Bibliography: leaves 153-179. / xvi, 179 leaves : ill. (some col.) ; 30 cm. / Title page, contents and abstract only. The complete thesis in print form is available from the University Library. / Annual species of Medicago, or medics, are important pasture legumes in the neutral to alkaline soils of southern Australia but their nodulation and nitrogen fixation processes are retarded by soil nitrate. This study ascertains whether an observed tolerance to nitrate among medic species can be substantiated, and attempts to understand the underlying factors responsible. / Thesis (Ph.D.)--University of Adelaide, Dept. of Plant Science, (1995)

Bibliography: leaves 153-179. Annual species of Medicago, or medics, are important pasture legumes in the neutral to alkaline soils of southern Australia but their nodulation and nitrogen fixation processes are retarded by soil nitrate. This study ascertains whether an observed tolerance to nitrate among medic species can be substantiated, and attempts to understand the underlying factors responsible.

Graduation date: 2003

Nitrogen availability in agricultural soils from fertilizer, plant residue inputs, and soil organic matter has important implications beyond crop yield. Legume winter cover crops and one fourth the recommended N rate on sweet corn resulted in yields equivalent to those at the recommended rate in the Willamette Valley of western Oregon. Cereal rye winter crops absorbed an average of 40 kg N/ha that otherwise would have been leached, but did not effectively replace fertilizer N. Cereal rye as a cover crop therefore shows an ability to immobilize N from fertilizer. This was further confirmed in an experiment with "N labeled urea where results showed that N derived from fertilizer in sweet corn or cereal rye plant residue was less available for crop uptake and loss from the system than inorganic N or N directly immobilized from fertilizer. Losses of N from fertilizer ranged from 40 to 73% of that which was in the soil over winter. Mineralization of organic matter N is an important process in N availability, especially when cover crops are used to replace fertilizer. Finding a general indicator or predictor of N mineralization in soils would help in reducing fertilizer N costs and leaching of inorganic N that is applied in excess of crop needs. In a screening of 17 biological and chemical properties of 19 differently managed soils from around the state of Oregon, a model using total soil N and ��-glucosidase activity provided the best model of mineralized N uptake by ryegrass. Biological activity is primarily responsible for the transformations that result in N availability in soils. Management of soils directly impacts soil biology, and results from multivariate analyses of biological and chemical parameters in differently managed soils showed that disturbance creates an overriding common biochemical state in soils. Beyond disturbance, vegetation and the nature of organic inputs also impart recognizable multivariate patterns in soils managed differently. These results suggest that indicators independent of soil type may be used to discern effects of management on agricultural soils. / Graduation date: 1999

Although legumes have been widely studied for their nitrogen-fixing ability, it is uncertain to what extent legume cover crops achieve their nitrogen-fixing potential under the climatic conditions encountered in western Oregon. Furthermore, it is unknown what factors control the proportions of legume cover crop N that are either sequestered into soil organic matter, or that contribute to the N requirements of the following summer crop. Soil was sampled in mid-September 1997, after harvest of a summer broccoli crop, from plots located at the North Willamette Research and Extension Center, Aurora, Oregon. Soil was sampled from main plots that had been either winter cover cropped with red clover (LN��� and LN���) or fallowed during the winter period (FN��� and FN���), and specifically from sub-plots in which the following summer crop had received either zero (N���) or an intermediate (N���) rate of N fertilizer as urea. Levels of total organic carbon (TOC), total Kjeldahl nitrogen (TKN), and readily mineralizable C and N were measured in both whole soil samples and in different aggregate-size classes (<0.25, 0.25-0.5 0.5-1.0, 1.0-2.0, and 2-5mm) prepared by dry sieving the soil. Aggregate size-class distribution was not affected by the cover crop treatment. Although there was no significant effect of cover crop treatment on either TKN or TOC levels in whole soil samples, TOC levels were consistently higher in the small aggregate size-classes <1 mm of the fallow than the legume treatment. There was a significantly higher level of mineralizable C in the <0.25 mm size class of the legume than the fallow treatment. There was a trend for the level of mineralizable N to be greater in soil from the legume than the fallow treatment. However, N fertilizer had a significant positive effect on the level of readily mineralizable N in both fallow and legume cover-cropped treatments, it had a negative effect on TKN levels among all aggregate-size classes. There were differences in the levels of mineralizable N measured among the aggregate-size classes, and immobilization of N between 20 and 40 days of incubation also differed among the aggregate-size classes. / Graduation date: 1999

No description available.

