Evaluation of Conservation Tillage System Performance for Rainfed Wheat Production in upland of Pakistan
Research Article
Evaluation of Conservation Tillage System Performance for Rainfed Wheat Production in upland of Pakistan
Muhammad Sharif1*, Shahzada Sohail Ijaz2, Muhammad Ansar3, Ijaz Ahmad4 and Syed Abdul Sadiq5
1Department of Soil Science,Balochistan Agriculture College, Quetta, Pakistan; 2Institute of Soil Science, PMAS-Arid Agriculture University Rawalpindi, Pakistan; 3Department of Agronomy, PMAS-Arid Agriculture University Rawalpindi, Pakistan; 4Ecotoxicology Research Institute, National Agriculture Research Centre, Islamabad, Pakistan; 5Department of Plant Breeding and Genetics, Balochistan Agriculture College, Quetta, Pakistan.
Abstract | Tillage and crop residue management practices are keyconsiderations for crop production in rainfed areas. The objective of the current study was to explorethe possibility of practicing conservation tillage systems for reducing input cost of small holder farming community of Pothwar, Pakistan. A two-year field study was carried out with a split plot design, having conventional tillage (CT), minimum tillage (MT), reduced tillage (RT) and zero tillage (ZT) systems in main plots,while residue retained (R+) and removed (R-)in sub-plots.The results showed that seedling emergence, wheat biomass and grain yield were statistically same under CT (83 plants m-2, 6.02 Mg ha-1, 3.32 Mg ha-1, respectively), MT (83 plants m-2, 5.90Mg ha-1, 3.26 Mg ha-1, respectively) and RT(72 plants m-2, 5.92 Mg ha-1,3.20Mg ha-1, respectively)tillage systemswith retention of crop residues,whilesignificantly lower values were recorded under ZT without residue return (54 plants m-2, 4.33Mg ha-1, 2.02Mg ha-1, respectively). The gross margins were highest with crop residue return under RT (Rs. 109375) followed by MT (Rs. 101800) and CT (Rs. 97840), whereas ZT without residue return gave the lowest gross margin of Rs. 7187.The study indicated that reduced tillage (chiseling) with retention of crop residue is a promising conservation tillage practicefor economical benefits and sufficient wheat yields in rainfed Pothwar, Pakistan.
Received | December 18, 2017; Accepted | January 15, 2018; Published | March 25, 2018
*Correspondence | Muhammad Sharif, Department of Soil Science, Balochistan Agriculture College, Quetta, Pakistan; Email: sharifbaloch84@yahoo.com
Citation | Sharif, M., S.S. Ijaz, M. Ansar, I. Ahmad and S.A. Sadiq. 2018. Evaluation of conservation tillage system performance for rainfed wheat production in upland of Pakistan. Pakistan Journal of Agricultural Research, 31(1): 37-44.
DOI | http://dx.doi.org/10.17582/journal.pjar/2018/31.1.37.44
Keywords | Minimum tillage, Reduced tillage, Zero tillage, Residue management, Grain yield, Gross margins
Introduction
Pothwar is the largest rainfed tract of northern Punjab, Pakistan, where fallow-wheat rotation is the most common practice on about 80% of the area (Razzaq et al., 2002). The six-month-fallow starts from the harvest of previous wheatinMay and continues till the seeding of next wheat crop in October. The rainfall is erratic, scanty and 70% of the rain is received during monsoon (fallow period) in the form of torrential rainstorms which not only lead to water losses but also the loss of soil through erosion.Current farmer’s practices during fallow period comprise of moldboard plowing followed by 8 -12 tillage operationswithtine cultivator for moisture conservation and weed control (Zahid et al., 1991; Ishaq et al., 2003). Low crop productivity is the common feature of the agriculture of area; however, there is great potential of increasing crop productivityif efficient use of resourcesand reduced input costs are ensured.
