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Temporal changes in N₂O-losses from two arable soils
by
Heinemeyer, Otto
, Kaiser, Ernst-August
in
Agricultural soils
/ Agrology
/ Agronomy. Soil science and plant productions
/ Arable soils
/ Biological and medical sciences
/ Chemical, physicochemical, biochemical and biological properties
/ Fundamental and applied biological sciences. Psychology
/ Nitrous oxide
/ Organic matter
/ Organic soils
/ Physics, chemistry, biochemistry and biology of agricultural and forest soils
/ Sandy loam soils
/ Silty soils
/ Soil biochemistry
/ Soil microorganisms
/ Soil science
/ Soil water
1996
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Temporal changes in N₂O-losses from two arable soils
by
Heinemeyer, Otto
, Kaiser, Ernst-August
in
Agricultural soils
/ Agrology
/ Agronomy. Soil science and plant productions
/ Arable soils
/ Biological and medical sciences
/ Chemical, physicochemical, biochemical and biological properties
/ Fundamental and applied biological sciences. Psychology
/ Nitrous oxide
/ Organic matter
/ Organic soils
/ Physics, chemistry, biochemistry and biology of agricultural and forest soils
/ Sandy loam soils
/ Silty soils
/ Soil biochemistry
/ Soil microorganisms
/ Soil science
/ Soil water
1996
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Temporal changes in N₂O-losses from two arable soils
by
Heinemeyer, Otto
, Kaiser, Ernst-August
in
Agricultural soils
/ Agrology
/ Agronomy. Soil science and plant productions
/ Arable soils
/ Biological and medical sciences
/ Chemical, physicochemical, biochemical and biological properties
/ Fundamental and applied biological sciences. Psychology
/ Nitrous oxide
/ Organic matter
/ Organic soils
/ Physics, chemistry, biochemistry and biology of agricultural and forest soils
/ Sandy loam soils
/ Silty soils
/ Soil biochemistry
/ Soil microorganisms
/ Soil science
/ Soil water
1996
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Journal Article
Temporal changes in N₂O-losses from two arable soils
1996
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Overview
N₂O-loss rates from two soils were measured over a continuous observation period of 2 years. The two soils, differing in texture (sandy loam and silty loam), are frequently used for intensive crop production. Rates were estimated using a closed soil cover box technique. N₂O-losses obtained were scrutinised with physical, chemical and microbiological properties of the soils as well as with climatic data. Large temporal changes in N₂O-emission rates were found. The data were approximately log-normal distributed. In spring maximal values of 20 g N₂O-N ha⁻¹ d⁻¹ were observed. According to this observation, two situations associated with high flux rates could be distinguished; 1. N₂O- production by soil at spring thaw and 2. N₂O-production within one week after N-fertilizer application. For both soils equal N₂O-losses were found, which are adequate to 1 kg N₂O-N ha⁻¹ per year. From this data was calculated that N₂O-losses ranged from 0.8-1.5% of the applied fertilizer N.
Publisher
Kluwer Academic Publishers,Springer
Subject
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