Liming and re-liming needs of acidic soils used for crop - pasture rotations

1997 ◽  
Vol 37 (5) ◽  
pp. 577 ◽  
Author(s):  
W. J. Slattery ◽  
G. W. Ganning ◽  
V. F. Burnett ◽  
D. R. Coventry

Summary. In a long-term liming experiment in north-eastern Victoria, we have re-applied lime and applied gypsum (1992 season) to assess wheat grain yield responses with on-going changes in soil pH and extractable aluminium. An acid-sensitive wheat (cv. Oxley) was grown in 2 seasons (1992–93), 12 years after initial applications of lime. Where lime (2.5 t/ha) was applied in 1992 to a previously unlimed soil, grain yield was increased by 19 and 46% respectively in the 2 seasons. However, the yield from these newly limed plots was well below the yields obtained from plots limed in 1980. Re-liming plots limed in 1980 resulted in further yield increases, with lime re-applied at 2.5 t/ha increasing yields by 12% in both seasons. Gypsum decreased grain yields on unlimed soil in the year of application but in the second year gave increases in yield. Whilst pH had changed little in the unlimed soil over the 12 years, the concentrations of extractable aluminium in the root zone increased substantially such that these concentrations far exceed levels which may affect acid-sensitive wheats. Liming at 2.5 t/ha did reduce the aluminium at 0–10 cm depth, but the concentrations at 10–20 cm depth (11.7 mg/kg) are likely to restrict grain yield. The data illustrate the progressive nature of soil acidification and the risk to wheat productivity through delaying treating this soil degradation problem.

2019 ◽  
Vol 236 ◽  
pp. 42-57 ◽  
Author(s):  
Romulo P. Lollato ◽  
Bruno M. Figueiredo ◽  
Jagmandeep S. Dhillon ◽  
Daryl B. Arnall ◽  
William R. Raun

2009 ◽  
Vol 60 (6) ◽  
pp. 566 ◽  
Author(s):  
R. F. Brennan ◽  
M. D. A. Bolland

Canola (oilseed rape, Brassica napus L.) is now grown in rotation with spring wheat (Triticum aestivum L.) on the predominantly sandy soils of south-western Australia. For both crop species, fertiliser nitrogen (N) and phosphorus (P) need to be applied for profitable grain production. The fertiliser N requirements have been determined separately for canola or wheat when adequate P was applied. By contrast, the fertiliser P requirements of the 2 species have been compared in the same experiment when adequate N was applied and showed that canola consistently required ~25–60% less P than wheat to produce 90% of the maximum grain yield. We report results of a field experiment conducted at 7 sites from 2000 to 2003 in the region to compare grain yield responses of canola and wheat to application of N and P in the same experiment. Four levels of N (0–138 kg N/ha as urea [46% N]) and 6 levels of P (0–40 kg P/ha as superphosphate [9.1%P]) were applied. Significant grain yield responses to applied N and P occurred for both crop species at all sites of the experiment, and the N × P interaction for grain production was always significant. To produce 90% of the maximum grain yield, canola required ~40% more N (range 16–75%) than wheat, and ~25% less P (range 12–43%) than wheat. For both crop species at 7 sites, applying increasing levels of N had no significant effect on the level of P required for 90% of maximum grain yield, although at 1 site the level of P required to achieve the target yield for both crop species when no N was applied (nil-N treatment) was significantly lower than for the other 3 treatments treated with N. For both crop species at all 7 sites, applying increasing levels of P increased the level of N required for 90% of the maximum grain yield. Fertiliser P had no significant effect on protein concentration in canola and wheat grain, and oil concentration in canola grain. As found in previous studies, application of increasing levels of N decreased oil concentration while increasing protein concentration in canola grain, and increased protein concentration in wheat grain. The N × P interaction was not significant for protein or oil concentration in grain. Protein concentrations in canola grain were about double those found in wheat grain.


2013 ◽  
Vol 105 (5) ◽  
pp. 1317-1327 ◽  
Author(s):  
Gaetano Amato ◽  
Paolo Ruisi ◽  
Alfonso S. Frenda ◽  
Giuseppe Di Miceli ◽  
Sergio Saia ◽  
...  