Conservation tillage system (minimum tillage, direct drilling, zero tillage etc) is being advocated worldwide for sustainable crop production which involves minimum soil disturbance and leaving crop residues on soil surface. The potential advantage of conservation tillage practices over conventional practices is due to leaving residue on soil surface that reduces erosion by providing barrier against rain-splash and runoff, reduces evaporation and increases infiltration (Franzluebbers, 2002). Crop residue also increases soil organic carbon that improves soil aggregation (Madari et al., 2005) soil water availability (Unger, 1994; Drury et al., 1999), number of biopores (Francis and Knight, 1993) that may facilitate root growth (Martino and Shaykewich, 1994) and water holding capacity. In short, conservation tillage with presence of residue on soil surface interfaces all soil ecology (Huang et al., 2008). This system also saves time and fuel cost (Baker et al., 2007) which is very important for small holder farmers of developing countries like Pakistan. However, the benefits of conservation tillage are dependent on soil properties, climatic condition of the area and the number of the years since the tillage system has been implemented (Rhoton, 2000).
Conservation tillage systems have been thoroughly studied under different ecologies (Fabrizzi et al., 2005) and worldover adopted on about 117 M ha. Out of total about 47% area is located in North America, 34% in South America and 14% in Australia. Ironically Asia has only 2.2% area under conservation tillage (ICARDA, 2012). The deficient research and development under developing countries including Pakistan demonstrate which is infact missed the opportunity. Therefore the currentstudy was conducted with the objective to evaluate different variants of conservation tillage with and without residue return in comparison withconventional intensive tillage system for crop production and economic returns for smallholder farmers of Pothwar, Pakistan.
Materials and Methods
Conservation tillage experiment was initiated in 2012 on a sandy clay loam soil at PMAS-Arid Agriculture University Research Farm Chakwal Road (latitude 33°36’0”N, longitude 73°02’0”E) in semi-arid dryland Pothwar, northern Punjab, Pakistan. The soil has sand 560 g kg-1, silt 190 g kg-1 and clay 250 g kg-1, pH around 7.85 and SOC 5.2 g kg-1. The climate of the experimental site is semi-arid, very hot in summer and low temperature in winter with 70% of the rain received during monsoon in the form of heavy showers.
Detail of treatments
The experiment was initiated on an area of 6000 m2 with treatments arranged in a split plot design having four replications. The main plot treatments were tillage systems i.e. Conventional Tillage (CT), Minimum Tillage (MT), Reduced Tillage (RT) and Zero Tillage (ZT). The sub plot-treatments involved residues retained (R+) and residues removed (R-). One year earlier than installation of treatments, the field was left without tillage and crop to offset the residual effects of previous tillage practices. In CT plots, the soil was ploughed with moldboard plow at the start of monsoon followed by 8-10 time shallow cultivation with tine cultivator applied after each major rainfall for weed control and moisture conservation. Wheat sowing in these plots was done with seed-cum-fertilizer drill. In MT, the field was also ploughed with intensive moldboard on the onset of monsoon and four time cultivation with tine cultivator, while sowing was done with conventional seed-cum-fertilizer drill. In RT, one time chisel plough was applied at the start of monsoon and then during fallow period weeds were controlled with roundup herbicide (Glyphosate @ 1 L acre-1) and wheat was sown through direct drilling with zero tillage drill. In ZT, field remained undisturbed for entire fallow period and weeds were controlled with roundup herbicide when needed. Winter wheat was directly sown with zero tillage drill. In sub-plot treatments +R involved just harvest of the previous crop spikes and retention of all the stubbles in field. In case of -R the crop was harvested with reaper and there was no crop residues left in field. The recommended doses of fertilizer NPK i.e. 100-60-30 in the form of urea, diamonium phosphate (DAP) and sulfate of potash (SOP) were used. Wheat was planted at seed rate of 100 kg ha-1.
