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Soil Carbon under the Snowpack in a Continuous Coniferous Forest Daniel P. Bradley February 19 th , 2011 Winter Ecology Mountain Research Station, University of Colorado, Boulder EBIO 4100, Sec 570

Soil Carbon under the Snowpack in a Continuous Coniferous Forest

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Soil Carbon under the Snowpack in a Continuous Coniferous Forest. Daniel P. Bradley February 19 th , 2011 Winter Ecology. Mountain Research Station, University of Colorado, Boulder EBIO 4100, Sec 570. Life in the Winter Soils. - PowerPoint PPT Presentation

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Page 1: Soil Carbon under the Snowpack in a Continuous Coniferous Forest

Soil Carbon under the Snowpack in a Continuous Coniferous Forest

Daniel P. BradleyFebruary 19th, 2011

Winter Ecology

Mountain Research Station,University of Colorado, Boulder

EBIO 4100, Sec 570

Page 2: Soil Carbon under the Snowpack in a Continuous Coniferous Forest

Life in the Winter SoilsSoil microbes in snow covered soils are respiring every

minute, consuming available nutrients, and off-gassing them as CO2 (King 08).

Our class experiment: 18.536 g (0.653 oz) of carbon could be converted into CO2 in 186 days (Oct 25 – May 1), in ~100 cm2 (Winter Eco 11).

Winter soil: An ideal environment for microbial life.

Page 3: Soil Carbon under the Snowpack in a Continuous Coniferous Forest

Pro’s and Con’s of Winter Microbial LifePro’s Con’sHighly protected

Predatory, UVHighly stable

TemperatureWater supply

via the snowpack, varying (Brooks 96)

A specialized niche

Food SupplyHigh, but non-replenishing

TemperatureNot ideal for metabolic

processes

Page 4: Soil Carbon under the Snowpack in a Continuous Coniferous Forest

The Food SupplyThe food supply in a finite amountWe can assume that the amount of food is

equal throughout the forest.

Page 5: Soil Carbon under the Snowpack in a Continuous Coniferous Forest

QuestionIf food is limited by the cover of the snowpack, does the

depth of the snowpack affect the amount of carbon (food) in the soil?

HA : There is a difference in soil carbon between sites of varying snowpack.

HO : There is not a difference in soil carbon

Page 6: Soil Carbon under the Snowpack in a Continuous Coniferous Forest

MethodsA deep and shallow site were found on Feb 5th Five samples for each site were taken, with 2 sub sites for

each site, from the top 5cm of the soil. The soils were refrigerated maintain metabolic processesThe soils were then sieved, weighed into 5 gram samplesThe samples were dried, combusted and weighed.Percent differences and averages were derived.

Page 7: Soil Carbon under the Snowpack in a Continuous Coniferous Forest

The Sites

CU Mountain Research Station - Google Earth

Page 8: Soil Carbon under the Snowpack in a Continuous Coniferous Forest

ResultsThe data show that there was a significant difference (p-

value ≤ 0.05) in soil carbon between the sites

Page 9: Soil Carbon under the Snowpack in a Continuous Coniferous Forest

The Datap-value = 0.0165 (paired t-test)

Mean percent difference: deep=0.1057, shallow=0.3322

Page 10: Soil Carbon under the Snowpack in a Continuous Coniferous Forest

The Datap-value = 0.0113(paired t-test)

Mean difference, in grams: deep=0.0056, shallow=0.0182

Page 11: Soil Carbon under the Snowpack in a Continuous Coniferous Forest

DiscussionThe shallow snowpack had more carbon underneath it,

why? Carbon is limiting for microbes, lower carbon indicates

higher microbe populations/activity (Nemergut 11). Temperature swings.

What is affecting snowpack?Wind, Precipitation

What is affecting the amount of carbon (litter) under the snowpack?Beetle kill?

Page 12: Soil Carbon under the Snowpack in a Continuous Coniferous Forest

SummarySnowpack does have an affect on the microbial

population of the soil, via carbon.More snowpack, more respiration, more carbon

consumed.

Page 13: Soil Carbon under the Snowpack in a Continuous Coniferous Forest

Literature Cited Brooks, Paul D., Mark W. Williams, and Steven Schmidt. "Microbial

Activity under Alpine Snowpacks, Niwot Ridge, Colorado " Biogeochemistry 32.2 (1996). 93-113. Mark Williams. Web. 25 Jan. 2011.

King , A. J., A. F. Meyer, and S. K. Schmidt. "High Levels of Microbial Biomass and Activity in Unvegetated Tropical and Temperate Alpine Soils." Soil Biology and Biochemistry 40.10 (2008): 2605-610. ScienceDirect. Web. 25 Jan. 2011.

Nemergut, Diana, CU-Boulder, INSTAAR. Personal interview. 16 Feb. 2011.

Winter Ecology 2011, and T. Kittle. TS. CU-Boulder, Mountain Research Station.