2009 ◽  
Vol 60 (3) ◽  
pp. 218 ◽  
Author(s):  
David W. Lester ◽  
Colin J. Birch ◽  
Chris W. Dowling

Within north-eastern Australia’s grain-production region there are few reports outlining nitrogen (N) and phosphorus (P) fertiliser effects on grain P concentration and P removal in grain. Two long-term N × P fertiliser experiments with different cultivation durations were conducted, one at ‘Colonsay’ on the Darling Downs in southern Queensland (commencing 1985 after 40 years of cultivation), and the other at ‘Myling’ on the north-west plains of New South Wales (commencing 1996 after 9 years of cultivation). Applications of N and P fertiliser independently influenced both grain P concentration and P removal for a range of summer and winter cereal and legume crops. Generally, if N fertiliser application increased grain yield, the grain P concentration decreased as grain yield increased; however, if grain yield did not respond to N fertiliser, grain P concentration was unaffected. P fertiliser applications typically increased grain P concentration. Wheat and barley grain P concentrations were generally higher in this subtropical region than reported values from temperate regions in Australia. Grain sorghum values were similar to those from subtropical areas overseas, but were greater than reported values from more tropical production zones. Mungbean and chickpea grain P concentrations were consistent with other reported values. Experimental results indicated grain P concentrations for estimating grain P removal in the northern grains region of 3400 mg/kg for sorghum, 3500 mg/kg for wheat and barley, and 4000–4500 mg/kg for mungbean. At both sites, grain P removal was greater with summer and winter cereals than with legume crops. Larger grain yields with N fertiliser application had the largest influence on grain P removal at the Colonsay site, with an additional 23.3 kg P/ha removed from plots with 80 kg N/ha applied compared with nil N over 5 analysed crops from 1998 to 2003. Grain P removal was 20.9, 17.1, and 19.7 kg P/ha in the 3 sorghum crops at this site in this period. Thus, application of P at 10 kg P/ha.crop for this 5-crop study period did not replace P removed. In the predominantly winter-cropped Myling experiment with a shorter duration of cultivation and smaller N fertiliser response, cumulative removal was more influenced by P fertiliser, with 10 kg fertiliser P/ha.crop generally sufficient to provide replacement P. These results support findings of negative P balances recently reported for grain production in this region and suggest a need for further investigation into the implications of a continuing negative P balance on the sustainability of grain production.


Geoderma ◽  
2012 ◽  
Vol 189-190 ◽  
pp. 442-450 ◽  
Author(s):  
Shengli Guo ◽  
Hanhua Zhu ◽  
Tinghui Dang ◽  
Jinshui Wu ◽  
Wenzhao Liu ◽  
...  

2011 ◽  
Vol 91 (3) ◽  
pp. 467-483 ◽  
Author(s):  
C. A. Campbell ◽  
G. P. Lafond ◽  
A. J. Vandenbygaart ◽  
R. P. Zentner ◽  
R. Lemke ◽  
...  

1997 ◽  
Vol 77 (4) ◽  
pp. 553-563 ◽  
Author(s):  
C. M. Monreal ◽  
R. P. Zentner ◽  
J. A. Robertson

We examined the influence of management on soil organic matter (SOM) dynamics and yield of wheat grain in semiarid Chernozemic and humid Gray Luvisolic soils. The Century model was tested with data obtained from long-term research plots cropped to wheat (Triticum aestivum L.) monoculture and cereal-hay (CH). Century simulated changes in soil organic-C (OC) and organic-N (ON) within 10% of actual measurements taken over decades. Our analysis indicated that management and soil erosion affected the time required for SOM to achieve new steady-state level (Tst). Tst ranged between 12 yr under wheat and 46 yr under CH cropping. Increasing the SOM content of degraded soils to new steady-state level appears to increase grain yield between 86 kg ha−1 and 840 kg ha−1.Wheat-fallow (WF) rotation plots receiving <10 kg N ha−1 yr−1, and with erosion >13.6 t ha−1 yr−1 degraded SOM. The average long-term yield of wheat grain (including new high yielding varieties) was maintained at <910 kg ha−1 yr−1 under degraded SOM content. Well-fertilized continuous wheat (CW) and CH rotation plots with erosion <4 t ha−1 yr−1 aggraded SOM content, and maintained the long-term average grain yield at >1290 kg ha−1 yr−1. Sustained OC levels were attained by returning 1030 kg C ha−1 yr−1 as plant residue (roots + aboveground) and keeping soil erosion ≤12.8 t ha−1 yr−1. Sustainable crop production systems need to consider SOM dynamics and erosion as factors limiting grain yield even after introducing genetically improved wheat varieties. Key words: Management, organic matter, erosion, dynamics, yield, manure, nitrogen, tillage, steady-state


Sign in / Sign up

Export Citation Format

Share Document