Fate of fertilizer nitrogen in a subarctic agricultural soil

Dissertation (Ph.D.) University of Alaska Fairbanks, 1988 A nitrogen balance approach was taken to determine the fate of fertilizer nitrogen in a subarctic agricultural soil. Urea and calcium nitrate fertilizers were compared in a three-year spring barley recrop field study. Methods of N application...

Full description

Bibliographic Details
Main Author: Knight, Charles Winsett
Other Authors: Sparrow, Stephen D.
Format: Doctoral or Postdoctoral Thesis
Language:unknown
Published: 1988
Subjects:
Online Access:http://hdl.handle.net/11122/9332
id ftunivalaska:oai:scholarworks.alaska.edu:11122/9332
record_format openpolar
spelling ftunivalaska:oai:scholarworks.alaska.edu:11122/9332 2023-05-15T18:28:20+02:00 Fate of fertilizer nitrogen in a subarctic agricultural soil Knight, Charles Winsett Sparrow, Stephen D. 1988 http://hdl.handle.net/11122/9332 unknown http://hdl.handle.net/11122/9332 Agronomy Dissertation phd 1988 ftunivalaska 2023-02-23T21:37:15Z Dissertation (Ph.D.) University of Alaska Fairbanks, 1988 A nitrogen balance approach was taken to determine the fate of fertilizer nitrogen in a subarctic agricultural soil. Urea and calcium nitrate fertilizers were compared in a three-year spring barley recrop field study. Methods of N application included incorporating the N fertilizer into the soil during spring tillage versus broadcasting it on the soil surface after planting. $\sp{15}$N labeled urea was applied on one-meter square subplots within the main fertilizer plots. Nitrogen transformations and movement were monitored with ammonia volatilization traps, suction cup lysimeters, deep soil cores, plant tissue samples, and grain samples. Environmental data including precipitation, soil temperatures and soil moisture tensions were collected. Fertilizer N loss by ammonia volatilization was negligible, amounting to only a few grams N/ha/day. Rate of urea hydrolysis was rapid in the cool soil and was not considered to be a limiting factor affecting N availability to the crop. There appeared to be a little nitrate leaching during the growing season, but some may have occurred between cropping seasons. Only 16 percent of the fertilizer N could not be detected when the crop was physiologically mature, and that loss was accredited mostly to denitrification. Fertilizer N use efficiency, determined by the Difference Method, was 73 and 60 percent for calcium nitrate and urea, respectively. When the crop was physiologically mature, average fertilizer N recovery rates determined by the Isotope Dilution Method were: 40 percent in the plants, 43 percent immobilized in the soil, 1 percent available in the soil, and 16 percent unrecovered. Barley yields were not significantly affected by N source, but plants took up more N where nitrate had been applied. Position of N placement had little effect on either N loss or barley yield, but the surface application of N resulted in delayed barley maturity when spring rains were deficient. Doctoral or Postdoctoral Thesis Subarctic Alaska University of Alaska: ScholarWorks@UA Fairbanks
institution Open Polar
collection University of Alaska: ScholarWorks@UA
op_collection_id ftunivalaska
language unknown
topic Agronomy
spellingShingle Agronomy
Knight, Charles Winsett
Fate of fertilizer nitrogen in a subarctic agricultural soil
topic_facet Agronomy
description Dissertation (Ph.D.) University of Alaska Fairbanks, 1988 A nitrogen balance approach was taken to determine the fate of fertilizer nitrogen in a subarctic agricultural soil. Urea and calcium nitrate fertilizers were compared in a three-year spring barley recrop field study. Methods of N application included incorporating the N fertilizer into the soil during spring tillage versus broadcasting it on the soil surface after planting. $\sp{15}$N labeled urea was applied on one-meter square subplots within the main fertilizer plots. Nitrogen transformations and movement were monitored with ammonia volatilization traps, suction cup lysimeters, deep soil cores, plant tissue samples, and grain samples. Environmental data including precipitation, soil temperatures and soil moisture tensions were collected. Fertilizer N loss by ammonia volatilization was negligible, amounting to only a few grams N/ha/day. Rate of urea hydrolysis was rapid in the cool soil and was not considered to be a limiting factor affecting N availability to the crop. There appeared to be a little nitrate leaching during the growing season, but some may have occurred between cropping seasons. Only 16 percent of the fertilizer N could not be detected when the crop was physiologically mature, and that loss was accredited mostly to denitrification. Fertilizer N use efficiency, determined by the Difference Method, was 73 and 60 percent for calcium nitrate and urea, respectively. When the crop was physiologically mature, average fertilizer N recovery rates determined by the Isotope Dilution Method were: 40 percent in the plants, 43 percent immobilized in the soil, 1 percent available in the soil, and 16 percent unrecovered. Barley yields were not significantly affected by N source, but plants took up more N where nitrate had been applied. Position of N placement had little effect on either N loss or barley yield, but the surface application of N resulted in delayed barley maturity when spring rains were deficient.
author2 Sparrow, Stephen D.
format Doctoral or Postdoctoral Thesis
author Knight, Charles Winsett
author_facet Knight, Charles Winsett
author_sort Knight, Charles Winsett
title Fate of fertilizer nitrogen in a subarctic agricultural soil
title_short Fate of fertilizer nitrogen in a subarctic agricultural soil
title_full Fate of fertilizer nitrogen in a subarctic agricultural soil
title_fullStr Fate of fertilizer nitrogen in a subarctic agricultural soil
title_full_unstemmed Fate of fertilizer nitrogen in a subarctic agricultural soil
title_sort fate of fertilizer nitrogen in a subarctic agricultural soil
publishDate 1988
url http://hdl.handle.net/11122/9332
geographic Fairbanks
geographic_facet Fairbanks
genre Subarctic
Alaska
genre_facet Subarctic
Alaska
op_relation http://hdl.handle.net/11122/9332
_version_ 1766210756428169216