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Variable crop residue managementMyers, Brian January 1900 (has links)
Master of Agribusiness / Department of Agricultural Economics / Jeffery R. Williams / Production agriculture is constantly evolving to become more efficient and
productive. Crop residue serves as a valuable source of nutrients for the soil, but it is
increasingly abundant with today’s enhanced crop genetics. If new technology can
effectively provide a way to micro-manage crop residue levels within a field, the benefits
will go beyond soil health. Surplus crop residue can be collected for secondary income
while leaving the optimum amounts in the field to maintain the environment and soil health
as well as promote future crop growth. The main objective of this study is to create a
budget model that will determine the economic impact of crop residue removal on a
controlled basis. The goals are to determine crop residue removal practices that are
sustainable for the long-term, while also enhancing soil quality and increasing grain yield
in future years. A sub-objective is to build a business case for producers to invest in
variable crop residue management. The hypothesis presented in this study is that the
increased complexity and price of a variable rate system is offset by more supplemental
profits, increased crop yields, and better management of soil health and nutrients.
The negative perceptions of crop residue removal include the fear of soil erosion or
loss of soil organic matter. By developing a budget model that is easy to use, takes
advantage of existing field data for inputs, and allows producers the ability to look at their
operations on a sub-field level, this study aims to provide the necessary motivation to
invest in new technology that will increase their productivity. By entering their site-specific
crop residue return rate data into a budget model, along with prices and costs related to
combine and auxiliary equipment, corn and corn stover, transportation and logistics, and
nutrient replacement, they will come up with a return per acre for both constant rate and
variable rate collection.
The budget model determines whether it is economically viable to harvest crop
residue from a continuous corn rotation at a variable rate across a field, rather than at a
constant rate, using a producer’s own specific field data. To validate the concept, data from
a joint study between John Deere and Iowa State is entered into the model. Prescriptions
for corn stover return rates are provided from the study for pre-defined grid areas.
Prescriptions are derived from a combination of data including grain yield, soil loss due to
wind and water erosion, climate, topography, and soil sample data at time of planting
(Nelson, et al. 2004).
The average corn stover removal percentage was less for variable rate collection
than constant rate collection, 26.05% to 31.85%. However, the assumption that grain yield
and corn stover yield are positively correlated did not prove to be true in this case study.
The variable rate plots had a lower average grain yield of 158.84 bushel/acre, compared to
160.46 for the constant rate plots, but they had more total corn stover available and
therefore a higher return rate of 3.70 tons/acre, compared to 3.05 for the constant rate plots.
This case study illustrates that less corn stover can be returned to the field through constant
or variable rate collection while sustaining higher grain yields than a conventional harvest
that would return all of the corn stover to the field. This case study demonstrates that
variable rate collection can be more expensive than constant rate, but not in every situation.
Every unique field site will require a specific crop residue management recommendation
that is determined by both economic and environmental factors.
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The growth of annuals sown in rice stubble /Muirhead, Warren Alexander. January 1967 (has links) (PDF)
Thesis (M. Ag. Sci) -- University of Adelaide, Dept. of Agriculture, 1967. / Includes bibliography.
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Tall fescue growth and nitrogen uptake as influenced by non-thermal residue managementQureshi, Maqsood Hassan 06 December 1994 (has links)
Graduation date: 1995
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Tillage and residue management effects on soil organic matter dynamics in a sandy-loamHalpern, Moshe T., January 1900 (has links)
Thesis (M.Sc.). / Written for the Dept. of Natural Resource Sciences. Title from title page of PDF (viewed 2009/6/25). Includes bibliographical references.
