Fate
of Manure Nitrogen Applied for Grass Silage Production
Final Report submitted by Washington State University
Livestock Nutrient Management Program
July 2009
Purpose:
Characterize the
effect of management factors such as re-seeding of cropland as well as timing
and amount of manure and irrigation water
application on crop uptake of nitrogen, soil nitrate-N concentration,
nitrate+nitrite-N concentration in shallow ground water underlying the field,
and the relationships between these matrices.
In 2004, there was an
interest by the Whatcom Conservation District and the Department of
Ecology’s Bellingham Field Office to do a study that quantitatively measured
management practices on a grass field where dairy manure was applied annually
and relate these practices to shallow groundwater nitrate+nitrite-nitrogen (N)
concentrations. The location of the field was in an area where the depth to
groundwater was relatively shallow (ranged from 0.5 to 11 feet depending on
seasonal variation), and the soil type was known to be one where
nitrate-nitrogen would leach (poorly graded sand with silt and loam).
A contractor for the Department of Ecology’s
(Ecology) Environmental Assessment Program (EAP) installed 6 shallow
groundwater wells (13 feet deep) and 1 deep groundwater well (38 feet
deep). The EAP sampled these wells
every 4 to 6 weeks from 2004 to 2008. The Washington State University (WSU)
Livestock Nutrient Management Program collected grass, manure, soil, and
irrigation water samples throughout the 4-year period. Weather data was also
collected during this time frame.
The
intent of the study was to measure surface activity and monitor groundwater
parameters to assess the effectiveness of recently adopted Dairy Nutrient
Management Plans in protecting the quality of the Sumas-Blaine Aquifer at a
typical dairy. Therefore, there was relatively little instruction by WSU or
Ecology on what management practices to adopt or use throughout the study. The
only area of management that was modified due to the data that was collected
from the study was the irrigation schedule. It appeared in 2005 (the first full
year of the study) that the grass field went dormant in the summer months. Soil
moisture and nitrate-N concentrations were low, and grass growth slowed. After
the first year, at our suggestion, the dairy farmer intentionally tried to
apply more irrigation water earlier in the growing season to prevent grass dormancy.
Management
Practices
Each
year the management practices on the field were different. Prior to the start
of the study in 2004, the field was re-seeded from grass back into grass in the
spring using conventional tilling practices (subsoiling, rotatilling, plowing,
disking, seedbed preparation, cultimulching, and planting).
Data
collection started in the fall of 2004.
Grass was harvested 4 times and manure was applied 3 times (Tables 1 and
2). In 2005, grass was harvested 4 times
(Table 1). The intent was to harvest a 5th cutting in the fall,
however the weather did not permit.
There was approximately 1.5 tons/acre of grass (on dry matter basis;
estimate made in December 2005) remaining in the field through the winter
months. Manure was applied 5 times in
2005 (Table 2). Irrigation water was applied 2 times from the beginning of
August through the middle of September (Table 3).
In
2006, grass was harvested 5 times and manure was applied 3 times (Tables 1 and
2). No manure was put on the field in early spring (March) because of the large
amount of grass remaining in the field through the winter. Commercial
fertilizer was applied on 5/25/06 because no manure was available (Table 4).
Irrigation water was applied 2 times in 2006 (Table 3).
In 2007, grass was harvested 5 times and
manure was applied 4 times (Tables 1 and 2). Commercial fertilizer was applied
on 6/26/07 because no manure was available (Table 4). Irrigation water was applied 3 times (Table
3).
In
2008, grass was harvested 5 times and manure was applied 5 times (Tables 1 and
2). Irrigation water was applied 2 times (Table 3).
Table
1. Grass harvest
dates from 2004 through 2008.
|
Year |
Grass Harvest Dates |
||||
|
2004 |
4/28/04 |
7/19/04 |
8/16/04 |
10/7/04 |
|
|
2005 |
4/28/05 |
6/12/05 |
7/17/05 |
8/25/05 |
|
|
2006 |
4/21/06 |
5/25/06 |
7/5/06 |
8/15/06 |
9/27/06 |
|
2007 |
5/6/07 |
6/14/07 |
7/30/07 |
8/28/07 |
10/10/07 |
|
2008 |
5/9/08 |
6/16/08 |
7/21/08 |
9/2/08 |
10/21/08 |
Table
2. Manure application
dates from 2004 through 2008.
|
Year |
Manure Application Dates |
||||
|
2004 |
3/18/04 |
4/30/04 |
7/14/04 |
|
|
|
2005 |
2/18/05 |
5/13/05 |
6/27/05 |
8/9/05 |
8/31/05 |
|
2006 |
None |
4/27/06 |
7/11/06 |
10/7/06 |
|
|
2007 |
3/14/07 |
5/18/07 |
8/6/07 |
9/7/07 |
|
|
2008 |
3/10/08 |
5/20/08 |
6/23/08 |
7/31/08 |
9/13/08 |
Table
3. Irrigation
water sampling dates from 2005 through 2008.
|
Year |
Irrigation Water Sample Dates |
||
|
2005 |
8/17/05 |
9/7/05 |
|
|
2006 |
7/22/06 |
8/22/06 |
|
|
2007 |
7/17/07 |
8/23/07 |
9/12/07 |
|
2008 |
7/8/08 |
8/16/08 |
|
Table
4. Commercial
fertilizer
dates
from 2006 and 2007.
|
Year |
Commercial
Fertilizer Dates |
|
2006 |
5/25/06 |
|
2007 |
6/26/07 |
Manure
was primarily applied using an aerator (also referred to as subsurface
deposition or
The
following questions were forwarded to the WSU Nutrient Management Program from
Nora Mena at the Washington State Department of Agriculture in February of
2009. Data from the study was used to
answer the questions. In some cases there was no information available.
What level of irrigation/rain
water will affect nitrate movement through the root zone- first foot, second,
etc.?
The soil samples that were collected for this grant were
taken only at the 1-foot level. There
was no measurement of root zone or second foot soil nitrate-N concentrations.
One-foot soil samples were taken weekly throughout the fall (August through
November), and analyzed for moisture level and nitrate-N concentration. Precipitation was recorded daily. There were times in the fall when the amount
of precipitation was high over a relatively short period of time (1 to 2 weeks). A fairly rapid decrease in 1-foot soil
nitrate-N concentrations occurred at the time of high precipitation. This was followed by elevated groundwater
nitrate+nitrite-N concentrations in the following winter months in 2006 and
2008. Below are some graphs highlighting
this information:

