The Effects Of Tillage Elimination On Intensive Soft Red Winter Wheat Production Systems PDF Download

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Effects of Tillage System, Grazing, and Seeding Date on Grain Yield of Hard Red Winter Wheat (Triticum Aestivum) and Effect of Production Objective and Tillage System on Forage Production

Effects of Tillage System, Grazing, and Seeding Date on Grain Yield of Hard Red Winter Wheat (Triticum Aestivum) and Effect of Production Objective and Tillage System on Forage Production
Author: Deena Leigh Morley
Publisher:
Total Pages:
Release: 2006
Genre:
ISBN:

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Managing Cover Crops Profitably (3rd Ed. )

Managing Cover Crops Profitably (3rd Ed. )
Author: Andy Clark
Publisher: DIANE Publishing
Total Pages: 248
Release: 2008-07
Genre: Technology & Engineering
ISBN: 1437903797

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Cover crops slow erosion, improve soil, smother weeds, enhance nutrient and moisture availability, help control many pests and bring a host of other benefits to your farm. At the same time, they can reduce costs, increase profits and even create new sources of income. You¿ll reap dividends on your cover crop investments for years, since their benefits accumulate over the long term. This book will help you find which ones are right for you. Captures farmer and other research results from the past ten years. The authors verified the info. from the 2nd ed., added new results and updated farmer profiles and research data, and added 2 chap. Includes maps and charts, detailed narratives about individual cover crop species, and chap. about aspects of cover cropping.


The Effects of Tillage Systems and Seeding Dates on Grain Yields of Wheat (Triticum Aestivum Vill., Host) on the Anatolian Plateau of Turkey

The Effects of Tillage Systems and Seeding Dates on Grain Yields of Wheat (Triticum Aestivum Vill., Host) on the Anatolian Plateau of Turkey
Author: Thomas G. Zinn
Publisher:
Total Pages: 132
Release: 1978
Genre: Wheat
ISBN:

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Wheat (Triticum aestivum) is the major food crop produced on the Anatolian Plateau of Turkey where due to limited rainfall the farmers follow the traditional system of fallow farming. They are presently producing an average of 1.15 tons of grain per hectare during the crop year. This rate of production does not meet the needs of the country and during the last 15-20 years Turkey has frequently had to import wheat. The present fallow system permits extensive livestock grazing during the late fall and winter months in the noncrop year. Spring tillage practices are delayed to permit weed growth for additional foraging by livestock during the early and late spring period. This delayed spring tillage, using wooden or steel plows, leaves the soil loose and subject to rapid drying. Little plant residue is left on the surface to protect the soil and maintain water infiltration rates. The farmer also must cultivate several times before planting in order to prepare a satisfactory seedbed. Under these conditions Turkish farmers have learned that seed planted early in the fall in dry, warm soil may be germinated by light rain, subsequently dry out and then die. Thus, they have over time adopted the practice of delaying planting until late fall when temperatures are cooler and frequent rains more certain. Under these conditions the crop is largely dependent upon late spring and early summer rains for satisfactory grain production. Climate in dryland regions of Oregon and Washington are similar to those in the Anatolian Plateau. Previous research conducted on the Anatolian Plateau indicated that modified technology from Oregon and Washington could be adopted to Turkish conditions resulting in substantial increases in grain yield. The objective of this study was to compare three fallow-tillage systems for moisture conservation and early vs. late seeding dates on subsequent grain yield of wheat. The tillage treatments were (1) a fall chisel operation followed by a spring chisel tillage, (2) chiselling twice in the spring in perpendicular directions, and (3) moldboard plowing in the spring. All three systems received subsequent tillages with a sweep-harrow combination as required to maintain a weedfree fallow and uniform seedbed. The amount of moisture conserved was not affected by the three tillage systems employed and grain yield was not different due to tillage method. All of the systems conserved sufficient water to allow early seeding into residual moisture with a deep furrow drill. A 94 per cent stand emerged within 15 days. At a later sowing date wheat was seeded into dry soil using a double disc drill. Emergence was delayed due to late rains. After 56 days an 89 per cent stand had emerged. In this experiment a 36 per cent grain yield increase resulted from early seeding; 3.79 tons per hectare compared to 2.79 tons per hectare from the late seeded plots, a highly significant difference. The 3.79 tons per hectare is 2.64 tons per hectare more than the average yield from local farms, where a traditional fallow system is followed. The major components contributing to the yield increases from early seeding were (1) more plants and heads per unit area, (2) more kernels per head and to a lesser degree (3) kernel weight. This study suggests that if Turkish farmers adopt improved summer fallow systems, wheat yields can be increased significantly; thus, reducing or perhaps eliminating the need for importing wheat. However, the loss of grazing land under a clean fallow system for livestock will need to be evaluated in terms of the total economic and social conditions to determine if the increased wheat yields warrant the change in farming practices. It is anticipated that the loss of forage during the fallow period would be offset by the increase of stubble and cereal aftermath as a result of grain yield increase during the cropping sequence.