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Crop residue management and its impacts on soil propertiesHe, Yuxin January 1900 (has links)
Doctor of Philosophy / Agronomy / DeAnn R. Presley / Crop residue removal for livestock feeding and biofuel production at large scales must be evaluated to assess impacts on soil productivity and properties. Among all the potential negative impacts, wind erosion is a major concern in the central Great Plains. We conducted an on-farm study from 2011 to 2013 by removing crop residue at five levels (0, 25, 50, 75, and 100%) to determine the effects of crop residue removal on soil wind erosion parameters such as dry aggregate size distribution including soil wind erodible fraction (EF <0.84 mm aggregates), geometric mean diameter (GMD) and geometric standard deviation (GSD), dry aggregate stability, and soil surface roughness. The sub-model of Wind Erosion Prediction System (WEPS) developed by the USDA-ARS, Single-event Wind Erosion Evaluation Program (SWEEP) is a stand-alone companion software package that can be applied to simulate soil loss and dust emission from a single windstorm event. We applied measured data (i.e. EF, GMD, GSD, and roughness) to SWEEP for predicting wind velocity that can initiate wind erosion and soil loss under each crop residue removal condition with wind velocity at 13 m sˉ¹. The threshold wind velocity to initiate wind erosion generally decreased with increase in crop residue removal levels, particularly for residue removal >75%. The total amount of soil loss in 3 hours ranged from about 0.2 to 2.5 kg mˉ² and depends on soil condition and crop residue cover. On the other hand, high-yielding crops can produce abundant crop residue, which then raises the question that if a farmer wants to reduce residue, what could they do without removing it? The application of fertilizer on crop residue to stimulate microbial activity and subsequent decomposition of the residue is often debated. We conducted wheat straw decomposition field experiments under different fertilizer rates and combinations at three locations in western Kansas following wheat harvest in 2011 and 2012. A double shear box apparatus instrumented with a load cell measured the shear stress required to cut wheat straw and photomicrography was used to measure the cross-sectional area of wheat straw after shearing. Total C and N were also analyzed. The fertilizer rate and timing of application during summer 2012 and Fall 2013 at the Hays site had impacts on wheat straw shear stress at break point. Across site years, earlier (fall) fertilizer application generally resulted in lower remaining aboveground biomass as compared to a spring application. Multivariate and linear regressions suggested that N and C:N ratio partially explain the results observed with respect to treatment effects on winter wheat residue decomposition.
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CO2 emission and O2 uptake of soil under different systems / Emissão de CO2 e captura de O2 do solo em diferentes sistemasAlmeida, Risely Ferraz [UNESP] 21 February 2017 (has links)
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Previous issue date: 2017-02-21 / Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES) / O oxigênio (O2) e o dióxido de carbono (CO2) no solo são os dois principais gases relacionados com a atividade dos microorganismos no solo. Assim, esta tese foi desenvolvida para observar a concentração e a relação entre a concentração do CO2 e O2 sob diferentes sistemas de resíduos. Para isso, realizamos dois experimentos de solo no Brasil e nos EUA, respectivamente. O primeiro experimento foi desenvolvido para examinar a relação entre fluxo de CO2 (FCO2) e o fluxo de O2 (FO2) usando a umidade do solo e o O2 como um predictor da respiração do solo em uma área de cana-de-açúcar sob diferentes manejos de resíduos (colheita mecânica - GH versus colheita queimada – BH). Portanto, os resultados do primeiro experimento estão descritos no Capítulo 2 e sendo intitulado de "Uso da captura de O2 como índice de respiração de CO2 em áreas de cana-de-açúcar sob diferentes manejos". O segundo experimento do solo observou o impacto do biochar na emissão ou sorção de CO2 e O2 nos solos. Assim, foram estudados três tipos de solos (Rosemount - RM, Potting Sol Sunshine - PS e UM), cinco biochars diferentes (biochar de chip de pinho - ICM, biochar de Carvalho Oak Royal - RO, biochar Acurel ativado - AAC, biochar de Bambu - B; biochar de Macadâmia - MC) e o tratamento controle (solo sem biochar). Consequentemente, os resultados foram descritos no Capítulo 3 e intitulado "Como a captura de O2 pode nos ajudar a entender os processos de sorção de CO2 via biochar?". Assim, nós podemos concluir com os nossos resultados que a concentração e relação entre FCO2 e FO2 dependem dos diferentes sistemas e condições dos solos estudados, tais como: manejo de resíduos de culturas do solo, umidade do solo e uso de biochar. O FO2 está positivamente correlacionado com o FCO2 via atividade biológica e com valores de coeficientes respiratório (RQ) próximos de 1,0. Além disso, podemos observar que valores de RQ maiores que 1 são resultados dos fluxos de troca solo-gás após precipitação ou maior disponibilidade