The effect of urea and pig slurry fertilization on denitrification, direct nitrous oxide emission, volatile fatty acids, water-soluble carbon and anthrone-reactive carbon in maize-cropped soil from the Po plain (Modena, Italy)

被引:29
作者
Arcara, PG
Gamba, C
Bidini, D
Marchetti, R
机构
[1] Ist Sperimentale Studio Difesa Suolo, I-50121 Florence, Italy
[2] Ist Agron Bari, Sez Perifer Modena, I-41100 Modena, Italy
关键词
denitrification; direct nitrous oxide emission; pig slurry; urea; maize;
D O I
10.1007/s003740050552
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
The use of zootechnical slurries in agriculture can increase N losses as N2O by direct emission and by denitrification, The aim of this research was to determine the influence of pig slurry, as well as its combination with mineral N, on N2O emissions in the field and their relationships with some fractions of soil organic matter, with soil moisture and with rainfall, In spite of varying amounts of organic substance applied, the diverse agronomic treatments did not produce substantial differences in N losses due to denitrification. Wide variations between the slurry fertilized and the urea-fertilized plots were not found, whereas the combination of pig slurry with urea usually produced an increase both in N2O emissions due to denitrification and in direct N2O emissions (N losses corresponding to about 50% of those due to denitrification). The greatest losses of N2O-N occurred in the first month following fertilizer administration. N2O emissions due to denitrification were highest in the days immediately following the administration of fertilizers and lowest in a later period. N2O emissions due to nitrification occurred later. Therefore, N2O emission via nitrification differed from N2O losses via denitrification which, under optimal conditions, presented peaks of activity during the whole growth cycle. The N2O-N losses were highly influenced by physical parameters, particularly rain. An increase in micropore water creates conditions of scarce oxygenation or of anaerobiosis which influence oxidation-reduction processes and, at the same time, can limit the diffusion of bacteria-produced gas towards the soil surface.
引用
收藏
页码:270 / 276
页数:7
相关论文
共 33 条
[1]  
ARCARA PG, 1990, AGRONOMIA, V24, P19
[2]  
ARCARA PG, 1995, ATT CONV PANDA SOTT, V3, P155
[3]   ORGANIC-MATTER AVAILABILITY FOR DENITRIFICATION IN SOILS OF DIFFERENT TEXTURES AND DRAINAGE CLASSES [J].
BEAUCHAMP, EG ;
GALE, C ;
YEOMANS, JC .
COMMUNICATIONS IN SOIL SCIENCE AND PLANT ANALYSIS, 1980, 11 (12) :1221-1233
[4]   RELATIONSHIPS BETWEEN FIELD-MEASURED DENITRIFICATION LOSSES, CO2 FORMATION AND DIFFUSIONAL CONSTRAINTS [J].
BENCKISER, G .
SOIL BIOLOGY & BIOCHEMISTRY, 1994, 26 (07) :891-899
[5]  
BOUWMAN AF, 1990, SOILS AND THE GREENHOUSE EFFECT, P61
[6]  
BRINK RH, 1960, SOIL SCI, V169, P157
[7]   RELATIONSHIPS BETWEEN DENITRIFICATION CAPACITIES OF SOILS AND TOTAL, WATER-SOLUBLE AND READILY DECOMPOSABLE SOIL ORGANIC-MATTER [J].
BURFORD, JR ;
BREMNER, JM .
SOIL BIOLOGY & BIOCHEMISTRY, 1975, 7 (06) :389-394
[8]   DENITRIFICATION RATE RELATIONSHIPS WITH SOIL PARAMETERS IN THE FIELD [J].
BURTON, DL ;
BEAUCHAMP, EG .
COMMUNICATIONS IN SOIL SCIENCE AND PLANT ANALYSIS, 1985, 16 (05) :539-549
[9]   DENITRIFICATION IN AN ACID SOIL - EFFECTS OF SLURRY AND POTASSIUM-NITRATE ON THE EVOLUTION OF NITROUS-OXIDE AND ON NITRATE-REDUCING BACTERIA [J].
CHRISTENSEN, S .
SOIL BIOLOGY & BIOCHEMISTRY, 1985, 17 (06) :757-764
[10]   LOSS OF NITROGEN FROM SOIL DURING NITRIFICATION OF UREA [J].
CHRISTIANSON, CB ;
HEDLIN, RA ;
CHO, CM .
CANADIAN JOURNAL OF SOIL SCIENCE, 1979, 59 (02) :147-154