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Minnesota Crop News > 2001-2008 Archives
October
31, 2002
Soil
Nitrate: Fall 2002
George Rehm, Nutrient Management Specialist
Collection of soil samples from depths below
6 inches has been a suggested management practice in southwestern,
western, and northwestern Minnesota for more than twenty years.
Analysis of these samples for nitrate-nitrogen (NO3-N)
has allowed for the fine tuning of current nitrogen recommendations.
Nearly everyone who works with nitrogen and nitrogen fertilizer
recommendations realizes that measurement of NO3-N
in soils is not absolutely perfect. Yet, use of this test where
appropriate, can have a substantial effect on nitrogen fertilizer
recommendations.
For many years, monitoring of NO3-N in soybean
fields that precede an intended corn crop led to the conclusion
that soil NO3-N has been relatively constant at
30 to 40 lb. N per acre for these production situations. However,
nitrogen is very transient in soils and quantities measured
are highly affected by environmental conditions. So, there
should be no expectations that measured NO3-N following
soybeans will remain constant over time. Some information collected
in the fall of 2002 is ample evidence for the variability of
NO3-N in soils.
Some of the information summarized by Agvise Laboratories
is provided in the following table.
General
Area |
Number
Of
Samples |
% of Testing in Each Category
lb./acre NO3-N to 24 in. |
0 to 20 |
21 to 40 |
41 to 60 |
61 to 80 |
81-100 |
100+ |
Northern
MN |
1367 |
6 |
35 |
32 |
16 |
6 |
5 |
| Northwest MN |
2289 |
2 |
20 |
33 |
23 |
12 |
10 |
| South Central ND |
1758 |
1 |
11 |
21 |
24 |
18 |
25 |
In all cases, wheat was the previous crop. In general, the
percentage of samples in each category appears to be related
to the weather for the past spring and summer. The growing
season in south central ND could be characterized as dry whereas
there was ample, and in many cases, above normal moisture in
northern and northwestern Minnesota.
Past experience has shown that soil nitrates increase where
there is a drought that severely restricts crop growth. Even
though there was ample moisture in northwest and northern Minnesota,
a substantial number of samples had levels of NO3-N
in excess of 40 lb. per acre. The results of this summary indicate
that substantial amounts of nitrate-nitrogen were produced
as a result of mineralization of soil organic matter.
Another summary of the analysis of soil samples for nitrate-nitrogen
is provided by Centrol of Cottonwood, Minnesota. Samples to
24 inches were taken from fields where corn would follow soybeans
as well as fields where the sugarbeet crop would follow corn.
That summary is provided in the tables that follow.
Soybeans to Corn Cropping System
|
Area |
| Measured NO3-N |
#1
|
#2
|
#3
|
| lb/acre to 42 in |
#samples |
% of total |
# samples |
% of total |
# samples |
% of total |
| 100+ |
3 |
7 |
1 |
2 |
0 |
0 |
| 80 to 99 |
3 |
7 |
1 |
2 |
1 |
2 |
| 60 to 79 |
5 |
12 |
5 |
10 |
8 |
13 |
| 50 to 59 |
8 |
20 |
8 |
16 |
3 |
5 |
| 40 to 49 |
8 |
20 |
11 |
22 |
10 |
17 |
| 30 to 39 |
1 |
2 |
12 |
24 |
18 |
30 |
| 20 to 29 |
10 |
24 |
6 |
12 |
13 |
22 |
| Less than 20 |
3 |
7 |
6 |
12 |
7 |
12 |
Corn to Sugarbeets Cropping System
|
Area |
| Measured
NO3-N |
#1
|
#2
|
#3
|
| Lb/acre to 24 in |
#samples |
% of total |
# samples |
% of total |
# samples |
% of total |
| 200+ |
1 |
3 |
1 |
4 |
10 |
21 |
| 150-199 |
2 |
6 |
1 |
4 |
6 |
13 |
| 120-149 |
5 |
15 |
3 |
11 |
10 |
21 |
| 100-119 |
11 |
33 |
2 |
7 |
8 |
17 |
| 80-99 |
4 |
12 |
4 |
15 |
5 |
10 |
| 60-79 |
4 |
12 |
5 |
19 |
7 |
15 |
| 40-59 |
3 |
9 |
3 |
11 |
2 |
4 |
| Less than 40 |
3 |
9 |
8 |
30 |
0 |
0 |
For the planting system where corn will follow soybeans, 50%
of the samples showed amounts of NO3-N in excess
of 40 lb. per acre. This is not consistent with what we would
expect.
Substantial amounts of NO3-N were found where corn
is to follow the sugarbeet crop. Recognize that the sampling
depth was 42 inches rather than 24 inches. Nevertheless, several
samples showed substantial amount of NO3-N.
High rates of fertilizer N are not usually applied to the
sugarbeet crop and no nitrogen fertilizer is applied to soybeans.
The source of the NO3-N can be questioned. The only
logical explanation is the mineralization of soil organic matter.
Most crop producers are reporting excellent yields for the
2002 growing season. Thinking back to past years, measurements
of NO3-N have shown relatively high levels of NO3-N
following a good crop. This was true even though the high-yielding
crop would have removed substantial amounts of N from the soil
system. These observations over the years lead to the conclusion
that environmental conditions, which produce good yields, are
also favorable for above average rates of mineralization of
soil organic matter. Thus, the higher than expected amounts
of residual NO3-N.
With two summaries available at this time and shown in previous
tables, this would appear to be a good fall to collect soil
samples for measurement of residual or carryover NO3-N
in southwestern, western and northwestern Minnesota. For intended
crops other than sugarbeets, guidelines recommend collection
of soil from 0 to 6 and 6 to 24 inches. If the sugarbeet crop
is planned, guidelines call for collection of soil from depths
of 0 to 6, 6 to 24 and 24 to 48 inches. For this crop the calculation
of residual NO3-N is based on analysis of soil from
each depth.
Considering the information available at this point in the
fall season, it would be a good practice to get a measure of
NO3-N. If values are higher than expected, rates
of nitrogen fertilizer can be reduced thereby lowering costs
without reducing yield.
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