silicate
(less than about
12 Acg-at Si/liter), the factor F („ c. )may be assumed to be equal to
0.1 xNote: The factor F is a function of the salinity of seawater samples. Between salinities 25 and 35%, the variation is less than 3% and may be neglected. The factor F, at a salinity S%0 is related to the factor, F, obtained as described above, by the approximate formula:
F ___ F x (1 4- 0.003 S) , 1.08
This correction should be used for the most precise work when the salinity varies by more than about 10%,, from a value of 28%,. The factor for pure water (zero salinity) is thus some 8%
less than the value obtained by the present method using synthetic sea water.
11.6. DETERMINATION OF REACTIVE NITRATE
INTRODUCTION
Since publication
of
the first editionof
this manual several new procedureshave
been proposedfor the
determinationof nitrate in
seawater. The
method basedon the
workof
Mullinand
Riley (Anal. Chim. Acta, 12: 464, 1955), previously describedin the
first edition has proven moderately satisfactorybut a
lengthy re-duction periodand
sensitivity tomotion are
serious disadvantages.The latter
we now bclieve is caused bythe
presenceof air
abovethe solution
during reductionand
can be minimized by carryingout the
reductionin a
small closed bottleof
some 60-ml capacity rather thanin the
recommended 125-ml Erlenmeyer flasks.The
methodof
Chowand Johnson
(Anal. Chim. Acta, 27: 441, 1962) basedon a zinc
dust reduction, hasthe
disadvantage that it involvesa
magnetically stirredsolution in an ice-bath
followed byfiltration. This
is neither cheap nor convenient when handling many samples atsea. The
rapidand
elegant procedure described byArmstrong
(Anal. Chem., 35: 1292, 1963) lacks sensitivity, can be troublesomein waters of
high "humicacid" content and
involves unpleasantconcentrations of
sulphuricacid. This
method, however, is idealfor
determinationson culture solutions
containing highconcentrations of nitrate,
especially when only smallvolumes of solution are
available.The
following procedure is basedon a
method byMorris and
Riley (Anal.Chim. Acta, 29: 272, 1963) with some modifications.
At
thesuggestion of
Grasshoff (Kiel. Meeresforsch., 20: 5, 1964) weuse ammonium
chloride.A
cadmium-mercury column has been replaced bya
cadmium-copper column basedon
the,workof Wood, Armstrong and Richards
(J. Marine biol. Assoc. U.K., 47: 25, 1967), although wehave
hadtrouble
withthe use of
EDTA suggested by these workersand have
reverted toammonium
chlorideas an
activator. Reductionof nitrate
tonitrite
is nearly completeand the
method described below is probablyas sensitive as
is practicable bya routine
spectrophotometric procedure.METHOD
A.
CAPABILITIESRange: 0.05-45 pg-at/liter 1. PRECISION
AT THE
20 pG-AT/LITER LEVELThe correct value lies in the range:
Mean
of
n determinations -±0.50/n1 14-at/1iter (using 1-cm cells).2. PRECISION
AT THE
1 ittG-AT/LITER LEVELThe correct value lies in the range:
Mean
of
n determinations -±-0.05/re itg-at/liter (using 10-cm cells) . 3. LIMITOF
DETECTIONThe
smallest amountof nitrate
nitrogen that can be detected with certainty isabout
0.05 ,ag-at/liter using 10-cm cells.71
72 A PRACTICAL HANDBOOK OF SEAWATER ANALYSIS B. OUTLINE OF METHOD
The nitrate in sea water is reduced almost quantitatively to nitrite when a sample is run through a column containing cadmium filings loosely coated with metallic copper. The nitrite thus produced is determined by diazotizing with sulphanilamide and coupling with N-(1-napthyl)-ethylenediamine to form a highly coloured azo dye the extinction of which is measured. A correction may be made for any nitrite initially present in the sample.
C. SPECIAL APPARATUS AND EQUIPMENT
The reduction columns may be conveniently prepared by joining end-to-end three pieces of glass tubing, viz: 10 cm of 5-cm internal diameter tube on to 30 cm of tubing 10 mm in internal diameter (which is to contain the metal filings, see Sect. E below) which in turn is joined to 35 cm of a tube 2 mm in diameter. The last tube is bent just below this join into a U so that it runs up parallel to the 10-mm diam tube and then its end is bent over to form an inverted U syphon. This last bend should be just level with the top of the 10-mm diam tube when the assembly is held upright to form a column. With this arrangement, liquid placed in the top reservoir tube should flow out of the system and stop when the level of liquid is such that it just covers the metal filings (see below). Place the reduction columns inside large glass or plastic cylinders (for protection) and fix to the outside of these a small cylinder of glass, drawn to a tube at one end and closed by a rubber tube and pinchclip. This cylinder should hold about 75 ml and be arranged under the exits of the reduction columns to collect effiuents. Mark the cylinder at 40 and at 50 ml.
50-ml graduated cylinders.
125-ml Erlenmeyer flasks. These should be kept grease-free so that the minimum amount of liquid is retained when the flasks are drained dry.
D. SAMPLING PROCEDURE AND SAMPLE STORAGE
Sample (100-!-2 ml) should be measured from sea-sampling bottles by a 100-ml measuring cylinder and placed in a 125-ml Erlenmeyer flask. Samples are stable for several hours cold and in the dark but the analysis should not be delayed for more than about 12 hr. If greater delays are unavoidable the samples should be frozen to -20 C in a deep-freezer where no detectable changes should occur for many weeks. Unless the number of samples is large it may be desirable to store samples at sea in this fashion and return them to a shore-base laboratory for analysis.
E. SPECIAL REAGENTS
1. CONCENTRATED AMMONIUM CHLORIDE SOLUTION
Dissolve 125 g of analytical reagent quality ammonium chloride in 500 ml of distilled water and store in a glass or plastic bottle.
2. DILUTE AMMONIUM CHLORIDE SOLUTION
Dilute 50 ml of concentrated ammonium chloride solution to 2000 ml with distilled water. Store the solution in a glass or plastic bottle.
II.6. REACTIVE NITRATE 73