In 2005, soil nitrate-N concentrations went from 22 ppm
(10/25/05) to 12 ppm (11/1/05) to 6 ppm (11/10/05) over the 2-week period
(figure 1). Soil moisture went from 36
to 43 to 46% over the same time period (increased 10 percentage units (figure
1). Between 10/25/05 and 11/1/05 there was 2.2 inches of precipitation, and
between 11/1/05 and 11/10/05 there was also 2.2 inches of precipitation (total
= 4.4 inches of rain over 2 week period).
Mean groundwater nitrate+nitrite-N concentrations continued to decrease
through the fall and winter despite relatively high rainfall over a 2-week
period (September = 20 mg/L and by March 2006 = 13 mg/L (figure 1).

In 2006, soil nitrate-N concentrations went from 31 ppm (11/1/06)
to 16 ppm (11/15/06) over a 2-week period (figure 2). Soil moisture went from 31 to 34% over the
same time period (increased 3 percentage units; figure 2) indicating movement
of nitrate below one foot. Between
11/1/06 and 11/15/06 there was 8 inches of precipitation. Mean groundwater nitrate+nitrite-N
concentrations increased from 9 mg/L in the fall to14 mg/L in the winter
(figure 2).

In 2007, soil nitrate-N concentrations went from 19 ppm
(10/16/07) to 12 ppm (10/30/07) over a 2-week period (figure 3). Soil moisture
went from 36 to 39% over the same time period (increased 3 percentage units;
figure 3). Between 10/16/07 and 10/30/07 there was 3 inches of precipitation.
Mean monthly groundwater nitrate+nitrite-N concentrations did not vary much
throughout the fall and winter (October – 8 mg/L through Feb – 9 mg/L).

In 2008, soil nitrate-N concentrations went from 30 ppm
(10/31/08) to 10 ppm (11/7/08) over a 1-week period (figure 4). Soil moisture went from 37 to 51% over the
same time period (figure 4). Between 10/31/08 and 11/7/08 there was 5 inches of
precipitation. The manure application
rate (715 lb/acre/year of total N; figure 5) was high compared to nitrogen
removal by the grass (393 lb/acre/year of nitrogen; figure 5). Fall soil nitrate-N concentrations (average
of September and October – 29 ppm) were higher than in previous years, and mean
monthly groundwater nitrate+nitrite-N concentrations increased from the fall
into the winter (October – 5 mg/L to March - 13 mg/L; figure 4).

