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
Chemical measurements of groundwater, soil water and stream water were made in watersheds C2 and C3 ...
We examined the impact of permafrost on dissolved organic matter (DOM) composition in Caribou-Poker ...
Groundwater samples were collected from an extensive monitoring well network in a discontinuous perm...
This study focuses on a mid-sized watershed of upper Ogilvie River (~4,500 km2 at the western extent...
The hydrogeochemistry of nine streams in the Caribou-Poker Creeks Research Watershed (CPCRW) during ...
Fundamental knowledge of groundwater systems in areas of permafrost is often lacking. The likelihood...
In order to better understand the water cycle in the discontinuous permafrost area, field observatio...
Prior to this investigation, denitrification had not been intensively measured in headwater catchmen...
This study investigates the runoff process and groundwater behavior in a subarctic watershed called ...
Groundwater flow regimes in the seasonally thawed soils in areas of continuous permafrost are relati...
To better understand groundwater–surface water dynamics in high latitude areas, we conducted a field...
This research project examines the extent of connection between groundwater and surface water near a...
In the continuous permafrost zone, unfrozen ground may exist beneath large lakes and streams. Sub-la...
In the continuous permafrost zone, unfrozen ground may exist beneath large lakes and streams. Sub-la...
Yearly file describing the samples collected at various sites near Toolik Research Station (68 38'N,...
Chemical measurements of groundwater, soil water and stream water were made in watersheds C2 and C3 ...
We examined the impact of permafrost on dissolved organic matter (DOM) composition in Caribou-Poker ...
Groundwater samples were collected from an extensive monitoring well network in a discontinuous perm...
This study focuses on a mid-sized watershed of upper Ogilvie River (~4,500 km2 at the western extent...
The hydrogeochemistry of nine streams in the Caribou-Poker Creeks Research Watershed (CPCRW) during ...
Fundamental knowledge of groundwater systems in areas of permafrost is often lacking. The likelihood...
In order to better understand the water cycle in the discontinuous permafrost area, field observatio...
Prior to this investigation, denitrification had not been intensively measured in headwater catchmen...
This study investigates the runoff process and groundwater behavior in a subarctic watershed called ...
Groundwater flow regimes in the seasonally thawed soils in areas of continuous permafrost are relati...
To better understand groundwater–surface water dynamics in high latitude areas, we conducted a field...
This research project examines the extent of connection between groundwater and surface water near a...
In the continuous permafrost zone, unfrozen ground may exist beneath large lakes and streams. Sub-la...
In the continuous permafrost zone, unfrozen ground may exist beneath large lakes and streams. Sub-la...
Yearly file describing the samples collected at various sites near Toolik Research Station (68 38'N,...
Chemical measurements of groundwater, soil water and stream water were made in watersheds C2 and C3 ...
We examined the impact of permafrost on dissolved organic matter (DOM) composition in Caribou-Poker ...
Groundwater samples were collected from an extensive monitoring well network in a discontinuous perm...