hydrometer lab

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 Particle-size analysis (hydrometer method) The purpose of this lab is to determine the percentage of sand, silt, and clay in soil samples using a hydrometer that measures the density of a solution. The hydrometer method is based on Stokes’ a!. Stokes’ a! states denser particles (usually larger) sink faster than less dense particles (smaller) !hen suspended in li"uid (of a gi#en temperature). There are t!o crit ical assumptions regarding t his$ %) the  particles all ha#e the same density--thus larger ones !ill settle first, and &) the parti cles are spherical. 'ctually , neither of these can be perfectly satisfied. The hydrometer thus measures t he density of the soil !ater miture. The more particles that are in suspension, the more dense the soil!at er miture !ill be. The more dense the miture, the better it !i ll support an ob*ect pl aced in the miture. That is, the more dense the miture, the higher the hydrometer !ill float in the soil !ater miture. 's larger  particles fall from suspension, the density of the soi l!ater miture decreases. 's the density decreases, the hydrometer si nks farther into the m iture. The stem of the hydrometer is marked in grams of sediment remaining in suspension. +o u !ill be analyzing t!o soils. --------------------------------------------------------------------------------------------------------- Procedure$ %) Ta ke about half of a mortar full of soil and lightly grind to break up the soil clumps. 'fter!ards take this sample and pass through the &mm sie#e to remo#e any gra#el. +o u ultimately !ant g of dri ed, crushed soil. epeat for other sample. &) /e igh the grams of air-dry soil (i.e., minus the gra#els) from each sample and place in &ml bottles (!ith a caps) and add %ml of sodium heametaphosphate to each. Shake for at least a half-hour. 0) 'fter shaking, transfer the mitures to %ml glass cylinders using a s"ueeze bottle to get all of the soil out of the bottles. 1) 2ill the cylinders !ith !ater to %ml. ) +ou !ill notice a %ml cylinder marked 3standard.’ This contains !ater and %ml of the sodium heametaphosphate solution. + ou !ill need to take a hydrometer reading of this and record it . ead the hydrometer at the point !here the !ater surface and s tem of hydrometer meet. 4) Stir the soil!ater mitures

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Soils lab: Particle-size analysis

Particle-size analysis (hydrometer method)

The purpose of this lab is to determine the percentage of sand, silt, and clay in soil samples using a hydrometer that measures the density of a solution.The hydrometer method is based on Stokes Law. Stokes Law states denser particles (usually larger) sink faster than less dense particles (smaller) when suspended in liquid (of a given temperature). There are two critical assumptions regarding this: 1) the particles all have the same density--thus larger ones will settle first, and 2) the particles are spherical. Actually, neither of these can be perfectly satisfied.

The hydrometer thus measures the density of the soil/water mixture. The more particles that are in suspension, the more dense the soil/water mixture will be. The more dense the mixture, the better it will support an object placed in the mixture. That is, the more dense the mixture, the higher the hydrometer will float in the soil/water mixture. As larger particles fall from suspension, the density of the soil/water mixture decreases. As the density decreases, the hydrometer sinks farther into the mixture. The stem of the hydrometer is marked in grams of sediment remaining in suspension.You will be analyzing two soils.

---------------------------------------------------------------------------------------------------------Procedure:

1) Take about half of a mortar full of soil and lightly grind to break up the soil clumps. Afterwards take this sample and pass through the 2mm sieve to remove any gravel. You ultimately want 50g of dried, crushed soil. Repeat for other sample. 2) Weigh the 50 grams of air-dry soil (i.e., minus the gravels) from each sample and place in 250ml bottles (with a caps) and add 100ml of sodium hexametaphosphate to each. Shake for at least a half-hour. 3) After shaking, transfer the mixtures to 1000ml glass cylinders using a squeeze bottle to get all of the soil out of the bottles.

4) Fill the cylinders with water to 1000ml.

5) You will notice a 1000ml cylinder marked standard. This contains water and 100ml of the sodium hexametaphosphate solution. You will need to take a hydrometer reading of this and record it. Read the hydrometer at the point where the water surface and stem of hydrometer meet.

6) Stir the soil/water mixtures

7) When you finish mixing, you will need to begin timing, because you take hydrometer readings according to the schedule below. The readings you take will give the density in g/L. We will assume a constant temperature--it remains about 20o C in the lab. Remember do not stir, bump, or alter the solution once you finish stirring it and begin taking readings.Readings:

A) at 40 seconds ____________

B) at 4 minutes _____________

C) at 37 minutes _____________

D) at 2 hours ________________

Calculation: [be sure to subtract the reading of the standard from each of these. Example: If the standard reading was 2 and reading A was 20, the calculation would be (50 18) x 2Total sand = (50 A) x 2

1) Sand

_____%Coarse silt = (A B) x 2

Coarse Silt

_____%Medium silt = (B C) x 2

Medium Silt

_____% 2) Total Silt ___%Fine silt = (C D) x 2

Fine Silt

_____%Clay = D x 2

3) Clay

_____%8) Plot these percentages (1, 2, 3) on your textural triangle. What textural class is each of these soils?9) What horizons did each of these soils originate from? 10) What are some possible error sources in determining texture in these analyses?