The amount of grass nitrogen harvested was greatest in 2006
and 2007 (430 and 458 lbs of nitrogen/acre, respectively; figure 5). The
application of manure total N in 2006 and 2007 (363 and 386 lbs/acre,
respectively) was about half of that applied in 2005 and 2008 (642 and 715 lbs
of manure total N/acre; figure 5). In fact, the amount of grass nitrogen
harvested in 2006 and 2007 was greater than the amount of manure total N
applied (figure 5).
In general, during the fall, when there was a high amount of
precipitation over a relatively short period of time, soil moisture increased
and soil nitrate-N concentrations decreased. Decreasing depth to water
following fall precipitation events indicates movement of soil pore-water
through the unsaturated zone to the water table. As the water moved vertically
through the soil profile, nitrate-N appears to move from the 1-foot level with
the soil pore-water to the water table.
In 2008, the concentration of nitrate-N in the 1-foot soil
sample tended to be greater during the fall (ranged from 10 to 41 ppm; figure
4) than the soil nitrate-N concentrations in 2005 (ranged from 5.5 to 22 ppm;
figure 1); 2006 (ranged from 14 to 31 ppm; figure 2), and 2007 (ranged from 10
to 25 ppm; figure 3).
Mineralization activity after
application, how soon, how much, what conditions?
This information was not collected during this study. There
is a possibility that some of this information may become available in another
study that is being conducted by Dr. Joe Harrison and the Washington State
University Livestock Nutrient Management Program.
What information is important
for nutrient planners to consider when developing recommendations for whole
farm nutrient management?
Comparison
of NLOS model predictions and observed concentrations of nitrogen in soil. This was completed by conference call and ADOBE Connect in
April 2009.
What did we learn regarding good
manure management for grass fields that have been re-seeded?
Information about manure management practices that would be
ideal in a year when there was re-seeding of a grass field was not collected
during this study.
In 2008, the amount of manure total N applied (715 lbs total
N/acre) exceeded the amount of grass nitrogen harvested (393 lbs/acre) by
almost double (figure 5). Average fall soil nitrate-N concentrations (average
of September and October soil samples) in 2008 were higher (29 ppm) compared to
average fall soil nitrate-N concentrations in 2006 (21 ppm) and 2007 (16 ppm)
when manure total N applied was similar to grass total nitrogen harvested
(figure 21). These results suggest that, in grass fields that have received
manure for many years, the amount of manure total N applied to the field can be
similar to the total amount of grass N harvested that year without compromising
quantity or quality of the grass stand. In 2006 and 2007, when total manure N
applied was similar to grass N harvested, the quantity (grass yield; figures 6
through 9) and quality (measured as crude protein; data not shown) of the grass
harvested equaled or exceeded the quantity and quality of grass N harvested
when approximately double the amount of manure total N was applied than grass N
harvested (year 2008; figure 5).




Other factors besides the nitrogen supplied to the grass
crop effect grass yield. Moisture level in the soil as well as available heat
units appear to have affected grass yield at different times throughout the
study.
Grass yields (tons of dry matter/acre) were lower in 2008
(figure 9) than in 2006 and 2007 (figures 7 and 8) despite the fact that the
amount of manure total nitrogen applied was almost twice as much as grass
nitrogen harvested in 2008 (figure 5). The dairy farmer had also applied
irrigation water earlier in the growing season compared to previous years in an
attempt to keep soil moisture levels higher (soil moisture remained at 25% or
greater during the driest part of the growing season) and prevent grass from
slowing in growth due to lower soil moisture content during the summer months.
The grass stand in 2008 was 4 years old, and there was a high concentration of
clover in the stand. These factors may have contributed to the lower grass
yield in 2008. However, it
appears that the air temperature in 2008 was noticeably lower than in previous
years, and this would affect yield.
Growing degree units (GDU) are a measure of thermal time by
calculating the daily accumulation of heat. There are different equations
available for calculating GDU. Three methods were used in this study and will
be reported below.
The first method used to calculate GDU for corn crops is
written below.
GDU = (maximum temperature + minimum temperature)/2 – 50° F
Daily maximums greater than 86° F are set equal to 86.
Daily minimums less than 50° F are set equal to 50.
At 50° F it is
assumed that corn growth is 0. As temperature increases, the growth rate
increases.
The optimum temperature for crop growth is considered 86° F.
The cumulative grass yield (7.2 tons/acre) was highest in
2007 and lowest in 2008 (5.9 tons/acre; figures 8 and 9). The cumulative GDU
values through October were 2,344 and 1,648 in 2007 and 2008, respectively
(figure 10). This is a difference of 696 GDU (daily accumulation of heat units)
between the 2 years. The greater heat units in 2007 aided in greater grass
yields.
GDU =
(maximum temperature + minimum temperature/2 – 50º F