de O2 no meio. Assim, o FO2 pode ser utilizado como um índice para categorizar uma fonte de respiração de CO2. Para concluir, o biochar pode ser utilizado para sequestrar CO2 da atmosfera em curto período de tempo. No entanto, acreditamos que mais estudos devem ser desenvolvidos para elucidar a sorção de CO2 e O2 pelo biochar e suas reações (biológicas e/ou químicas) quando adicionado biochar no solo. / The soil O2 and CO2 concentration are the two most important gases related to soil microorganisms. Thus, this thesis was developed to observe the concentration and relationship between carbon dioxide (CO2) and oxygen (O2) under different residue systems. For that, we run two soil experiments in Brazil and the USA, respectively. The first experiment was developed to examine the relationship between CO2 and O2 using soil moisture and O2 as a soil respiration predictor in a sugarcane area under different managements of residues (mechanical harvesting - GH versus straw burning - BH). Therefore, the first experimental results are described in the Chapter 2 and entitled “Use of O2 uptake as an index of CO2 respiration in sugarcane areas under different managements”. We run the second soil experiment measuring biochar’s impact on CO2 production or sorption and O2 uptake in amended soils. Thus, we studied three soil types (Rosemount - RM; Potting soil Sunshine - PS; and UM) and five different biochars (Pine chip biochar - ICM; Royal Oak hardwood lump charcoal - RO; Accurel activated charcoal - AAC; Bamboo - B; and Macadamia nut - MC) and control treatment (Soil without biochar). Consequently, the results are described in the Chapter 3 and entitled “How O2 uptake can help us understand the CO2 sorption processes by biochar?”. Thus, we can conclude with our results that the concentration and relationship between FCO2 and FO2 depend on different systems and soil conditions, for example: soil crop residue managements, soil moisture and use of biochar. The FO2 is positively correlated with FCO2 at biological condition with respiratory quotient (RQ) values close to 1.0. Moreover, we can observe that RQ values higher than 1 are results of soil–gas exchange fluxes after precipitation or higher available on O2. Thus, the FO2 can be used as an index for categorizing the source of FCO2 respiration. To finish, we can observe that the biochar can be used to sequester CO2 from the atmosphere by the absence of biological activities in a short period of time. However, we believe that more study should be developed to elucidate the CO2 and O2 sorption by biochars and their reactions (biological and/or chemical) when added biochar in soil.
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The growth of annuals sown in rice stubbleMuirhead, Warren Alexander. January 1967 (has links) (PDF)
Includes bibliography.
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Annual bluegrass (Poa annua L.) emergence under different residue management practices in perennial ryegrass and determination of resistant and susceptible annual bluegrass germination under controlled temperature and moistureSchuster, Matthew D. 03 December 1999 (has links)
With the loss of field burning the amount of crop residue that remains in
perennial ryegrass fields has increased. As the amount of crop residue remaining in the
field increases so does annual bluegrass. This has resulted in the increased use of
herbicides to control annual bluegrass. However, this increased use has also resulted in
herbicide-resistant annual bluegrass. Field experiments were initiated in 1997 to
investigate residue management options available to growers and their impacts on
annual bluegrass emergence. Two sites, Glaser and Wirth, were established with three
residue management treatments replicated four times. The treatments included full-straw,
bale/flail, and vacuum sweep. Perennial ryegrass seed yield and annual bluegrass
seed contamination were evaluated. The vacuum sweep treatment had lower annual
bluegrass emergence than the full-straw or the bale/flail treatments during the 1997-98
growing season, for both sites. The fall of 1998 was much drier than the fall of 1997.
Annual bluegrass emergence in all plots was lower in 1998 than in 1997 because of the
dry conditions. Fall emergence in 1998 was higher in the vacuum sweep treatment than
in the other two treatments, which may have been the result of better soil-seed contact
in the vacuum sweep treatment. Lower emergence in the spring at the Wirth site
compared to the Glaser site may have been due to narrow crop row spacing and cultivar
selection, which shaded the annual bluegrass. When growing seasons were combined,
there were no treatment differences. However, more emergence was observed in the
spring at the Glaser site compared to the Wirth site. Yield was highest for the vacuum
sweep treatment at the Glaser site in the 1998-99 growing season. However,
competition from volunteer perennial ryegrass in the full-straw and bale/flail treatments
could have accounted for this increase. No other differences in yield and no difference
in contamination among treatments were observed. However, contamination at the
Glaser site was higher in the 1998-99 growing season than in the 1997-98 growing
season.
