stream water were made in watersheds C2 and C3 in CPCRW (DOC, DON, NO3-N, NH4-N, Al, Mg, Ca, Mn, Si, K, Na, SO4 and conductivity). One watershed C3 had extensive permafrost and the other C2 had limited permafrost. Stream discharge data was collect...
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Bonanza Creek LTERBoreal Ecology Cooperative Research Unit University of Alaska FairbanksP.O. Box 756780 FairbanksAK99775USA907-474-6364907-474-6251
1997
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Online Access: | http://hdl.handle.net/10255/dryad.11903 http://metacat.lternet.edu/knb/metacat/knb-lter-bnz.25.8/xml |
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ftdryad:oai:v1.datadryad.org:10255/dryad.11903 2023-05-15T17:55:41+02:00 Biogeochemistry of Permafrosted/NonPermafrosted Watersheds in CPCRW: Summer 1995 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 1985-07-14 to 1995-09-03 1985-07-14 to 1995-09-03 1997-07-26 text/plain http://hdl.handle.net/10255/dryad.11903 http://metacat.lternet.edu/knb/metacat/knb-lter-bnz.25.8/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.25.8/xml knb-lter-bnz.25.8 http://hdl.handle.net/10255/dryad.11903 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. biogeochemistry permafrost hydrology dissolved organic carbon dissolved organic nitrogen dissolved inorganic nitrogen nitrate ammonium calcium magnesium potassium aluminum sodium manganese silica sulfate carbon and nitrogen flux dataset 1997 ftdryad 2020-01-01T14:26:38Z Chemical measurements of groundwater, soil water and stream water were made in watersheds C2 and C3 in CPCRW (DOC, DON, NO3-N, NH4-N, Al, Mg, Ca, Mn, Si, K, Na, SO4 and conductivity). One watershed C3 had extensive permafrost and the other C2 had limited permafrost. Stream discharge data was collected from permanently installed flumes. Soil water retained within the rooting zone (0.3 - 0.5 m) was high in DOC, DON and DIN but low in dissolved minerals (dominantly Ca, Mg and Na) and conductivity. The reverse was true for groundwater from springs and wells. Permafrost in C3 prevented deep percolation of water and generated stormflows rich in DOC. Stormflow accounted for 24% of total streamflow in C3 but only 3% of total streamflow in C2. The presence of permafrost appears to result in higher fluxes of DOC, DON and DIN into stream water from upland soils. Dataset permafrost Dryad Digital Repository (Duke University) |
institution |
Open Polar |
collection |
Dryad Digital Repository (Duke University) |
op_collection_id |
ftdryad |
language |
unknown |
topic |
biogeochemistry permafrost hydrology dissolved organic carbon dissolved organic nitrogen dissolved inorganic nitrogen nitrate ammonium calcium magnesium potassium aluminum sodium manganese silica sulfate carbon and nitrogen flux |
spellingShingle |
biogeochemistry permafrost hydrology dissolved organic carbon dissolved organic nitrogen dissolved inorganic nitrogen nitrate ammonium calcium magnesium potassium aluminum sodium manganese silica sulfate carbon and nitrogen flux Biogeochemistry of Permafrosted/NonPermafrosted Watersheds in CPCRW: Summer 1995 |
topic_facet |
biogeochemistry permafrost hydrology dissolved organic carbon dissolved organic nitrogen dissolved inorganic nitrogen nitrate ammonium calcium magnesium potassium aluminum sodium manganese silica sulfate carbon and nitrogen flux |
description |
Chemical measurements of groundwater, soil water and stream water were made in watersheds C2 and C3 in CPCRW (DOC, DON, NO3-N, NH4-N, Al, Mg, Ca, Mn, Si, K, Na, SO4 and conductivity). One watershed C3 had extensive permafrost and the other C2 had limited permafrost. Stream discharge data was collected from permanently installed flumes. Soil water retained within the rooting zone (0.3 - 0.5 m) was high in DOC, DON and DIN but low in dissolved minerals (dominantly Ca, Mg and Na) and conductivity. The reverse was true for groundwater from springs and wells. Permafrost in C3 prevented deep percolation of water and generated stormflows rich in DOC. Stormflow accounted for 24% of total streamflow in C3 but only 3% of total streamflow in C2. The presence of permafrost appears to result in higher fluxes of DOC, DON and DIN into stream water from upland soils. |
format |
Dataset |
title |
Biogeochemistry of Permafrosted/NonPermafrosted Watersheds in CPCRW: Summer 1995 |
title_short |
Biogeochemistry of Permafrosted/NonPermafrosted Watersheds in CPCRW: Summer 1995 |
title_full |
Biogeochemistry of Permafrosted/NonPermafrosted Watersheds in CPCRW: Summer 1995 |
title_fullStr |
Biogeochemistry of Permafrosted/NonPermafrosted Watersheds in CPCRW: Summer 1995 |
title_full_unstemmed |
Biogeochemistry of Permafrosted/NonPermafrosted Watersheds in CPCRW: Summer 1995 |
title_sort |
biogeochemistry of permafrosted/nonpermafrosted watersheds in cpcrw: summer 1995 |
publisher |
Bonanza Creek LTERBoreal Ecology Cooperative Research Unit University of Alaska FairbanksP.O. Box 756780 FairbanksAK99775USA907-474-6364907-474-6251 |
publishDate |
1997 |
url |
http://hdl.handle.net/10255/dryad.11903 http://metacat.lternet.edu/knb/metacat/knb-lter-bnz.25.8/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 1985-07-14 to 1995-09-03 1985-07-14 to 1995-09-03 |
genre |
permafrost |
genre_facet |
permafrost |
op_relation |
http://metacat.lternet.edu/knb/metacat/knb-lter-bnz.25.8/xml knb-lter-bnz.25.8 http://hdl.handle.net/10255/dryad.11903 |
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_ |
1766163660492767232 |