There was a 42% reduction in GDU through October in 2008
compared to 2007. Grass yield was reduced by 22% in 2008 compared to 2007.
The cumulative GDU through October was plotted against the
cumulative grass yield for the years 2005 through 2008 (figure 11). Cumulative
GDU through October explained ~79% of the variation in grass yield (figure 11).
![]()

In 2005, the weather conditions did not allow for the final
cutting of grass to be harvested. Therefore, in December 2005, measurements
were collected to determine the approximate quantity of grass remaining in the
field. Below is a graph including the remaining grass in the field for the
fall/winter 2005. Cumulative GDU through December explained ~64% of the
variation in grass growth (figure 12).
GDU =
(maximum temperature + minimum temperature/2 – 50º F

Grass growth starts prior to 50° F in the Pacific Northwest. The exact time at which grass
growth begins is not well documented. Therefore, 2 equations were used to
calculate GDU using a grass growth model.
1)
The second method for
calculating GDU is from a British Columbia Publication – Determining range
readiness and growing degree-days (GDDs) – Rangeland Health Brochure 11
(Fraser, 2006).
GDU's start to accumulate after pasture is snow free, and
cannot begin before March 1. There must be 5 consecutive days when the daily
average temp exceeds 32° F
before GDU's begin to accumulate (referred to as "start up")
GDU = (maximum temperature + minimum temperature)/2 – 32° F
If GDU is negative it is not included in the data set (no
growth occurred)

Figure 13 is a graph plotting cumulative GDU (°F) using the Fraser (2006) equation referred to above:
![]()
The cumulative GDU through October was plotted against
cumulative grass yield for the years 2005 through 2008 (figure 14). Cumulative
GDU through October explained ~66% of the variation in grass yield (figure 14).
![]()

The third method
for calculating GDU is from the publication titled ‘N rate and timing
relationships with tissue N concentration and seed yield in perennial ryegrass’
(Griffith and Thomson, 1996).
GDU's start to accumulate January 1. The base temperature
for temperate grass is 32° F.
GDU = (maximum temperature + minimum temperature)/2 – 32° F
If GDU is negative it is not included in the data set (no
growth occurred)
Figure 15 is a graph plotting cumulative GDU (°F) using the Griffith and Thomson (1996) equation referred
to above:
![]()

The cumulative GDU through October was plotted against
cumulative grass yield for the years 2005 through 2008 (figure 16). Cumulative
GDU through October explained ~66% of the variation in grass yield (figure 16).
![]()

Three methods were used to estimate growing degree units.
All of the methods had a fairly strong relationship (at least 64% of the
variation in yield was explained by thermal heat units) with grass yield. This
suggests that thermal heat units strongly influence grass growth. The more heat
units the higher the yield.
Soil Moisture has
also been shown to influence grass growth in this study
In 2005, there was 1.2 inches of precipitation between
6/29/05 and 7/17/05 (figure 17).
However, between 7/17/05 and 8/11/05 there was only about 0.2 inches of
precipitation (figure 17). During this
time period, soil moisture levels dipped below 20%, and were very low at the
7/28/05 (14%) and 8/5/05 (13%) soil sampling dates (figure 17). Soil nitrate-N
concentrations were also very low (5 to 6 ppm) during the 7/28/05 and 8/5/05
soil sampling dates (figure 17). The grass had slowed in growth and manure was
applied 3 weeks and 3 days after the July cutting. The addition of manure as
well as irrigation water during mid August increased both soil moisture and
nitrate-N concentrations (figure 17).


In later years of the study the dairy farmer applied
irrigation water earlier in the growing season (started in July instead of
August). In 2007, irrigation water was
applied around the week of 7/17/07 for the first time followed by 2 more
irrigation events during the remainder of the growing season. During July and August, soil moisture levels
remained at 20% or higher, and soil nitrate-N levels remained between 18 and 20
ppm, also (figure 18). The time between the July and August cutting was reduced
by 1 week and 4 days from 2005 to 2007, however grass yield (0.88 and 0.86
tons/acre) and nitrogen removal (61 and 62 lbs N/acre) were similar in 2005 and
2007, respectively.
These results suggest that applying irrigation water earlier
in the growing season (in this study it was July instead of August) can
increase soil moisture content which will reduce the likelihood of grass
becoming dormant during the driest part of the year. This can increase the
yield of grass harvested, and hence increase the amount of nitrogen removed
over a growing season.
Summary of nitrate+nitrite-N
concentrations in wells over 4 year period and relationship to surface activity
and conditions.
Conventional tilling (subsoiling, rotatilling, plowing,
seedbed preparation, cultimulching) of the soil and re-seeding back to grass
resulted in elevated soil nitrate-N and groundwater nitrate+nitrite-N
concentrations in the fall following re-seeding. This study also documented
elevated groundwater nitrate+nitrite-N concentrations in the 2nd
fall after conventional tilling (figures 19 and 20).


