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1
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- Soil Analysis Lab Procedures
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2
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- 1. Visual Examination – Macroscopic
- Texture: Use the flow chart in the sample field guide to make a visual
and manual determination of whether the sediment is silt, sand, clay,
loam, or a mixture.
- This will help you describe the type of sediment and the environment in
which it was deposited.
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3
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- 1. Visual Examination – Macroscopic
- Density: Use the Fractionation Testing Method for sorting the sediment
in a column of water and describe its various component levels.
- This involves placing a fixed amount of sediment (the same for each
sample you analyze) into a graduated cylinder filled with water, shake
it up, watch it settle, and record the approximate percentage of each
group of particle sizes separated by the water.
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4
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- 1. Visual Examination – Macroscopic
- Permeability: Use a filter paper to measure the rate at which water
seeps through the sediment sample, which is the permeability of the
sample. This is useful in characterizing the sediments ability to absorb
water (for farming)
- Place the filter paper over a beaker, include a fixed amount of sediment
(same amount for each sample), pour a fixed amount of water through the
paper and sediment, and record how long it takes for the water to seep
through the sediment.
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5
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- 2. Visual Examination – Microscopic
- Examine your sample under the microscope, draw and describe your
observations, especially focusing on the types of inclusions (such as
quartz, caliche) and the evidence of biotics (such as seeds, plant
materials, and insects). If you can’t identify anything, just draw what
you see.
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6
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- 3. Color Examination
- Use the sample field guide to describe the color of the sample. The
specific determination of color is used to compare sediments across
strata and from different places. The field guide helps avoid variations
in color description from person to person.
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7
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- 4. Chemical Essay
- Carbonate Testing: Add drops of hydrochloric acid (HCl) to your sample.
If you detect bubbles, that indicates carbonates. Carbonates form from
the decomposition of shellfish, and suggest the sediment was from a
water environment (lakes, oceans, rivers).
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8
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- 4. Chemical Essay
- Sulfide Testing: At the same time as you test the samples for carbonates
(above), smell the sample (carefully!!!). If you detect a “rotten egg”
smell, this indicates the presence of sulfides. Sulfides are the result
of recent organic decomposition, meaning dead animal flesh in the
sediment.
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9
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- 4. Chemical Essay
- pH Testing: Make sure your sediment sample is wet with purified water.
Put a strip of pH paper in the water and watch for a color change, then
compare it to the guide to tell the pH of the water. The pH describes
acidity or alkalinity, and is used to determine the usefulness of the
sediment for agriculture.
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10
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- 4. Chemical Essay
- Organic Reduction: [I’ll do this test, just record the results I get]
Using the triple balance, measure the weight (mass) of a sample of
sediment, then apply heat to the sample, “cooking it,” and measure the
sample again, noting the difference in weight before and after. This
difference is due to the oxidation of organics, which will cook at low
heats. This is called organic mass fractionization
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11
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- Texture: Sample 1 - sand Sample 2 – clay
- Density: Sample 1 - Sample 2 –
- 10% heavy 20% heavy
- 60% medium 30% medium
- 30% light 50% light
- Permeability: Sample 1 - Sample 2 –
- 60 sec 100 sec
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12
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- Microscopic Exam:
- Illustrations
- Sample 1 – Sample 2 –
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13
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- Color:
- Sample 1 - Light Brown Sample 2 - Dark Yellow
- Carbonate Testing:
- Sample 1 - negative Sample 2 – positive
- Sulfide Testing:
- Sample 1 - negative Sample 2 – negative
- Ph Testing:
- Sample 1 – 6 Sample 2 – 7
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14
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- Organic Reduction:
- Sample 1 - Sample 2 –
- start weight = 199.90 g start weight = 175.50 g
- ending weight = 170.75 g ending weight = 170.00 g
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15
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- Summary: In our experiment and analysis of the three soil samples,
several differences were noted. These include:
- yada, yada, yada….
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