Long-term Effects of Tillage, Nitrogen, and Rainfall on Winter Wheat Yields

Long-term Effects of Tillage, Nitrogen, and Rainfall on Winter Wheat Yields
Author: Kelli Marie Camara
Publisher:
Total Pages: 466
Release: 1999
Genre: Nitrogen fertilizers
ISBN:

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Winter wheat is commonly grown in dryland cropping systems in the Pacific Northwest region of semi-arid eastern Oregon. For agronomic, economic, and environmental reasons, it is important to understand the long-term sustainability of such dryland systems. The objective of this study was to evaluate the long-term effects of tillage, nitrogen (N), soil depth, and the influence of precipitation on wheat yields in dry land cropping systems of eastern Oregon. Data were taken from the Tillage/Fertility or "Balenger" experiment, which was established in 1940 by a Soil Conservation employee, and is one of the oldest replicated research experiments in the western United States. The experiment consisted of a winter wheat-summer fallow rotation arranged in a randomized block design with three replications. The main plot consisted of three primary tillage treatments (moldboard plow, offset disk, and subsurface sweep) and subplots consisted of six nitrogen treatments that changed over time and most recently ranged from 0 to 180 kg ha−1. Soil depth of individual plots ranged from 1.2- to 3.0-m. The study was divided into four main time periods (1940-1951, 1952-1961, 1962-1987, and 1988-1997) within which experimental treatments were consistently maintained. The moldboard plow tillage treatment significantly increased yields by more than 300 kg ha−1 over the subsurface sweep tillage treatment in all four time periods. Yields with the moldboard plow system were significantly higher than with the offset disk system in time periods 3 and 4. The same trend was evident for mean yield in time periods 1 and 2, but differences were not statistically significant. In time periods 1, 2, and 3, mean yields were higher with the offset disk tillage treatment than the subsurface sweep tillage system, although the differences were not statistically significant. In time period 4, mean yield was higher for the subsurface sweep system than the offset disk treatment, but differences were not statistically significantly. The optimum amount of N for winter wheat differed from year to year, within, and between experiment periods. This was apparently in response to rainfall patterns and improved management factors, specifically more N responsive semi-dwarf varieties. For time period 1, the maximum fertilizer rate was 11.2 kg N ha−1, which tended to produce higher mean grain yields than an application rate of than 0 kg N ha−1, regardless of the quantity or distribution of precipitation. For time period 2, the maximum fertilizer rate was 33.7 kg N ha−1, which produced significantly higher grain yields than an application rate of than 0 kg N ha−1, regardless of the quantity or distribution of precipitation. For time period 3 (1962-1987), which had below-normal annual and growing season precipitation, yield increased with the addition of 45 kg N ha−1. For time period 4 (1988- 1997), which had above-normal annual and growing season precipitation, yield increased with the addition of 90 kg N ha−1. Yield increases at greater rates of N were insignificant. For time periods 3 and 4, maximum mean yield was obtained at an application rate of 135 kg N ha−1. The response of wheat yield to N during dry years was greater for deep (> 2.8 m) soils than for shallow soils. In addition to amount, rainfall distribution during the winter (October to March) and growing (April to June) season significantly affected yield. Results demonstrate the importance of rainfall and nitrogen to winter wheat production in eastern Oregon, and that the most environmentally sound tillage systems are not necessarily the most profitable from farmers' point of view.


Growing Winter Wheat on the Great Plains

Growing Winter Wheat on the Great Plains
Author: Ellery Channing Chilcott
Publisher:
Total Pages: 24
Release: 1917
Genre: Wheat
ISBN:

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"Limited rainfall is the controlling factor in crop production in the Great Plains. The average yields of a series of years can be foretold from the records of past years; but because the rainfall is fluctuating in amount and uncertain in distribution, the yields of a simple year can not be foretold with any certainty. The chances of success are, however, much better when the soil is wet to a considerable depth at seeding time than they are when the soil contains little or no available water at that time. The relation between the amount of water in the soil at seeding time and the yield is much closer with winter wheat than with other crops. This crop should, therefore, be seeded on the best-prepared land and that in which the greatest amount of water is stored. Except in the southern section, the response of winter wheat to summer tillage is greater than that of any other crop. Summer-tilled land should be seeded to winter wheat wherever this crop can be grown. The growth of corn is one of the best preparations for winter wheat, especially north of Kansas. With increase in the length of season and the time between harvest and seeding, there is an increase in the value of early preparation for winter wheat. In the northern section the crop can be replaced with spring wheat without serious loss. In the central section winter wheat has a greater advantage over spring wheat and can not be replaced by the latter without serious loss. In the southern section, winter wheat is less certain and less productive than farther north and can not be replaced by spring wheat. It is, however, profitably raised under favorable conditions of oil, season, and preparation. In this section particularly it should be recognized that the chances of producing a crop are low when it is seeded on land that does not contain water enough in storage to wet the soil to a depth of 3 feet."--Page 2