Results from this study coupled with the fact that the dairy
farmer planned to re-seed this test field in 2009 led to the opportunity to do
a study comparing the effects of re-seeding grass using conventional tilling
practices to minimum tilling practices on soil nitrate-N and groundwater
nitrate+nitrite-N concentrations. This study is in the initial phases and will
continue for the next 2 years.

In 2005, there didn’t appear to be movement of nitrate-N
into the groundwater related to times of heavy rainfall in the fall. Mean groundwater nitrate+nitrite-N
concentrations (average groundwater nitrate+nitrite-N concentrations in mg/L
were: Sept = 20, Oct = 19, Nov = 19, Dec = 17; figure 21) continued to decrease
during the winter despite relatively high manure total N application (642
lb/acre; figure 5). However, in 2008, following another year of high manure
total N application (715 lb/acre) and the highest average fall soil nitrate-N
value observed (29 ppm), mean groundwater nitrate+nitrite-N concentrations
increased from 6 to 11 mg/L from November to December (figure 21). Fall
groundwater nitrate+nitrite-N concentrations (mg/L) were greater in 2005 than
in 2006 through 2008 (figure 21). The elevated levels of nitrate+nitrite-N in
the groundwater in 2005 compared to following years may have been a residual
effect of the release of nitrate-N in the soil due to conventional tilling and
re-seeding in the spring of 2004.
In 2006, the amount of grass nitrogen harvested (430 lbs
N/acre) was actually greater than the amount of total manure N applied (363 lbs
N/acre) over the growing season (figure 5). However, approximately 90 lb of
manure total N/acre was applied on 10/7/06 after the final cutting (on
9/27/06). Soil nitrate-N from the final
manure application apparently leached into the groundwater during the following
winter. The mean groundwater nitrate+nitrite-N concentration increased from 7
mg/L in November 2006 to 15 mg/L in January 2007 (figure 21).
In 2007, soil nitrate-N concentrations were low compared to
the other years. The average soil nitrate-N concentration for September and
October was 16 ppm, whereas average soil nitrate-N concentrations for September
and October were 29, 20, 21, and 29 ppm for 2004, 2005, 2006, and 2008,
respectively (figure 21). Mean groundwater nitrate+nitrite-N concentrations
remained below the 10 mg/L drinking water standard from May 2007 through
November 2008. Some of the reasons for
the lower soil nitrate-N and groundwater nitrate+nitrite-N concentrations in
2007 may be:
It had been 3 years since re-seeding the grass field using
conventional tillage methods,
The amount of manure total N applied for the previous 2
growing seasons (2006 and 2007) was less than the amount of grass N harvested
and about half of that applied in 2005 and 2008,
No manure was applied after the final grass harvest on
10/10/07,
Denitrification due to low oxygen in some of the wells
removed nitrate that would have been there.
Describe methods used in the study
(needed to ensure appropriate translation into use for planning and management
activities)
How was organic N mineralization from the same year
applications, previous year applications, and soil organic matter accounted
for?
Are the assumptions researchers used about appropriate N
application rates the same assumptions used in local dairies Nutrient
Management Plans?
The
intent was not to recommend the ‘appropriate N application rate’, therefore, we
made no assumptions as to how organic N mineralization from the same year
applications, previous year applications, or soil organic matter were accounted
for. The data presented in this report and other material (such as fact sheets,
field day presentations, or excel files in conference calls) is actual information
that was recorded and measured.
The
intent of the study was to document the activities that took place on the
research field such as the timing, amount, and method of manure
application. Other activities that were
documented included the time and amount of grass harvested, the time and amount
of irrigation water applied, and the fact that conventional tilling of the
field occurred prior to the start of the study in 2004. Other data that was
collected during the study by either WSU or the Department of Ecology consisted
of weather data, grass yield and nitrogen content, manure nutrient content,
soil nitrate-N data, irrigation water nitrogen content, and groundwater
nutrient content.
In
regard to the comment ‘need to ensure appropriate translation into the use for
planning and management activities’, we used a worksheet developed to estimate
plant-available nitrogen (Oregon State University Extension Bulletin EM 8954-E,