Monoculture corn (Zea mays L.) production may result in increased soil degradation through intensive cultivation and N fertilizer use. Intercropping may reduce these negative effects. The objectives of the study were to examine at two sites the effects of monocropping and intercropping corn on soft physical and chemical properties. A sandy loam soil of the Chateaugay series and a sandy loam soft of St Dainase series were used in a field experiment for 1993 and 1994 growing seasons. Soil with corn monoculture planted at 60 and 90 cm row width had lower soil, organic matter than that under intercrops. Soil aggregate stability treatment effects varied with soil. Corn intercropped with perennial rye grass (Lolium perenne L.) showed the highest of aggregate stability. Similar trends were noted with wet-sieved aggregate diameters. Monoculture corn tended to produce higher soil bulk density than intercrops. There was some evidence of compaction after late seeding of intercrops. Monoculture corn resulted in more acidity and lower pH than corn with intercrops. Extractable P and K by Mehlich III were lower in monoculture corn than corn-soybean intercrops. Intercropping tended to reduce residual soil NO3 -- levels but this effect varied with depth. Single and broadcast N application resulted in higher N residues with corn planted at 75 cm row width than split and banded application. Intercropping tended to reduce soil degradation and pollution as measured by aggregate stability and NO3 -- residues.

Although the physiological nitrogen demand of the soil microbial biomass is a major determinant of N mineralization in forest soils, the exact nature of the relationship is unclear. This study investigated the relationships between a respiration-based indicator of microbial physiological N demand (NIR) and N availability in forest soils. NIR was found to correlate significantly with net mineralized N in the field and annual foliar litterfall N fluxes. In a laboratory incubation, NIR was shown to be sensitive to changes in soil available C and N pools. These results demonstrated that microbial physiological N demand is determined by relative availabilities of labile C and N, and that it is significantly related to N cycling in forest soils. Results from a seasonal study of a forested watershed suggest that nutrient availability determined tree production and soil C availability, which in turn determined microbial physiological N demand and nitrogen dynamics in the forest.

A two year study was conducted on the Macdonald Campus Farm on a 2.4 ha site of shallow St. Amble loamy sand cropped to corn (Zea mays L.). Three types of tillage practice (conventional tillage, reduced tillage, and no-till) were combined with 2 residue levels (with and without) in a randomized complete block design. The effect of these practices on NO 3--N distribution at 0--50 cm in the soil profile, and on plant N uptake were studied. Organic matter, pH, bulk density, and soil moisture contents were also monitored. Residues were found to have a greater influence on soil NO3--N transformations (mineralization and immobilization), than tillage. In July 1996 residues suppressed NO3--N levels in reduced tillage (RT), but increased NO3--N levels in conventional tillage (CT). Residues initially increased N03--N levels in no-till (NT), but a few weeks later caused a sharp decline in NO 3--N levels in NT. In August 1996, RT and NT treatments without residue were found to have much greater concentrations of NO 3--N than those with residue. The effect of N suppression caused by residues was observed in Spring 1996, July 1996, August 1996, and August 1997. Reduced tillage demonstrated less NO 3--N fluctuation than the other tillage treatments. Wheel tracked rows had up to 20 times more NO3--N at 0--15 cm than the non wheel tracked rows, caused by the uneven distribution of N fertilizer. However, high NO3--N levels in the wheel tracked rows decreased to levels comparable with those in non fertilized (non wheel track) rows at 50 cm. Corn yields were not affected by tillage or residue treatments, neither were they influenced by the percentage of tissue N content. (Abstract shortened by UMI.)

Thesis (Ph. D.)--University of Hawaii at Manoa, 1995. / Includes bibliographical references (leaves 130-136). / Microfiche. / xi, 136 leaves, bound 29 cm