Response of paddy field cyanobacterium, Westiellopsis prolifica Janet to the inorganic nitrogenous fertilizers

M. Shamina
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Abstract

Cyanobacteria are oxygen evolving, nitrogen fixing prokaryotes occur in every conceivable habitats but abundantly in water logged rice fields in several rice growing countries. Nitrogen fixing cyanobacteria play a vital role in the maintanence of soil fertility and sustainability in rice field ecosystems (Roger & Reynaud, 1979). Cyanobacterial inoculation to rice crop was found to be effective in different agroclimatic conditions like tropical or temperate climates and soil types such as saline soils, phosphorous rich soils, alkaline or acidic soils etc. (Singh et al., 2017). The paddy field ecosystem provides an environment favourable for the growth of cyanobacteria with respect to their requirement for light, water, temperature, humidity and nutrient availability. In submerged soil system, biological nitrogen fixation contributes 25 to 30 kg nitrogen per hectre for one cropping season (Saexena et al., 2007; Kaushik, 2001). They are cosmopolitan in distribution and occur in every conceivable habitat where life is possible. They are reported to occur in extreme climatic conditions such as hot springs, polar deserts and Antartic regions (Halder, 2015, 2016). Even though they are ubiquitious, they prefer to grow in rice fields because the soil pH, temperature, humidity, crop canopy and soil moisture are favourable for its growth in paddy fields. It releases a large number of secondary metabolites into the paddy fields which also influences the growth of paddy (Wilson, 2006). The beneficial effect of cyanobacterial biofertilizer for paddy such as increase in number of tillers, seeds, length of the plant and leaf, yield etc. has been well documented (Karthikeyan et al., 2009; Sao & Samual, 2018; Radhakrishnan & Venkitaraman, 2005). Cyanobacterial biomass is also used for the production of various bioactive compounds, food items and biofuels (Hall et al., 1995; Malik et al., 2001; Paumann et al., 2005). They can control the deficiency of nitrogen in the soil and also improves its properties. Apart from nitrogen fixation, it also influences the overall growth of paddy including the grain yield (Roger et al., 1980; Singh, 1981; Alam et al., 2014). Since the urea and ammonium sulphate are the easily available and commonly used inorganic nitrogen fertilizer in the paddy fields of India, this made the the author to study how much these synthetic nitrogen fertilizers such as urea and ammonium sulphate influences the growth of paddy field cyanobacterium, Westiellopsis prolifica.
稻田蓝藻对无机氮肥的响应
蓝藻是一种进化氧气、固定氮的原核生物,存在于每一个可能的栖息地,但在几个水稻种植国的水稻田中却大量存在。在稻田生态系统中,固氮蓝藻在维持土壤肥力和可持续性方面起着至关重要的作用(Roger & Reynaud, 1979)。研究发现,在不同的农业气候条件下(如热带或温带气候)和土壤类型(如盐渍土、富磷土壤、碱性或酸性土壤等),接种蓝藻对水稻作物都是有效的(Singh等,2017)。水田生态系统为蓝藻的生长提供了一个有利的环境,就其对光、水、温度、湿度和养分有效性的需求而言。在淹水土壤系统中,生物固氮在一个种植季节每公顷贡献25至30公斤氮(Saexena等人,2007;Kaushik, 2001)。它们分布在世界各地,出现在每一个可能有生命的栖息地。据报道,它们发生在极端气候条件下,如温泉、极地沙漠和南极地区(Halder, 2015, 2016)。尽管它们无处不在,但它们更喜欢在稻田中生长,因为土壤pH值、温度、湿度、作物冠层和土壤水分都有利于它们在稻田中生长。它向稻田释放了大量次生代谢物,也影响了水稻的生长(Wilson, 2006)。蓝藻生物肥料对水稻的有益影响,如增加分蘖数、种子、植株和叶片的长度、产量等,已得到充分的证明(Karthikeyan等人,2009;Sao & Samual, 2018;Radhakrishnan & Venkitaraman, 2005)。蓝藻生物量也用于生产各种生物活性化合物、食品和生物燃料(Hall等,1995;Malik et al., 2001;Paumann et al., 2005)。它们可以控制土壤中氮的缺乏,也可以改善土壤的性质。除固氮作用外,还影响水稻的整体生长,包括籽粒产量(Roger et al., 1980;辛格,1981;Alam et al., 2014)。由于尿素和硫酸铵是印度水田中容易获得和常用的无机氮肥,因此作者研究了尿素和硫酸铵等合成氮肥对水田蓝藻(Westiellopsis prolifica)生长的影响程度。
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