January 2008) as a method to approximate the amount of plant-available nitrogen
that was present each year of the study.
Table 5. Data from this study was entered into a
worksheet that estimates plant-available nitrogen (PAN) from manure (Oregon
State University Extension Bulletin EM 8954-E, January 2008).
|
Year |
PAN from manure NH4-N (lbs/acre) |
PAN from this year’s manure organic-N (lbs/acre) |
PAN from residual manure organic N (lbs/acre) |
Total manure PAN (lbs/acre) |
|
2005 |
211 |
96 |
33* |
341 |
|
2006 |
76 |
92 |
56* |
224 |
|
2007 |
85 |
99 |
65* |
249 |
|
2008 |
185 |
154 |
76 |
415 |
*The PAN from residual organic N (lbs/acre) prior to 2004 was estimated based on 2004 estimates because earlier data was not available.
In 2006 (May) and 2007 (June), there was 1 application of commercial
fertilizer applied late spring and early summer, when no manure was available.
Table 6. Calculations for plant-available nitrogen from commercial
fertilizer (communication with Dr. Dan Sullivan, Oregon State University in
April 2009).
|
Year |
PAN from commercial NH4-N fertilizer application (lbs/acre) |
Crop N removal from this years
PAN application (lbs/acre)* |
Unaccounted for PAN from
commercial fertilizer (stored in soil, stored below ground in plant, or lost
via gas loss or leaching; lbs/acre)** |
Residual N mineralized from
commercial N application (lbs/acre) |
|
2006 |
30 |
18 |
12 |
<1 |
|
2007 |
48 |
29 |
19 |
<1 |
* Above-ground crop nitrogen
removal efficiency for perennial grass is 60%.
** Remainder of nitrogen not recovered
in above-ground forage (40% of PAN) is stored in soil organic matter, roots, or
lost.
In 2006 and 2007, PAN application from commercial ammonium
fertilizer should be added to total PAN from manure to estimate the total
amount of PAN available from manure and commercial fertilizer.
Total amount of PAN available from manure and commercial
fertilizer (lbs/acre)
·
2006 = 224 + 30 = ~254
·
2007 = 249 + 48 = ~297
Table
7. Comparison between measured manure and commercial
fertilizer applications and calculations from the plant-available N worksheet (Oregon
State University Extension Bulletin EM 8954-E, January 2008).
|
Year |
Manure + Commercial Fertilizer
Ammonium-N (lbs/acre)* measured |
Manure + Commercial Fertilizer
Ammonium-N (lbs/acre)** |
Nitrogen Mineralized from Soil OM
(lbs/acre)*** calculated |
Sum of Measured Manure NH4-N,
Commercial Fertilizer N, and N Mineralized from Soil OM (lbs/acre) |
Total Manure + Commercial PAN
(lbs/acre) worksheet |
Difference between PAN and
Measured Manure and Commercial Fertilizer Ammonia + Estimated Mineralize N
from Soil (lbs/acre) |
|
2005 |
411 |
226 |
144 |
555 (370)^ |
341 |
214 (29)^^ |
|
2006 |
172 |
108 |
140 |
312 (248) |
254 |
70 (-6) |
|
2007 |
192 |
127 |
168 |
360 (295) |
297 |
82 (-2) |
|
2008 |
316 |
174 |
148 |
464 (322) |
415 |
49 (-93) |
|
Accum 2005 - 2008 |
1091 |
635 |
600 |
1690 (1235) |
1307 |
383 (-72) |
*Manure + commercial
fertilizer ammonium-N was not adjusted for volatilization losses in these
calculations.
**The assumption
was made that approximately 45% of the manure ammonium-N was volatilized.
***Estimated soil OM
= For every 1% Soil OM there is 20 lbs N available per acre per year for crops
(Cogger et al., 2001 and Sullivan et al., 2000).
^The values in
parenthesis have been adjusted for manure ammonia volatilization losses (column
labeled ‘Manure + Commercial Fertilizer Ammonium-N (lbs/acre)’ + column labeled
‘Nitrogen Mineralized from Soil OM (lbs/acre)’).
^^ The values in
parenthesis have been adjusted for manure ammonia volatilization losses (column
labeled ‘Sum of Measured Manure NH4-N, Commercial Fertilizer N, and N
Mineralized from Soil OM (lbs/acre)’ - column labeled ‘Total Manure +
Commercial PAN (lbs/acre)
worksheet’).
Results from Table 7 indicate that there is
similarity (less than 9% difference) between the measured amount of manure
ammonium nitrogen adjusted for volatilization losses + commercial fertilizer
nitrogen + estimated nitrogen mineralized from the soil and plant available
nitrogen estimates from worksheet in 3 of the 4 years.
Table
8. Measured crop nitrogen removal and plant
available nitrogen from manure and commercial fertilizer.
|
Date |
Crop Nitrogen Removal (lbs/acre) measured* |
Total Manure + Commercial PAN
(lbs/acre) worksheet |
Difference between measured crop nitrogen
removal and estimated crop nitrogen removal from PAN** |
|
2005 |
440^ |
341 |
99 |
|
2006 |
430 |
254 |
176 |
|
2007 |
458 |
297 |
161 |
|
2008 |
393 |
415 |
22 |
*Crop nitrogen
removal was measured by harvesting grass in 2-ft by 2-ft squares in 10
