LAB 4. SPECTROPHOTOMETRIC
ANALYSIS OF PHOSPHORUS
Introduction
Soil is a
complex and variable mixture of rock fragments, organic matter, moisture,
gases, and living organisms that provides mechanical support for growing
plants. Soil also stores supplies of water and other critical nutrients for
growing plants and as a result the productivity of the site is directly related
to the productivity of the soil. The elements nitrogen, phosphorus, potassium
and calcium are all essential to the growth and the development of both plants
and animals.
Soil test
phosphorus (STP) is not an indication of total P in the soil but how much is
available for plant use. If STP numbers are to be compared, the laboratory test
method for extracting P and how the number is reported (parts per million or
pounds per acre) must be known. Different testing labs use different methods
for extracting P, producing different test results that are difficult to
compare even for the same sample.
Soil testing facilities
may report results in pounds per acre of elemental P. Other soil testing labs
may report their results in parts per million (ppm) without making the
conversion to pounds per acre (lbs/A). This conversion from ppm to lbs/A
involves assuming that a 6-inch deep layer of soil (furrow slice) covering one
acre weighs 2,000,000 pounds. To convert soil test results from ppm to lbs/A, you’ll
need to multiply the value in ppm by 2. For example, a soil test P value of 150
ppm is correlated to 300 lbs/A. In addition Kg P/ha = ppm X 10
About 99% of the total phosphorus in soils is
tied up in compounds that are not readily available to plants. Approximately
two-thirds of this total is inorganic-P. The remaining portion is organic-P.
Phosphorus can be released into plant available forms from either of these
sources. Inorganic-P often reacts with soluble aluminum, iron, or calcium in
the soil solution to form relatively insoluble compounds. These reactions
depend on soil pH. Inorganic-P can be relatively unavailable at either a very
low or very high soil pH. Organic-P compounds are continually being immobilized
and released by soil microorganisms and growing plants.
Of the three primary nutrients, phosphorus is
the least mobile in the soil, so leaching of P into groundwater is not often a
concern. This does not mean that phosphorus will not move off-site, however.
Phosphorus, both inorganic and organic, can readily be transported to surface
water along with eroding soil particles. Phosphorus can also be lost while
dissolved in water.
Purpose
To introduce the
student to spectrophotometric analysis of soil phosphorus through the
preparation of standards and the determination of a calibration curve using a
Bauch and Lomb spectrophotometer.
Prepared Reagents:
1. 1000
ml of Stock Phosphate solution (25 mg/l)
2. Ammonium
Molybdate Reagent
3. Dilute
Stannous Chloride Solution (Prepared daily)
Apparatus:
1. 1-
digital pipette
2. 1-25ml
volumetric flasks
3. 1-4ml
volumetric pipette
4. 1-25ml
burette
5. 1-
test tube stand
6. 11-test
tubes
7. 6-
50ml beakers
8. 1-
spectrophotometer cuvet
9. parafilm
10. labels
Procedure:
1. Determine
the amount of Stock Phosphate Solution required to prepare 5 – 25ml standards
of 1, 5, 10, 15, 20 mg/l using the following dilution formula:
C1V1
= C2V2
Where C1 =
concentration of stock phosphate solution (ie. 25 mg/l)
V1
= volume of stock solution required to make a given standard
C2
= concentration of standard to be prepared
V2
= volume of standard to be prepared (ie 25 ml)
Table
1: Amount of
stock phosphate solution (25 mg/L) required to prepare standards of varying
concentration.
STANDARD (mg/l) |
AMOUNT STOCK SOLUTION REQUIRED (ml) |
0 |
|
1 |
|
5 |
|
10 |
|
15 |
|
20 |
|
2. Preparation of Standards:
Prepare standards by starting with the
lowest concentration first (1 mg/l); using a
25 ml burette, transfer the required
amount of stock solution to a 25 ml volumetric flask
and dilute with distilled water to the 25 ml mark. Pour into an appropriately labelled clean beaker.
3. Set up 11 test tubes
in a test tube rack.
Using a 4-ml volumetric
pipette, transfer:
·
4 ml of each of the
standards (from Step #2) to a separate test tube and label each test tube (eg. 1,
5, 10, 15, 20 mg/l)
·
4 ml of the known sample
(prepared samples) to a separate test tube. Repeat. Label each test tube (eg.
Known trial #1, Known trial #2)
·
4 ml of the unknown
sample (prepared samples) to a separate test tube. Repeat twice. Label each
test tube (eg. Unknown trial #1, Unknown trial #2, Unknown trial #3)
·
4 ml of distilled water to a
separate test tube and label as “Blank”
4. Colour Complexing of
the Standards, Samples and Blank
For all
5 standards, the one known (2 trials) and the one unknown (3 trials) and the
blank (1) proceed with the
following procedure:
·
Using a digital pipette, add 1
ml of the molybdate reagent
·
Using a digital pipette, add 1
ml of the dilute stannous chloride solution
Wrap the top of each test tube with
parafilm and invert several times to mix.
A blue colour should be present. Allow
samples to stand for 10 minutes in a test tube
rack and measure transmittance at 680 mm (red filter)
5. Transfer
the “Blank” to a cuvette and calibrate the meter to 100% (transmittance).
Pour your blank
back into the test tube in case you need to calibrate the meter again.
6. Starting with the lowest concentration,
transfer the solution to the same cuvet, wipe
the outside of the cuvette, place in the spectrophotometer and analyze. Record Absorbance. Use this same cuvette for all readings for the
remaining 5 standards and record.
7. Use the same cuvette as in #6 and the
same methodology to analyze the known concentration
(2 trials) to validate the calibration curve, record
8. Use the same cuvette as in #6 and the
same methodology to analyze the unknown
concentration (3 trials), record
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