1994
DOI: 10.1097/00010694-199408000-00004
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The Effect of Different Moisture Regimes and Soil Characteristics on Nitrous Oxide Emission and Consumption by Different Soils

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Cited by 84 publications
(42 citation statements)
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“…The amount of N 2 0-N produced from soil No.1 was two to three orders greater than that reported previously (Martikainen and De Boer 1993;Bandibas et al 1994). We added 15N-labeled NH4 + and N0 3 -to soil No.1 to ensure that N 2 0 was actually produced and to determine whether or not N2 was produced from soil No.1.…”
Section: Nitrous Oxide Production From Tea Field Soilcontrasting
confidence: 55%
See 1 more Smart Citation
“…The amount of N 2 0-N produced from soil No.1 was two to three orders greater than that reported previously (Martikainen and De Boer 1993;Bandibas et al 1994). We added 15N-labeled NH4 + and N0 3 -to soil No.1 to ensure that N 2 0 was actually produced and to determine whether or not N2 was produced from soil No.1.…”
Section: Nitrous Oxide Production From Tea Field Soilcontrasting
confidence: 55%
“…They suggested that tea field soil has specific microflora. N 2 0 production from acid soils has been found in coniferous forest soil (Martikainen and De Boer 1993), coastal plain soil (Weier and Gilliam 1986), and other soils (Bandibas et al 1994), but there are few reports on N 2 0 production from strongly acid tea field soil.…”
mentioning
confidence: 99%
“…The production of N 2 O in soils is affected by the presence of readily-available C fractions such as water-soluble organic C (Burford and Bremner, 1975), oxygen availability (Linn and Doran,1984), temperature (Saad and Conrad, 1993), pH (Bandibas et al, 1994), and the supply of ammonium and nitrate (Firestone and Davidson, 1989;Smith et al 1997). As a result, it is easy to understand that any agricultural practice that causes changes in the soil N substrates or soil environmental conditions can lead to important variations in soil N 2 O production.…”
Section: Introductionmentioning
confidence: 99%
“…Saitama 3 soil showed the highest potential (1.463 J1.g N 2 0-N g-l d-1 ) and Kumamoto 1 soil showed the lowest potential (0.001 J1.g N 2 0-N g-l d-1 ) among all the soil samples. The rates of N 2 0 production from soil under aerobic conditions reported previously were 3.5 ng N 2 0-N g-l d-1 for a loamy soil at pH 6.3 (Klemedtsson et al 1988), 72 ng N 2 0-N g-l d-1 for a podzolized forest soil at pH 3.7 (Martikainen and De Boer 1993), and 1.016 J1.g N 2 0-N g-l d-1 for a heavy clay soil at pH 6.3 (Bandibas et al 1994). The potential of the Saitama 3 soil was higher than the values previously reported.…”
Section: Resultsmentioning
confidence: 58%
“…Several studies have been carried out on N 2 0 production from soils that originally showed various pH values. Bandibas et al (1994) reported the results of a laboratory experiment showing that the N 2 0 emission rate from soils under field water holding capacity was correlated positively with the soil pH. Yamulki et al (1997), using a grassland soil core in a laboratory experiment, reported that the N 2 0 flux from neutral soil (pH 7.6) was significantly higher than that from acidic soil (pH 3.9).…”
Section: Resultsmentioning
confidence: 99%