locations throughout a 22-acre field. Dry matter yield was estimated from the
grass harvested in the 2-ft by 2-ft squares. The grass from these squares was
sub-sampled and sent to a lab for crude protein and nitrate analyses. Dry
matter yield was multiplied by the nitrogen content (estimated from crude
protein content) in the grass samples to estimate nitrogen removal by the crop.
**The
difference between measured crop nitrogen removal and plant-available nitrogen
from manure and commercial fertilizer is partially the nitrogen that is
released from soil OM. We would estimate that nitrate-nitrogen released from
soil OM annually would be approximately 145 to 165 ppm.
^338
lbs/acre crop N harvested and removed from field + 102 lbs/acre of crop
nitrogen remaining in field because the last cutting was unable to be
harvested.
In 2005 and 2008 manure plus commercial fertilizer ammonium
nitrogen applied was approximately double the amount that was applied in 2006
and 2007. In 2005 and 2008 (99 and 22 lbs/acre, respectively), the difference
between measured crop nitrogen removal and plant available nitrogen from manure
and commercial fertilizer was less than in 2006 and 2007 (176 and 161 lbs/acre,
respectively; Table 8).
The equations in the worksheet used to calculate plant
available nitrogen from manure and commercial fertilizer do not account for
nitrate-nitrogen that will become available during the growing season from soil
OM. Therefore, the difference between measured crop nitrogen removal and plant
available nitrogen from manure and commercial fertilizer would be an estimate
of the amount of nitrate-nitrogen that is released from soil OM. The difference
between measured crop nitrogen removal and plant available nitrogen from manure
and commercial fertilizer in 2005 and 2008 (99 lbs/acre in 2005 and 22 lbs/acre
in 2008; Table 8) was less than the amount of nitrate-nitrogen that would be
available from the soil OM annually (approximately 145 to 165 ppm). This is an
indication that more manure ammonium nitrogen was applied in 2005 and 2008 than
the crop actually needed for growth throughout the year because there is a high
probability that more nitrate-nitrogen was release from soil OM than the 99 and
22 lbs/acre that was calculated in Table 8. This indicates that the crop did
not remove all of the nitrogen that was available over the growing season.
Explanation of how manure application rates were
determined. For example:
Who calibrated the equipment, how and when?
·
Custom operators did all of the manure
applications to the field. The custom operator that was doing manure
application at each event was not recorded. However, I know of 2 custom operators
that did manure applications (Northwest Liquid Transport and Edaleen
Dairy). I believe Pacific Pumping may
have done some of the manure applications in the first 2 years of the study.
·
Who calibrated the equipment, how and
when was not recorded during this study.
Who ran the equipment making the applications?
·
Employees who worked for Northwest
Liquid Transport, Edaleen Dairy, and Pacific Pumping drove the tractor that
applied manure to the field.
Who collected the manure tests for each application, how
and when?
·
Lynn VanWieringen with WSU Livestock
Nutrient Management Program collected the manure sample as it was coming out of
the manure application equipment at each manure application event. Lynn would
walk out to the manure application equipment while manure was being applied to
the test field and fill a 5-gallon bucket with manure. The manure in the bucket would be stirred
vigorously and a sample would be taken to measure the ammonia N content with an
Agros Meter. As soon as that sample was analyzed, the remaining manure in the
5-gallon bucket would be stirred vigorously and manure would be placed in
nalgene containers. The manure samples would be placed in a freezer within a
half- hour of being acquired.
Who determined the rate and method of manure application?
·
The dairy farmer
Who recorded the actual amount of manure applied?
·
The custom operators had a flow meter on
the pump or in the tractor that was monitored while manure was applied to the
field. Typically Lynn would ask the dairy farmer how much he intended to put
on, and then would ask the tractor driver how much was being put on while the
sample was being collected. However, prior to any amount being entered
in the spreadsheet, the dairy farmer would calculate the actual amount of manure
that went onto the field from the bill that the custom operator sent. This
system is not as precise as if this was a ‘controlled research study’ where the
researcher actually applied and measured manure application rates. However,
