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Soils - Field Characterization, Collection, and Laboratory Analysis Readings – Principles of Terrestrial Ecosystem Ecology, by Chapin (Ch. 3) Understanding.

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Presentation on theme: "Soils - Field Characterization, Collection, and Laboratory Analysis Readings – Principles of Terrestrial Ecosystem Ecology, by Chapin (Ch. 3) Understanding."— Presentation transcript:

1 Soils - Field Characterization, Collection, and Laboratory Analysis Readings – Principles of Terrestrial Ecosystem Ecology, by Chapin (Ch. 3) Understanding Earth, by Grotzinger and Jordan (Ch. 16) Abir Biswas The Evergreen State College

2 Context of this introductory lab Students had background in mineral and rock ID (physical geology) In class, topics that we had/were discussing included –Physical and chemical weathering processes (Grotzinger) –Development of soil profiles (Chapin) –Soil horizons and soil classification (Chapin) –Soil properties (Chapin)

3 Goals of this (2 day) Field & Lab activity Field-- coniferous and deciduous ecosystems Soil characterization (and observations of the surrounding ecosystems) Soil development in coniferous vs. deciduous ecosystems Lab– measuring soil moisture, organic C content, grain size distribution General laboratory procedures incl.: –investigating the homogeneity/heterogeneity of real field samples… and considering representative subsamples –using balances and ovens –using sieves (Some) Quantitative reasoning Quantifying moisture content, organic C content Grain size distribution (% coarse sand, % fine sand, % silt) Class data to see the value of replicates, get averages etc.

4 Considerations and potential pitfalls Time Our 3 coniferous and 3 deciduous were dug several years ago and were covered– in 30-60 mins students could walk to, find and clear sites (no re-digging) –Several students suggested digging pits could have been helpful –Maybe 3 replicates are not needed … but sites going down to ~1m seem ideal and it seems like the first time investment is worth the time Soil Horizon identification Students particularly struggled to distinguish soil horizons in the field-- especially between O and A horizons Chapin Figure 3.9. A generic soil profile showing the major horizons that are formed during soil development. Density of dots reflects the concentration of soil organic matter. (from Chapin Ch. 3.)

5 Customizing for your school and field site Different student backgrounds– with geology students could better consider composition of C horizon, with ecology students maybe better consider transformations of C through soils profiles and/or the broader ecosystem Contrasting sites– helps to highlight differences in soil formation processes, or perhaps an elevational transect? Other ideas…? THANKS!

6 Variation in veg/soils on Evergreen’s campus (http://academic.evergreen.edu/projects/eeon/maps/tesc_canopy.pdf)http://academic.evergreen.edu/projects/eeon/maps/tesc_canopy.pdf


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