Experiments were conducted in growth chambers to determine how differing
environmental conditions affect seed germination of diuron-susceptible and diuron-resistant
annual bluegrass. Cumulative germination for the susceptible-biotype
decreased from 96% to 88% while the resistant-biotype remained above 95% as
temperature decreased from 3 0/20 C to 10/2 C. The susceptible-biotype germinated
sooner than the resistant-biotype regardless of temperature. The susceptible-biotype
had a higher rate of germination than the resistant-biotype at 30/20 C, but not when the
temperature decreased to 10/2 C. Germination response to differing matric potentials
did not vary much within a biotype for a given soil type and temperature. Therefore,
parameters estimated at -1.03 MPa were chosen to contrast susceptible- and resistant biotypes,
and soil types, for each temperature. Maximum cumulative germination was greater than 96% for all treatments. When germination on a given soil type was
contrasted, differences were only seen for the susceptible biotype vs. resistant biotype
on Dayton soil; and the resistant biotype on Dayton soil vs. resistant biotype on
Woodburn soil at both temperatures. The lag in onset of germination was shorter for
the susceptible biotype on Dayton soil and resistant biotype on Woodburn soil than the
resistant biotype on Dayton soil at 30/20 C. At 18/5 C, the lag in onset of germination
was shorter for the susceptible biotype on Dayton soil and resistant biotype on
Woodburn soil than the resistant biotype on Dayton soil (P = 0.000 1 and 0.0001,
respectively). But the rate of germination was faster for the resistant biotype on Dayton
soil than both the susceptible biotype on Dayton soil and resistant biotype on Woodburn
soil at 18/5 C (P = 0.02 and 0.0004, respectively). The rate of germination did not
differ at 3 0/20 C. When just the soils were contrasted, at 18/5 C all annual bluegrass
seeds on the Woodburn soil germinated sooner and the rate of germination was higher
than on the Dayton soil. These results indicate that the hydraulic properties of the soils
may influence germination. However, this was not observed at 30/20 C. The results
suggest that the susceptible-biotype was more sensitive to temperature while the
resistant-biotype was more sensitive to moisture. Changing crop management in ways
that will reduce annual bluegrass emergence and establishment is needed. By altering
management strategies, growers may obtain more efficient and effective use of
herbicides, while reducing the selection of herbicide-resistant annual bluegrass. / Graduation date: 2000
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Physiological responses of creeping red fescue to stubble management and plant growth regulatorsMeints, Paul David 29 September 1997 (has links)
Legislation to reduce open field burning in grass seed fields within the Willamette
valley of western Oregon changed established production practices. In the creeping
grasses such as Kentucky bluegrass (Poa pratensis L.) and creeping red fescue (Festuca
rubra L.) non-thermal management resulted in reduced yield.
Studies were conducted to examine the effects of three stubble height treatments in
comparison to open field burning in creeping red fescue seed production. The effects of
light quality on characteristics of plant development were investigated in field and
controlled environments. Exogenous applications of plant growth regulators (PGR's)
were made to elucidate the causes of low seed yields observed without burning.
Field plots were prepared in fall of 1994, and 1995 in creeping red fescue
commercial production fields as well as at Hyslop research farm in 1995. Three cultivars
were included in the trial; Shademaster and Hector, which produce many rhizomes, and
Seabreeze which produces few rhizomes. The effects of stubble height, PGRs, and field
burning were measured during fall regrowth and flowering. Non-structural carbohydrates available for early regrowth were reduced when stubble was removed below 5.0 cm,
particularly in first-year stands. Fall tiller height was increased by stubble remaining and
was negatively correlated with flowering. Rhizome development was reduced when
stubble was removed mechanically or burned to the crown, whereas yield potential was
increased.
Fall ethylene application reduced fall tiller height, fall tiller number, and percent
fertile tillers the following spring and was similar to control treatment compared with
burn. Other PGRs did not produce consistent results in this study. Excess ethylene
produced by decaying stubble may impact floral induction and reduce yield potential in
creeping red fescue seed crops.