because there is a cost associated with manure application, the amount that was
actually applied to the field was agreed upon by both the custom operator and
dairy farmer. If the custom outfit said that more was applied than actually was
the dairy farmer would get upset for paying too much money and too high of an
application rate, and if the custom operator said less was applied than actual
was they would receive less money.
How did the researchers and the farm operator communicate
information regarding soil and manure tests and application time and rates?
The dairy farmer and Lynn would talk on the phone, in
person, or by e-mail. Many times the dairy farmer left a message on the phone
answering machine as to when manure would be applied or when grass would be
harvested. All data was sent to the dairy farmer prior to each conference call
related to the study. At different times during phone conversations the data
would be discussed.
Barb Carey from the Department of Ecology would e-mail the
dairy farmer about when she would be coming up to do groundwater sampling. Barb
and the dairy farmer would visit at times while she was sampling.
Conventional
tilling of the soil (subsoiling, rotatilling plowing, seedbed preparation, and
cultimulching) probably caused the greatest increase in soil nitrate-N and
groundwater nitrate+nitrite-N concentrations in this study. The average
groundwater nitrate+nitrite-N concentration during the fall following
conventional tilling (November 2004 through January 2005) was ~27 mg/L. The average
groundwater nitrate+nitrite-N concentration the second fall after conventional
tilling (November 2005 through January 2006) was ~17 mg/L.
The
accumulative amount of manure total N applied over a growing season likewise
had a major impact on soil nitrate-N and groundwater nitrate+nitrite-N
concentrations. In 2008, when approximately double the amount of manure total N
was applied that of grass N harvested, soil nitrate-N and groundwater
nitrate+nitrite-N concentrations increased in the fall and winter,
respectively. In November 2008, the average groundwater nitrate+nitrite-N
concentration was 6 mg/L, and increased to 11 mg/L in December 2008. This level is only slightly higher than the
drinking water standard of 10 mg/L. However, denitrification associated with
low dissolved oxygen concentrations lowered nitrate-N concentrations in some
wells.
Timing
of manure total N applied can impact soil nitrate and groundwater
nitrate+nitrite-N concentrations. In 2006, the amount of grass nitrogen
harvested was greater than the amount of manure total N applied. Therefore, the
assumption could be made that soil nitrate-N and groundwater nitrate+nitrite-N
concentrations should have remained relatively low throughout the fall and
winter months, respectively. However, 90 lbs/acre of manure total N applied in
October after the last cutting of grass probably lead to elevated groundwater
nitrate+nitrite-N concentrations during the winter (November 2006 – 7 mg/L,
December 2006 - 13 mg/L, and January 2007 – 15 mg/L).
Grass
yield, and hence the amount of nitrogen removed, can be impacted by weather
conditions.
In
2005, the grass growth slowed when soil moisture levels dipped below 20%. Irrigating earlier in the growing season
during subsequent years (July instead of August) prevented soil moisture levels
from dipping below 20%. In some years,
this reduced the time between cuttings by over 1 week during the summer months.
Air
temperature can impact grass growth. In
2008, the quantity of grass harvested was lower than previous years. A measure of daily accumulation of heat (GDU)
indicated approximately 696 less GDU (42%) in 2008 (the coolest year of the
study) than in 2007 (the warmest year of the study). It appeared that lower thermal heat over time
impacted grass yields in 2008.
Cogger, C.G., A.I. Bary, S.C. Fransen, and D. Sullivan. 2001. Seven years of biosolids versus inorganic nitrogen applications to tall fescue. J. Environ. Qual. 30:2188-2194.
Fraser, D.A. 2006. Determining
range readiness and growing degree-days (GDDs). B.C. Min. For. Range, Range
Br., Kamloops, B.C. Rangeland Health Brochure 11.
Griffith S. M. and T. W. Thomson.
1996. N Rate and timing relationships with tissue N concentration and seed
yield in perennial ryegrass. Seed Production Research at Oregon State
University.
Sullivan, D. M. 2008. Estimating
Plant-available Nitrogen from Manure. Oregon State University Extension
Bulletin EM 8954-E.
Sullivan, D. M., C.G. Cogger, A.I.
Bary, and S.C. Fransen. 2000. Timing of dairy manure applications to perennial
grass on well drained and poorly drained soils. J. Soil Water Conserv.
55:147-152.