The crop samples were collected by randomly casting the square quadrate of 1 m2 at three places in each replication of the treatments. For crop biomass plant samples were placed in oven, dry weighed was measured and for yield grains were separated from spikes and average grain yield was presented in Mg ha-1. Harvest index was calculated by dividing grain yield into total biomass and multiply by hundred.
The profitability of different tillage systems were measured by calculating gross margins and efficiency coefficients. The gross margin is gross income less the variable costs incurred in achieving that income. Variable costs were those which were directly attributable to the enterprise: e. g. tillage, weed control, seeding, fertilization and harvest operations. The gross margin was not equivalent to gross profit because it did not include fixed or overhead costs such as depreciation, interest payments or permanent labor, all of which had to be met regardless of enterprise size (Scott, 2001). All input costs and output prices used in the economic calculations were those recorded during the experiment in (Table 1). The efficiency coefficient was calculated by dividing gross income with the total variable cost incurred for achieving that income.
Table 1: Detail of inputs and outputs under different tillage treatments used for economic analyses.
Detail of Inputs and Outputs | 2012-13 | 2013-14 |
Inputs (Rs.)* | ||
M.B Plough /hr | 1200 | 1400 |
Roundup Spray /L) | 1050 | 110 |
Cultivator /hr | 1000 | 1200 |
Seed drill | 1200 | 1200 |
Fertilizer DAP/50 kg | 4500 | 4500 |
Fertilizer Urea /50 kg | 2000 | 2000 |
Seed /50 kg | 2500 | 2800 |
Fungicide /L | 600 | 700 |
Harvest /hr | 1800 | 2200 |
Threshing /hr | 2100 | 2400 |
Outputs (Rs.) | ||
Grain yield/40 kg | 1200 | 1200 |
Straw yield/40 kg | 320 |
350 |
*: Rs (Pakistani rupees) 1 US$ = 98 Rs
Metrological data and statistical analysis
Metrological data on temperature, rain fall during experimental year was collected from agro-metrological centre at Chakwal (Figure 1) and the data for statistically analysis was collected for various parameters was subjected to analysis of variance (ANOVA) under split-plot design and means was compared at 5% level of significance by Least Significance Difference (LSD) test (Steel et al., 1997).
Results and Discussion
Seedling emergence
Seedling emergence was significantly affected by different tillage systems with and without retention of crop residues. In both years the seedling emergence Figure 2a and b was significantly higher under CT followed by MT and RT with and without retention of crop residues. The seedling emergence was low under ZT in both years (56 and 54 plant m-2) without retention of crop residues as well as with retention of crop residues (58 and 56 plant m-2).
Seedling emergence is the important parameter for crop establishment and ultimately contributes to crop biomass and yield. The higher seedling emergence in tilled plots may be related to higher moisture storage during fallow period, reduction in bulk density and pulverized soil that provide a favorable condition for crop germination while in ZT plot there was a compacted layer on soil surface during crop sowing and establishment. (Chiroma et al., 2006; Thomas et al., 2007) reported improved seedling emergence due to adequate and proper water availability. There is dire need to improve germination under zero tillage treatments.
Crop biomass
Crop biomass in 2012-13 was numerically higher under CT 6.02 Mg h-1 followed by MT 5.92 Mg h-1 and RT 5.9 Mg h-1 with retention of crop residues while lower values were observed under ZT 4.33 Mg h-1 without retention of crop residues (Figure 3a). The same trend was also observed during the year 2013-14 (Figure 3b), that wheat crop biomass was significantly higher under CT with retention of crop residues. In both experimental years the trend under different tillage systems was CT> MT>RT>ZT with and without retention of crop residues. The retention of crop residues also helped to increase biomass than without retention of crop residues under different tillage systems.
The better biomass yield during both years under CT is due to higher water content at wheat sowing and loosening of surface soil due to intensive ploughing that resulted in better seed-soil contact and hence germination. The intensive ploughing also loosened the soil which may have helped the roots to penetrate deeper and extract more water and nutrients. (Gill et al., 2000) also conducted a tillage experiment in same region and concluded that mouldboard plough loosen the soil which help to increase crop biomass. The ZT plots had lower water content as well as a relatively compact surface layer that not only reduced seed germination but also hindered root penetration at initial crop stages.
