Zhang Huanchao, Cao Zhihong, Wang Gaiping, Zhang Hongai, Wong M H
The Institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008, China.
Chemosphere. 2003 Sep;52(9):1461-6. doi: 10.1016/S0045-6535(03)00483-1.
A winter wheat field plot experiment was conducted on two types of paddy soils, from November, 2000 to June, 2001 to assess P losses to its surrounding watercourses by runoff in the Taihu Lake Region. Commercial NPK compound fertilizer and single superphosphate fertilizer were applied to furnish 0, 20, 80, and 160 kg P ha(-1). The experiments consisted of six replicates of each treatment in Changshu site and four replicates in Anzhen site, with a plot size of 5x6 m2 in a randomized block design. Results revealed that the average concentration of dissolved P (DP), particulate P (PP), and total P (TP) in runoff water during the winter season was 0.13, 0.90 and 1.04 mg P l(-1) respectively, from P20 plots in Anzhen site. While it was 0.67, 1.08 and 1.75 mg P l(-1) respectively, from P20 plots in Changshu site. The seasonal TP load (mass loss) from P20 plot ranged from a low of 290.88 g P ha(-1)season(-1) to a high of 483.54 g P ha(-1)season(-1), with a mean of 382.29 g P ha(-1)season(-1) in Anzhen, but from 444.92 to 752.21 g P ha(-1)season(-1), with a mean of 539.13 g P ha(-1)season(-1) in Changshu. Both in Anzhen and Changshu PP represented a major portion of the TP lost in runoff, the average PP/TP was about more than 80% in P0 and P20 plot, but it was decreased with the increase of P rate. The average seasonal P loads (DP, PP, and TP) in Changshu were greater than in Anzhen although runoff volume in Anzhen (45 mm season(-1)) was more than in Changshu (36 mm season(-1)). This was probably associated with the differences of soil physical and chemical properties between the two sites. Phosphate fertilizer rate significantly affected P concentrations and P loads by runoff. Both the mean concentrations and the average seasonal P loads from the P80 plots were lower than from the P160 plots, but obviously higher than from the P20 and P0 plots. There was no significant difference found between the P20 plots and the P0 plots both in Anzhen and Changshu sites. It indicated that P loads by runoff would be greatly increased in 5-10 years due to the accumulation of soil P if 20 kg P ha(-1) applied each wheat season in this area.
2000年11月至2001年6月,在太湖地区的两种稻田土壤上进行了冬小麦田间试验,以评估径流造成的磷流失到周边水道的情况。施用了商业氮磷钾复合肥和过磷酸钙单肥,施磷量分别为0、20、80和160 kg P ha⁻¹。实验在常熟试验点每个处理设置6个重复,在安镇试验点每个处理设置4个重复,小区面积为5×6 m²,采用随机区组设计。结果表明,冬季安镇试验点P20小区径流水中溶解磷(DP)、颗粒磷(PP)和总磷(TP)的平均浓度分别为0.13、0.90和1.04 mg P l⁻¹。而常熟试验点P20小区径流水中溶解磷、颗粒磷和总磷的平均浓度分别为0.67、1.08和1.75 mg P l⁻¹。P20小区的季节性总磷负荷(质量损失)在安镇试验点低至290.88 g P ha⁻¹季节⁻¹,高至483.54 g P ha⁻¹季节⁻¹,平均为382.29 g P ha⁻¹季节⁻¹;而在常熟试验点则为444.92至752.21 g P ha⁻¹季节⁻¹,平均为539.13 g P ha⁻¹季节⁻¹。在安镇和常熟试验点,颗粒磷在径流流失的总磷中均占主要部分,P0和P20小区的颗粒磷/总磷平均约超过80%,但随着施磷量增加而降低。常熟试验点的季节性磷负荷(溶解磷、颗粒磷和总磷)平均高于安镇试验点,尽管安镇试验点的径流量(45 mm季节⁻¹)大于常熟试验点(36 mm季节⁻¹)。这可能与两个试验点土壤理化性质的差异有关。磷肥施用量显著影响径流中的磷浓度和磷负荷。P80小区的平均浓度和季节性磷负荷均低于P160小区,但明显高于P20和P0小区。在安镇和常熟试验点,P20小区和P0小区之间均未发现显著差异。这表明,如果该地区每个小麦季节施用20 kg P ha⁻¹,由于土壤磷的积累,5至10年内径流造成的磷负荷将大幅增加。