NITROGEN UPTAKE OF SRI PADDY FIELD COMPARE TO CONVENTIONAL FIELD
DOI:
https://doi.org/10.11113/jt.v78.7259Keywords:
System of Rice Intensification (SRI), nitrogen uptake, biochar applicationAbstract
The aim of this research is to compare nitrogen uptake in SRI field and conventional paddy field. Three SRI plots and three conventional plots were given same amount of organic fertilizer and three different biochar amount. In SRI field, S1 were plot with 5 ton/ha biochar application, S2 were plot with 10 ton/ha biochar application, and S3 were plot with 20 ton/ha biochar application. Similarly, in conventional paddy field, K1, K2, and K3 were plots with 5 ton/ha, 10 ton/ha, and 20 ton/ha biochar application. Mineral fertilizer were not used in this research. Result shows that, Nitrogen uptake in SRI paddy field (average of 262.9 mg/g Dry mass) were less than Conventional paddy field (average of 323.8 mg/g Dry mass). However, average of the grain weight of 1000 paddy grain shows that grain from SRI field is heavier (average of 20.7Â g) than conventional paddy field (average of 19.0 g). Biochar application of 5 ton/ha, for both SRI and conventional fields shows higher result in most of plant parameters (plant height, amount of grain, total weight). SRI method usually shows the high production compare to conventional method. However, in this experiment there is almost no difference in SRI field (3.6 ton/ha) and conventional field (3.7 ton/ha). Plant observation shows that SRI paddy develop good rooting system than conventional paddy field that implies on more nutrient uptake. Soil were suspected to be the cause of low nitrogen uptake in SRI field.
References
L. W. Limei Zhao. 2010. Comparisons of Yield, Water Use Efficiency, and Soil Microbial Biomass as Affected by the System of Rice Intensification. Commun. Soil Sci. Plant Anal. 41(1): 1-12.
A. Dobermann. 2004. A Critical Assessment of the System of Rice Intensification (SRI). Agric. Syst. 79(3): 261-281.
Q. Yu, J. Liu, Y. Zhang, and J. Li. 2002. Simulation of Rice Biomass Accumulation by an Extended Logistic Model Including Influence of Meteorological Factors. Int. J. Biometeorol. 46(4): 185-191.
L. Tang, Y. Zhu, D. Hannaway, Y. Meng, L. Liu, L. Chen, and W. Cao. 2009. Ricegrow: A Rice Growth and Productivity Model. NJAS-Wagening. J. Life Sci. 57(1): 83-92.
H. Shimono, S. Fujimura, T. Nishimura, and T. Hasegawa. 2012. Nitrogen Uptake by Rice (Oryza sativa L.) Exposed to Low Water Temperatures at Different Growth Stages. J. Agron. Crop Sci. 198(2): 145-151.
S. F. Shih. 1987. Using Crop Yield and Evapotranspiration Relations for Regional Water Requirement Estimation1. JAWRA J. Am. Water Resour. Assoc. 23(3): 435-442.
T. Näsholm, K. Kielland, and U. Ganeteg. 2009. Uptake of Organic Nitrogen by Plants. New Phytol. 182(1): 31-48.
C. Masclaux-Daubresse, F. Daniel-Vedele, J. Dechorgnat, F. Chardon, L. Gaufichon, and A. Suzuki. 2010. Nitrogen Uptake, Assimilation and Remobilization in Plants: Challenges for Sustainable and Productive Agriculture. Ann. Bot. 105(7): 1141-1157.
Ardiansyah, B. I. Setiawan, C. Arif, S. K. Saptomo, and M. Mizoguchi. 2012. Soil Macro Nutrient (N, P, K) during Growth Stages under Conventional and SRI (System of Rice Intensification) Practices in Tropical Soil. In PAWEES 2012: Challenges of Water & Environmental Management in Monsoon Asia, Thailand.
R. G. Allen, L. S. Pereira, D. Raes, and M. Smith. 1998. Crop Evapotranspiration: Guidelines for Computing Crop Water Requirements. Rome: Food and Agriculture Organization of the United Nations. 1.
W. Stoop, N. Uphoff, and A. Kassam. 2002. A Review of Agricultural Research Issues Raised by the System of Rice Intensification (sri) from Madagascar: Opportunities for Improving Farming Systems for Resource-Poor Farmers. Agric. Syst. 71(3): 249-274.
A. Satyanarayana, T. M. Thiyagarajan, and N. Uphoff. 2006. Opportunities for Water Saving with Higher Yield from the System of Rice Intensification. Irrig. Sci. 25(2): 99-115.
K. A. Hameed, A.-K. J. Mosa, and F. A. Jaber. 2011. Irrigation Water Reduction Using System of Rice Intensification Compared with Conventional Cultivation Methods in Iraq. Paddy Water Environ.
G. Abera, E. Wolde-mesk, S. Beyene, and L. R. Bakken. 2012. Nitrogen Mineralization Dynamics under Different Moisture Regimes in Tropical Soils. Int. J. Soil Sci. 7(4): 132-145.
S. D. C. Case, N. P. McNamara, D. S. Reay, and J. Whitaker. 2012. The Effect of Biochar Addition on N2O and CO2 Emissions from a Sandy Loam Soil–the Role of Soil Aeration. Soil Biol. Biochem. 51: 125-134.
Ardiansyah, S. Shiozawa and K. Nishida. 2008. Thermal Properties and Shrinkage-Swelling Charateristic of Clay Soil in a Tropical Paddy Field. J. Jpn. Soc. Soil Phys. 110: 67-77.
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