soil moisture
| Abstract | |
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| Gaius Shaver, James A Laundre, 2023 Summer soil temperature and moisture at the Anaktuvuk River Moderately burned site from 2010 to 2013. 10.6073/pasta/6efb5c5e73e83ac58692b0e5ec23730e |
Soil moisture and temperature were recorded at the Anaktuvuk River burn area during the summers from 2010 to 2013. Six sensors were deployed and measured temperature on half-hourly intervals over the summer and into the fall depending on battery function. Sensors were place in a hexagonal shape around a central datalogger. Note that over time sensor depths changed due to frost heave and other environmental factors. All data contained should be treated as suspect where sensors may have been at surface. These sensors were removed August 20, 2013, no replacement sensors were installed. |
| Gaius Shaver, James A Laundre, 2014 Summer soil temperature and moisture at the Anaktuvuk River Unburned site from 2010 to 2013. 10.6073/pasta/13cfe1cfa528cb7fe15bd8fb672b68d3 |
Soil moisture and temperature were recorded at the Anaktuvuk River burn area during the summers from 2010 to 2013. Six sensors were deployed and measured temperature on half-hourly intervals over the summer and into the fall depending on battery function. Sensors were place in a hexagonal shape around a central datalogger. Note that over time sensor depths changed due to frost heave and other environmental factors. All data contained should be treated as suspect where sensors may have been at surface. These sensors were removed August 23, 2013, no replacement sensors were installed. |
| Gaius Shaver, James A Laundre, 2014 Summer soil temperature and moisture at the Anaktuvuk River Severely burned site from 2010 to 2013. 10.6073/pasta/3094e3e293703580c95e17ddce51af65 |
Soil moisture and temperature were recorded at the Anaktuvuk River burn area during the summers from 2010 to 2013. Six sensors were deployed and measured temperature on half-hourly intervals over the summer and into the fall depending on battery function. Sensors were place in a hexagonal shape around a central data logger. Note that over time sensor depths changed due to frost heave and other environmental factors. All data contained should be treated as suspect where sensors may have been at surface. These sensors were removed August 20, 2013, no replacement sensors were installed. |
| Abstract | |
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| Donald Schell, 1993 Arctic LTER 1991: Percent moisture, bulk density, percent loss on ignition and percent organic carbon were measured for peat collected from soils in the Imnavait Creek watershed.. 10.6073/pasta/027e46f118de965c56f556b76518c06f |
Percent moisture, bulk density, percent loss on ignition and percent organic carbon were measured for peat collected from soils in the Imnavait Creek watershed. |
| Gaius Shaver, 2005 Plant available NH4, NO3, and PO4 was determined at sites near ARC LTER Toolik acidic tundra and at a toposequence along the floodplain of the Sagavanirktuk River using 2 N KCL and weak HCL extracts, Arctic LTER 1987 to 2002. 10.6073/pasta/48fd52a09bf83e6c6bcecb49b48e9358 |
Plant available NH4, NO3, and PO4 was determined at sites near ARC LTER Toolik acidic tundra and at a toposequence along the floodplain of the Sagavanirktuk River using 2 N KCL and weak HCL extracts. This file complies data collected at different times from 1987 through 2001 and includes initial extracts taken for buried bag method of net nitrogen mineralization. |
| Donald Schell, 1989 Radiocarbon dates for an elevational gradient by Toolik Lake, North Slope of Alaska 1988.. 10.6073/pasta/90a45bbe7265d037228609a2054afac5 |
Two cores of peat, approximately 15 cm2, were cut to the depth at which mineral soils were encountered at each site. The sites of sampling correspond to an elevational gradient leading from the lakeside upslope to the begining of the water track at the ridgetop. Each sample was divided into three sections, one section to be used for radiocarbon age , one for loss on ignition, and the remainder to be kept for future needs. |
| Gaius Shaver, 2006 Nitrogen mineralization was determined on Arctic LTERToolik and Sag River tussock tundra using the buried bag method, Toolik Field Station, Alaska, Arctic LTER 1989-2013.. 10.6073/pasta/79e01a508bb9021e265eec2a8201b2f9 |
Nitrogen mineralization was determined on LTER and Sag River tussock tundra using the buried bag method. Yearly bags have been deployed every August since 1990. |
| Abstract | |
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| Gaius Shaver, 2013 Summary of soil temperature, moisture, and thaw depth for 14 chamber flux measurements sampled near LTER shrub sites at Toolik Field Station, Alaska, summer 2012.. 10.6073/pasta/7ccf390e6fe4824e93b7a2b844605a40 |
Soil temperature at 5cm and 10cm depth [°C], volumetric water content (VWC) [%] and depth of thaw [cm] for 14 shrub canopy flux plots measured in vicinity of the Toolik Field Station, AK in 2012. |
| Abstract | |
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| Gaius Shaver, James A Laundre, 2021 Soil temperatures and moisture for Arctic Long Term Experimental Research (ARC LTER) heath experimental plots, Toolik Field Station, North Slope Alaska for 2001-2018. . 10.6073/pasta/5bec91673a0bd177777381b490247241 |
Soil temperatures at 2 depths, 5 and 10 cm, canopy temperatures and soil moisture at 10 cm were measured in a heath tundra Arctic Long Term Experimental Research (ARC-LTER) site at Toolik Lake Field Station, North slope, Alaska. Air temperature and relative humidity and global radiation were also measured but are presented in another dataset. Only control and nutrient addition (nitrogen plus phosphorus ) treatments plots were measured . |
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| Jeff Welker, Paddy Sullivan, 2011 Welker ITEX Tussock Microclimate Data. 10.6073/pasta/7cb89929b6e87969e416add3dfea36f5 |
Hourly air temperature, humidity, wind speed, soil temperature and soil water data from the control area of the ITEX tussock tundra snowfence study site |
| Jeff Welker, Paddy Sullivan, 2011 Welker IPY snow fence shrub site soil temperatures and soil water content Toolik, Alaska 2008.. 10.6073/pasta/4966e339bb9da53ce005bc75b84eab56 |
Soil temperature from three locations on the eastern side of the Toolik River where by snow fences were established as part of IPY. This is a study of how soil temperatures at 10 cm and soil moisture change across the summer at our IPY snow fence site . |