Grain yield
Wheat grain yield was also significantly affected by different tillage systems with and without retention of crop residues. In 2012-13 grain yield was significantly higher under CT 3.26 Mg h-1 followed by MT 3.21 Mg h-1 and RT 3.12 Mg h-1 then by ZT 2.58 Mg h-1 with retention of crop residues (Figure 4a). Lower values were observed under ZT 2.46 Mg h-1without retention of crop residues. The same tendency during 2013-14 (Figure 3b) was also noted i.e. CT>MT>RT>ZT. The yield was low under ZT without retention of crop residues. In all tillage systems retention of crop residues showed pronounced effect on grain yield than no residue especially in CT, MT and RT plots.
In CT, MT and RT plots the higher grain yield was also due to higher water infiltration, enough residual moisture stored during fallow period, seed bed preparation which reduced bulk density and provided better condition for initial crop germination and development that led to establishment of a bumper crop and ultimately increased crop yield. Also in RT plots the higher grain yield may be attributed to breaking of sub-surface hard pan by chisel plough which enhanced higher water penetration in lower depth during fallow period that encouraged root development and thus helped for better crop establishment. In ZT plots the lower grain yield was related to inferior crop establishment due to poor initial crop germination. Theretention of crop residues also showed promising effect to increased wheat yield than without retention of crop residues. The decrease of crop yield in ZT plots may be related to delay in initial crop germination. In ZT plots there was surface compacted layer that may had affected the crop germination and establishment which ultimately decreased crop yield. (Radford et al, 2001; Gemtos and Lellis, 1997) also reported that late germination decreased crop yield. The compacted top layer also restricts root development (Whalley et al., 1995).
Harvest index
Harvest index was also affected by different tillage systems with and without retention of crop residues during first experimental year. The harvest index value was statistically similar under CT, MT and RT with retention of crop residues but low under ZT without residue retention. In 2nd experimental years during 2013-14 the trend remained sameunder different tillage system (Figure 5b). The HI was higher without retention of crop residues.
The HI was low under ZT with and without retention of crop residues. Luver (2007) founded no significant effect of different tillage systems on harvest index. (Ahadiyat and Ranamukhaarachchi, 2008) observed that harvest index was higher under conventional tillage than conservation tillage systems.
Gross margin and efficiency coefficient
The result of gross marginal return illustrate that during 2012-13 highest GM return was recorded under RT (Rs. 109375) followed by MT (Rs. 101800) and CT (Rs. 97840) with retention of crop residues while least GM was recorded under ZT (Rs. 44975) without retention of crop residues (Figure 6a). The trend remained same during 2013-14 in 2nd experimental year where RT (Rs. 100380) remained higher followed by MT (Rs. 89590) and CT (Rs. 81990) Figure 5b. The lower amounts of GM (Rs. 41400) were observed under ZT.
In order to decide on tillage systems with best economic return per investment, efficiency coefficients were calculated. The efficiency coefficients during 2012-13 were 4.24 for ZT followed by RT (4.13) and MT (3.55) with retention of crop residues while lower under CT (1.76) without retention of crop residues (Figure 7a). The same trend was also observed during 2013-14 i.e. higher under ZT (3.57), RT (3.45) without retention of crop residues and lower under CT (1.75) with retention of crop residues (Figure 6b).
The higher gross marginal return and efficiency coefficient under RT demonstrated that reduced tillage
perform better economic in comparison with other tillage systems. (Ahmad et al., 2007) in the same region reported that conservation tillage was found to be economically beneficial compared to conventional tillage by reducing input cost. In Pakistan and India at rice-wheat system (Hobbs and Gupta, 2004) reported that zero tillage reduces the cost of production up to $ 60 mostly due to decreasing fuel cost by 60-80 L per hectare and labor cost. (Jin et al.,2007) have also observed that conservation tillage is economically beneficial.
