LONG-TERM TRENDS IN TOTAL NITROGEN OF A VERTISOL SUBJECTED TO ZERO-TILLAGE, NITROGEN APPLICATION AND STUBBLE RETENTION

被引:36
作者
DALAL, RC
机构
[1] Queensland Wheat Research Institute, Toowoomba, QLD
来源
AUSTRALIAN JOURNAL OF SOIL RESEARCH | 1992年 / 30卷 / 02期
关键词
NITROGEN DECLINE; VERTISOL; ZERO-TILLAGE; RESIDUE RETENTION; CONSERVATION PRACTICES;
D O I
10.1071/SR9920223
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
The effects of conservation practices, zero-tillage and stubble retention, on long-term trends in total N (0-0.1 m depth) of a Vertisol used mainly for wheat cropping were studied in a semi-arid subtropical environment (28-degrees 12' S. and 152-degrees 06' E.) in Queensland. Trends in total N content of a Vertisol (65% clay, pH 7.2) were discerned during a 22-year period of management practices including: zero-tillage (ZT) and conventional tillage (CT); stubble retention (SR) and stubble burning (SB); and fertilizer N application of nil (N1), 23 kg N ha-1 yr-1 (N2) and 69 kg N ha-1 yr-1 (N3). Soil total N (0-0.1 m) declined under all treatments at an overall rate of 25 +/- 2 kg N ha-1 yr-1 although after 22 years soil under ZT, SR and N3 treatments still contained higher soil total N than under CT, SB and Nl treatments. Apparent fertilizer N recovery in the soil-plant system was poor (34-64%) under CTSB, CTSR and ZTSB and ZTSR treatments, because N removed by the wheat crop was equivalent to less than 20% of fertilizer N in the first 12 years of management practices, due mainly to disease. Deep leaching losses of NO3-N was the likely factor for poor recovery of N. The ZTSR treatment showed better apparent N recovery than the CTSB treatment, most likely due to greater immobilization of fertilizer N, more N uptake in grain due to additional available soil water and hence less leaching losses of NO3-N. Under the current cultural practices, soil total N (0-0.1 m) may decline further to reach a steady state (about 1000 kg N ha-1). However, the apparent N recovery in the soil-plant system can be increased by disease control (for example, resistant cultivars and winter-summer crop rotations) and optimum utilisation of soil water (opportunity cropping) to minimize NO3-N leaching losses and to maximise production of crop biomass.
引用
收藏
页码:223 / 231
页数:9
相关论文
共 23 条
[1]  
[Anonymous], NITROGEN AGR SOILS
[2]  
BARTHOLOMEW WV, 1960, 7TH T INT C SOIL SCI, V111, P471
[3]  
Blevins R. L., 1984, No-tillage agriculture. Principles and practices., P190
[4]   ORGANIC-MATTER AND MICROBIAL BIOMASS IN A VERTISOL AFTER 20-YR OF ZERO-TILLAGE [J].
DALAL, RC ;
HENDERSON, PA ;
GLASBY, JM .
SOIL BIOLOGY & BIOCHEMISTRY, 1991, 23 (05) :435-441
[5]   INCLUSION OF NITRATE AND NITRITE IN THE KJELDAHL NITROGEN DETERMINATION OF SOILS AND PLANT MATERIALS USING SODIUM THIOSULFATE [J].
DALAL, RC ;
SAHRAWAT, KL ;
MYERS, RJK .
COMMUNICATIONS IN SOIL SCIENCE AND PLANT ANALYSIS, 1984, 15 (12) :1453-1461
[7]   LONG-TERM TRENDS IN FERTILITY OF SOILS UNDER CONTINUOUS CULTIVATION AND CEREAL CROPPING IN SOUTHERN QUEENSLAND .5. RATE OF LOSS OF TOTAL NITROGEN FROM THE SOIL-PROFILE AND CHANGES IN CARBON - NITROGEN RATIOS [J].
DALAL, RC ;
MAYER, RJ .
AUSTRALIAN JOURNAL OF SOIL RESEARCH, 1986, 24 (04) :493-504
[9]  
DORAN JW, 1987, SSSA SPEC PUBL, V19, P53
[10]  
DRAPER N, 1966, APPLIED REGRESSION A