Increasing organic C and N in soil under bromegrass with long-term N fertilization

被引:32
作者
Malhi, SS
Nyborg, M
Harapiak, JT
Heier, K
Flore, NA
机构
[1] Agriculture and Agri-Food Canada,Department of Renewable Resources
[2] University of Alberta,undefined
[3] Western Co-operative Fertilizers Limited,undefined
关键词
carbon sequestration; grassland;
D O I
10.1023/A:1009727530325
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Two field experiments were conducted on bromegrass (Bromus inermis Leyss.) on a thin Black Chernozem (Typic Boroll) at Crossfield, Alberto, Canada to determine the long-term effects of N fertilization on changes in concentration and mass of organic C and N in soil. In both experiments, bromegrass was harvested for hay each year. In the experiment where ammonium nitrate (AN) was applied annually at 0 to 336 kg N/ha for 27 consecutive years from 1968 to 1994, the concentration of total C in the 0-5 cm soil layer increased from 50.33 g/kg in the zero-N treatment to 61.64 g/kg with 56 kg N/ha and to 64.15 g/kg with the 112 kg N/ha rate. Total C in soil also increased in the 5-10, 10-15 and 15-30 cm layers but to a lesser extent. The mass of total C in the 0-30 cm soil layer was increased by 18.46 Mg/ha with 56 kg N/ha and by 23.38 Mg/ha with the 112 kg N/ha rate as compared to the zero-N treatment. Total N in soil followed a similar trend as total C. In the experiment which received four N sources [ammonium nitrate (AN), urea, calcium nitrate (CN) and ammonium sulphate (AS)] applied annually at 168 and 336 kg N/ha for 15 years from 1979 to 1993, the total C in soil was greater where N fertilizer was applied, but the increase in total C varied with N source. The concentration of total C in soil in the 0-5 cm layer tended to be greater with AN and AS than with CN, with the smallest increase from urea. The mass of total C in soil (average of four N sources) at the 168 kg N/ha rate was increased by 18.98 Mg/ha in 0-30 cm and by 43.48 Mg/ha in the 0-60 cm layer as compared to the check treatment. The concentration of total C in soil also increased in the deeper layers to a depth of 60 cm, but the increases were much smaller than in the 0-5 cm layer. The changes in total N in soil followed a similar pattern as total C. In conclusion, long-term annual additions of fertilizer N to bromegrass resulted in a marked increase in total C and N in soil and the increases were influenced by both rate and source of N fertilizer. The implications of these results are that grasslands can be managed to lessen the increase in atmospheric CO2 concentration, while also improving fertility (N-supplying capacity) and tilth of soil.
引用
收藏
页码:255 / 260
页数:6
相关论文
共 16 条
[1]  
BALL DF, 1964, CAN J SOIL SCI, V15, P89
[2]   EFFECT OF CROP ROTATIONS AND CULTURAL-PRACTICES ON SOIL ORGANIC-MATTER, MICROBIAL BIOMASS AND RESPIRATION IN A THIN BLACK CHERNOZEM [J].
CAMPBELL, CA ;
BIEDERBECK, VO ;
ZENTNER, RP ;
LAFOND, GP .
CANADIAN JOURNAL OF SOIL SCIENCE, 1991, 71 (03) :363-376
[3]   DRY-MATTER YIELD AND NITROGEN RECOVERY FROM BROMEGRASS IN SOUTH-CENTRAL ALBERTA AS AFFECTED BY RATE OF LONG-TERM NITROGEN APPLICATIONS [J].
HARAPIAK, JT ;
MALHI, SS ;
NYBORG, M ;
FLORE, NA .
COMMUNICATIONS IN SOIL SCIENCE AND PLANT ANALYSIS, 1992, 23 (11-12) :1245-1256
[5]   YIELD AND N UPTAKE BY 7 PERENNIAL GRASS SPECIES AS AFFECTED BY HIGH-RATES OF N FERTILIZER [J].
LUTWICK, LE ;
SMITH, AD .
JOURNAL OF RANGE MANAGEMENT, 1979, 32 (06) :433-436
[6]  
MALHI SS, 1991, DEV PLANT SOIL SCI, V45, P547
[7]   EFFECTS OF NITROGEN APPLICATION ON YIELD AND QUALITY OF BROMEGRASS HAY IN CENTRAL ALBERTA [J].
MALHI, SS ;
MCBEATH, DK ;
BARON, VS .
CANADIAN JOURNAL OF PLANT SCIENCE, 1986, 66 (03) :609-616
[8]   LONG-TERM N FERTILIZATION OF A SOLONETZIC SOIL - EFFECTS ON CHEMICAL AND BIOLOGICAL PROPERTIES [J].
MCANDREW, DW ;
MALHI, SS .
SOIL BIOLOGY & BIOCHEMISTRY, 1992, 24 (07) :619-623
[9]   DYNAMICS OF SOIL MICROBIAL BIOMASS AND WATER-SOLUBLE ORGANIC C IN BRETON L AFTER 50 YEARS OF CROPPING TO 2 ROTATIONS [J].
MCGILL, WB ;
CANNON, KR ;
ROBERTSON, JA ;
COOK, FD .
CANADIAN JOURNAL OF SOIL SCIENCE, 1986, 66 (01) :1-19
[10]  
MCGILL WB, 1988, CAN SOC SOIL SCI CAN