Conclusions
From the two year field investigation our results confirmed that reduced tillage (chiseling) withretention of crop residue might enhance crop yield while conventional tillage system through moldboard plough without retention of crop residues increases input cost. We conclude that conservation tillage practices especially the reduced tillage (chiseling) with retention of crop residues has potential to improve soil quality and economic benefits for farmers while providing sufficient crop yield in rainfed upland of Pakistan.
Author’s Contribution
Muhammad Sharif conducted the research and wrote teh article. Shahzada Sohail Ijaz, Muhammad Ansar, Ijaz Ahmad and Syed Abdul Sadiq reviewed the article and gave uselful suggestion on editing and improvement of the artice.
References
Ahadiyat, Y.R. and Ranamukhaarachchi, S.L. 2008. Effects of tillage and intercropping with grass on soil properties and yield of rainfed maize. Int. J. Agric. Biol. 10(1): 133-139.
Ahmed, M.S., Ashraf, M. and Gill, M.A. 2007. Partial budgeting of different sowing technologies of wheat. Sarhad J. Agric. 23(1): 4-15.
Baker, C.J. 2007. No-tillage seeding in conservation agriculture. Food and Agriculture Organization of the United Nations and CAB International, Oxford. pp. 326.
Chiroma, A. M., Folorunso, O.A. and Alhassan, A.B. 2006. The effects of land configuration and wood-shavings mulch on the properties of a sandy loam soil in northeast Nigeria. Tropicultura. 24(3): 33-38.
Drury, C.F., Tan, C., Welacky, T.W., Olaya, T.O., Hamill, A.S. and Weaver, S.E. 1999. Red clover and tillage influence on soil temperature, water content, and corn emergence. Agron. J. 91(2): 101–108. https://doi.org/10.2134/agronj1999.00021962009100010016x
Fabrizzi, K.P., Garcia, F.O., Costa, J.L. and Picone, L.I. 2005. Soil water dynamics, physical properties and corn and wheat responses to minimum and no-tillage systems in the southern Pampas of Argentina. Soil Till. Res. 81(2): 57-69. https://doi.org/10.1016/j.still.2004.05.001
Francis, G.S. and Knight, T.L. 1993. Long-term effects of conventional and no-tillage on selected soil properties and crop yields in Canterbury, New Zealand. Soil Till Res. 26(3): 193–210. https://doi.org/10.1016/0167-1987(93)90044-P
Franzluebbers, A.J. and J.A. Stuedemann. 2002. Particulate and non-particulate fractions of soil organic carbon under pastures in the Southern Piedmont USA. Environ. Pollut., 116: 53-62.
Gemtos, T.A. and Lellis, T. 1997. Effects of soil compaction, water and organic matter contents on emergence and initial plant growth and sugar beet. J. Agric. Eng. Res. 66(1): 121–134. https://doi.org/10.1006/jaer.1996.0126
Gill, S.M., Akhtar, M.S. and Saeed, Z. 2000. Soil water use and bulk density as affected by tillage and fertilizer in rainfed wheat production system. Pak. J. Biol. Sci. 8(1): 223-226.
Hobbs, P.R. and Gupta, R.K. 2004. Problems and challenges of no-till farming for the rice-wheat systems of the indo-gangetic plains in South Asia. In: D. O. Hansen, N. Uphoff, P. R. Hobbs and R. Lal (eds). Sustainable Agriculture and the Rice-Wheat System. CRC press Boca Raton. pp.101-120. https://doi.org/10.1201/9780203026472.ch6
Huang, G.B., Zhang, R.Z., L.i G.D., Chan, K.Y., Heenan, D.P., Chen, W., Unkovich, M.J., Robertson, M.J. and Cullis, B.R . 2008. Productivity and sustainability of a spring wheat -field pea rotation in a semi-arid environment underconventional and conservation tillage systems. Field Crops Res. 107(1): 43-55. https://doi.org/10.1016/j.fcr.2007.12.011
ICARDA (International Center for Agricultural Research in the Dry Areas). 2012. Conservation agriculture: Opportunities for intensified farming and environmental conservation in dry areas research to action 2. ICARDA, Aleppo, Syria.