Light quality as measured by red:far-red ratio (R:FR) was reduced by canopy
closure during regrowth but not by the presence of stubble. In controlled environment
studies, red light (R) promoted taller tillers, greater stage of development, and greater
tiller number than far-red (FR) light. Sunlight enriched with FR completely inhibited
rhizome formation. Results suggest that environments with excess reflected FR may
negatively impact early development of creeping red fescue seed crops. / Graduation date: 1998
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EFFECTS OF UTILIZING CROP RESIDUES IN WINTER FEEDING SYSTEMS ON BEEF COW PERFORMANCE, REPRODUCTIVE EFFICIENCY AND ECONOMICS2013 June 1900 (has links)
Over 2 years (Year 1, 2009-2010; Year 2, 2010-2011), two separate experiments were conducted to evaluate the effects of winter feeding system (n=3) on beef cow performance, reproductive performance, economics and forage degradability. The three systems (treatments) were grazing pea crop residue (PEA) cv. ‘Performance 40-10’ (Year 1, TDN = 50.2%, CP = 7.3%; Year 2, TDN = 56.9%, CP = 8.9%) in field paddocks, grazing oat crop residue (OAT) cv. ‘Baler’ (Year 1, TDN = 59.1%, CP = 2.9%; Year 2, TDN = 66.9%, CP = 5.3%) in field paddocks, and feeding mixed grass-legume hay in drylot pens (DL) (Year 1, TDN = 61.4%; CP = 8.8%; Year 2, TDN = 52.3%, CP = 12.3%). In the first experiment, 90 dry, pregnant Black Angus cows (Year 1, 629 kg ± 74 kg; Year 2, 665 ± 69 kg) stratified by body weight (BW) and days pregnant were randomly allocated to 1 of the 3 systems. Cows were allocated feed in the field or pen on a 3 d basis and supplemented oat grain daily at 0.4-0.6% BW depending on environmental conditions. Dry matter intake (DMI) was estimated for each system using the herbage weight disappearance method. Cow BW, body condition score (BCS), and rib and rump fat were measured at start and end of trial and cow BW was corrected for conceptus gain based on calving data.
When data from the first 20 d were pooled over 2 years, initial cow BW was greater (P < 0.01) for the DL and OAT cows compared to the PEA cows and final cow BW was different (P < 0.01) between all 3 winter feeding systems. The change in BW was also greater (P < 0.01) for DL cows compared to cows on the OAT and PEA treatments. Analysis of the first 20 d of Year 1 study period and the total Year 2 study period, showed a significant (P < 0.01) year by treatment interaction for final BW and BW change. The differences (P < 0.01) in initial BW, final BW and BW change between the first 20 d of Year 1 study period and the total Year 2 study period (20 d) suggest feed quality, animal preference and weather conditions may cause difficulties when grazing residues in winter grazing systems.
Analysis of the entire trial period in Year 1 (62 d) indicates differences (P < 0.01) for final BW and BW change between cows on all three systems. The change in rib and rump fat was also different (P < 0.01) between cows in all 3 systems. In Year 2 (20 d), initial BW, final BW and BW change were different (P < 0.01) between DL and PEA cows, and between (P < 0.01) OAT and PEA cows. No difference (P > 0.05) was found for cow rib and rump fat in Year 2 and no difference (P > 0.05) was found for BCS in either Year 1 or Year 2 for cows managed in all 3 systems. Differences (P < 0.05) were observed for calving rate and calf birth weight between the DL and OAT system cows, but not between (P > 0.05) cows managed in the DL and PEA or OAT and PEA systems. Costs per cow per day were $1.22, $1.01 and $2.77 for PEA, OAT and DL systems in Year 1, respectively. In Year 2, cow costs per day were $1.59, $1.44 and $1.84 for PEA, OAT and DL systems, respectively.
In experiment 2, three ruminally cannulated, dry Holstein cows were fed a silage based total mixed ration (TMR) of 22 kg barley silage, 7 kg chopped alfalfa hay and 1 kg energy supplement (DAC-485). In-situ degradability was studied to determine the extent of degradation of pea, oat and grass-legume hay collected at start (SOT) and end of test (EOT) in experiment one. Rate of degradation (Kd) of DM was greater (P < 0.01) for PEA EOT compared to HAY, OAT SOT and OAT EOT. Dry matter rate of degradation for PEA SOT was greater (P < 0.05) compared to OAT SOT and OAT EOT. The effectively degradable fraction of CP was greater (P = 0.03) for HAY compared to PEA EOT. The ruminally undegradable fraction of CP was greater (P = 0.03) for PEA EOT compared to HAY. Acid detergent fiber rate of degradation (Kd) was greater (P = 0.01) for PEA EOT compared to HAY, OAT SOT and OAT EOT. Acid detergent fiber rate of degradation for PEA SOT was greater (P < 0.05) compared to OAT SOT and OAT EOT. No differences (P > 0.05) were observed between either OAT SOT and OAT EOT or PEA SOT and PEA EOT for S, D, U, ED or RU suggesting that weathering did not have an effect on the degradability of the forages.
The results of these experiments show that it is possible to maintain cow BW through the winter months in Western Canada by grazing oat crop residues, which have the potential to reduce winter feeding costs.
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