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Grassland soils in the Boreal Cordillera Ecozone
2023.2.2.12 · Subsérie · 2007-2009
Parte de Dr. Paul Sanborn fonds

A comparative study of grassland soils at 3 sites in northwestern BC and southern Yukon was published as:
Sanborn, P. 2010. Topographically controlled grassland soils in the Boreal Cordillera ecozone, northwestern Canada. Canadian Journal of Soil Science 90: 89-101. https://doi.org/10.4141/CJSS09048

This grew out of a field trip with Ministry of Forests range personnel to the Stikine and Tuya River valleys, near Telegraph Creek BC on August 27-28, 2007. (Two pedons were sampled in 2007, BC07-03 and BC07-04, but those results were not included in the paper.)

In August 2008, Dr. Paul Sanborn returned to the Stikine to sample pedon BC08-06, after field work in Yukon which collected the other two pedons used in the paper, from near Carmacks (Y08-39) and Kluane Lake (Y08-41). (An additional pedon from Kluane, Y08-43, was sampled and analyzed, but it was from a forested site and was not included in the paper.)

Klutlan Glacier soils study data
2023.2.2.13.1 · Dossiê/Processo · 2007-2008
Parte de Dr. Paul Sanborn fonds

File contains the following data sets:

  • S925finl.xls [chemical analysis data, Ministry of Forests & Range, Analytical Chemistry Laboratory for pedons Y07-06 & Y07-07; also includes data for BC07-03 & BC07-04 (Boreal Cordillera grassland soils – see associated file note)]
  • S1007finl_revised2.xls [chemical analysis data, Ministry of Forests & Range, Analytical Chemistry Laboratory for pedons Y07-06 & Y07-07: oxalate & dithionite extractions, P retention; also includes P retention data for Nazko pedons BC07-07 & BC07-09]
  • CANTEST lab report 90206003.pdf [particle size analyses for Klutan Glacier pedons Y07-06 & Y07-07; also Tuya pedons BC07-03 & BC07-04 &]
Klutlan Glacier soils
2023.2.2.13 · Subsérie · 2007-2010
Parte de Dr. Paul Sanborn fonds

With the assistance of the Yukon Geological Survey, Dr. Paul Sanborn was able to visit the terminus of the Klutlan Glacier, a major outlet glacier which originates in the Alaska portion of the St. Elias Mountains. The stagnant terminus has a thick cover of debris, including a large component of White River tephra, providing enough soil material to support a boreal forest. Field work occurred on July 8, 2007, and results were published as:

Sanborn, P. 2010. Soil formation on supraglacial tephra deposits, Klutlan Glacier, Yukon Territory. Canadian Journal of Soil Science 90: 611-618. https://doi.org/10.4141/cjss10042