Ishaq, M. Ibrahim, M. and Lal, R. 2003. Persistance of subsoil compaction effects on soil properties and growth of wheat and cotton in Pakistan. Exptl. Agric. 39(1): 341-347. https://doi.org/10.1017/S0014479703001340
Jin, H., Li, H., Wang, X., Mchugh, A.D., Li, W., Gao, H. and N.J. Kuhn. 2007. The adoption of annual subsoiling as conservation tillage in dryland maize and wheat cultivation in northern Chinau. Soil Till. Res. 94(3): 493–502. https://doi.org/10.1016/j.still.2006.10.005
Luver, L.K., D.A. Horneck, D.J. Wysocki, J.M., Hart, S.E. Petrie and N.W. Christensen. 2007. Winter wheat in summer-fallow systems-intermediate precipitation zone. Oregon State University Fertilizer Guide G80-E. http://ir.library.oregonstate.edu/xmlui/bitstream/handle/1957/20640/fg82.pdf
Madari, B.P., Machado, L.O., Torres, E., Andrade, A.G. and Valencia, L.O. 2005. No tillage and crop rotation effects on soil aggregation and organic carbon in a Rhodic Ferralsol from southern Brazil. Soil Till. Res. 80(2): 185-200. https://doi.org/10.1016/j.still.2004.03.006
Martino, D.L. and Shaykewich, C.F. 1994. Root penetration profiles of wheat and barley as affected by soil penetration resistance in field conditions. Can. J. Soil Sci. 74(1):193–200. https://doi.org/10.4141/cjss94-027
Radford, B.J., Yule,D.F., McGarry, D. and Playford, C. 2001. Crop responses to applied soil compaction and to compaction repair treatments. Soil Till. Res. 61(2): 157–166. https://doi.org/10.1016/S0167-1987(01)00194-5
Razzaq, A., Munir, M., Hashmi, N.I., Hobbs, P.R. and Majid, A. 2002. Current management practices for wheat production in rainfed agro-ecological zone in northern Punjab. Pak. J. Agric. Res. 17(2): 201-205.
Rhoton, F.E. 2000. Influence of time on soil response to no-till practices. Soil Sci. Soc. Am. J. 64(1): 700–709. https://doi.org/10.2136/sssaj2000.642700x
Scott, F. 2001. Farm Budget handbook 2001: Northern NSW. Winter Crops, NSW Agriculture, Australia. p. 76.
Steel, R.G.D., J.H. Torrie and M.A. Boston. 1997. Principles and procedure of statistics: A biometrical approach. McGraw Hill Inc. New York. P. 633.
Thomas, G.A., G.W. Titmarsh, D.M. Freebairn and B.J. Radford. 2007. No-tillage and conservation farming practices in grain growing areas of Queensland – a review of 40 years of development. Aust. J. Exp. Agric., 47(2): 887–898. https://doi.org/10.1071/EA06204
Unger, P.W. 1994. Impacts of tillage practices on water-use efficiency.White Paper Farming for a Better Environment. J. Soil Water Conserv. 24(2): 20-28.
Whalley, W.R., Dumitru, E. and Dexter, A.R. 1995. Biological effects of soil compaction. Soil Till. Res. 35(2): 53–68. https://doi.org/10.1016/0167-1987(95)00473-6
Zahid, M.S., Khan, M.A., Razzaq, H.R. and Majid, A. 1991. Cropping systems intervention in the FSR target area Fatehjang (Pakistan). J. Agric. Plant Sci. 12 (1):99-102.
To share on other social networks, click on any share button. What are these?