Ji Xiong-Hui, Zheng Sheng-Xian, Lu Yan-Hong, Liao Yu-Lin
Hunan Institute of Soil & Fertilizer, Changsha 410125, China.
Ying Yong Sheng Tai Xue Bao. 2007 Jul;18(7):1432-40.
By using leakage pond to simulate the double cropping paddy fields in Dongtinghu Lake area, this paper studied the effects of urea (CF) and controlled release nitrogen fertilizer (CRNF) on the dynamics of surface water pH, electrical conductivity (EC), total nitrogen (TN), ammonia nitrogen (NH4(+)-N) and nitrate nitrogen (NO3(-)-N) and the runoff loss of TN in alluvial sandy loamy paddy soil and purple calcareous clayed paddy soil, the two main paddy soils in this area. The results showed that after applying urea, the surface water TN and NH4(+)-N concentrations reached the peak at the 1st and 3rd day, respectively, and decreased rapidly then. Surface water NO3(-)-N concentration was very low, though it showed a little raise at the 3rd to 7th day after applying urea in purple calcareous clayed paddy soil. In early rice field, surface water pH rose gradually within 15 days after applying urea, while in late rice field, it did within 3 days. EC kept consistent with the dynamics of NH4(+)-N. CRNF, especially 70% N CRNF, gave rise to distinctly lower surface water pH, EC, and TN and NH4(+)-N concentrations within 15 days after application, but NO3- concentration rose slightly at late growth stages, compared with urea application. The monitoring of TN runoff loss indicated that during double cropping rice growth season, the loss amount of TN under urea application was 7.70 kg x hm(-2), accounting for 2.57% of applied urea-N. The two runoff events occurred within 20 days after urea application contributed significantly to the TN runoff loss. CRNF application resulted in a significantly lower TN concentration in runoff water from the 1st runoff event occurred within 10 days of its application, and thereafter, the total TN runoff loss for CRNF and 70% N CRNF application was decreased by 24.5% and 27.2%, respectively, compared with urea application.
通过利用渗漏池模拟洞庭湖地区的双季稻田,本文研究了尿素(CF)和控释氮肥(CRNF)对该地区两种主要水稻土——冲积砂质壤土水稻土和紫色钙质黏土水稻土——地表水pH值、电导率(EC)、总氮(TN)、氨氮(NH₄⁺-N)和硝态氮(NO₃⁻-N)动态变化以及TN径流损失的影响。结果表明,施用尿素后,地表水TN和NH₄⁺-N浓度分别在第1天和第3天达到峰值,随后迅速下降。地表水NO₃⁻-N浓度很低,尽管在紫色钙质黏土水稻土中施用尿素后第3至7天略有升高。在早稻田中,施用尿素后15天内地表水pH值逐渐上升,而在晚稻田中,3天内上升。EC与NH₄⁺-N的动态变化一致。与施用尿素相比,CRNF,尤其是70%氮CRNF,在施用后15天内使地表水pH值、EC以及TN和NH₄⁺-N浓度明显降低,但在生长后期NO₃⁻浓度略有上升。TN径流损失监测表明,在双季稻生长季节,施用尿素下TN损失量为7.70 kg·hm⁻²,占施用尿素氮的2.57%。施用尿素后20天内发生的两次径流事件对TN径流损失贡献显著。施用CRNF后,在其施用后10天内发生的第一次径流事件中,径流水中TN浓度显著降低,此后,与施用尿素相比,CRNF和70%氮CRNF施用的总TN径流损失分别降低了24.5%和27.2%。