| 生物炭配施缓控释肥对稻田田面水氮素动态变化及径流流失的影响 |
| 摘要点击 1893 全文点击 729 投稿时间：2018-03-27 修订日期：2018-05-25 |
| 查看HTML全文
查看全文 查看/发表评论 下载PDF阅读器 |
| 中文关键词 生物炭 控释肥 稳定性肥 氮素 田面水 径流 |
| 英文关键词 biochar controlled-release fertilizer stabilized fertilizer nitrogen paddy field surface water runoff |
| 作者 | 单位 | E-mail | | 斯林林 | 浙江大学环境与资源学院, 浙江省农业资源与环境重点实验室, 杭州 310058
金正大生态工程集团股份有限公司, 养分资源高效开发与综合利用国家重点实验室, 临沂 276000
浙江大学环境与资源学院, 教育部环境修复与生态健康重点实验室, 杭州 310058 | sdarling2011@163.com | | 周静杰 | 浙江大学环境与资源学院, 浙江省农业资源与环境重点实验室, 杭州 310058
金正大生态工程集团股份有限公司, 养分资源高效开发与综合利用国家重点实验室, 临沂 276000
浙江大学环境与资源学院, 教育部环境修复与生态健康重点实验室, 杭州 310058 | | | 吴良欢 | 浙江大学环境与资源学院, 浙江省农业资源与环境重点实验室, 杭州 310058
金正大生态工程集团股份有限公司, 养分资源高效开发与综合利用国家重点实验室, 临沂 276000
浙江大学环境与资源学院, 教育部环境修复与生态健康重点实验室, 杭州 310058 | finm@zju.edu.cn | | 胡兆平 | 金正大生态工程集团股份有限公司, 养分资源高效开发与综合利用国家重点实验室, 临沂 276000 | |
|
| 中文摘要 |
| 在太湖流域，通过田间试验研究了控释肥（CRF）、生物炭配施控释肥（BC+CRF）、生物炭配施稳定性肥（BC+SF）、生物炭配施控释肥和稳定性肥（BC+CRF+SF）4种施肥处理对稻田田面水pH、氮素动态变化、氮素径流流失的影响.结果表明，田面水平均pH介于5.64~8.15，生物炭配施控释肥和稳定性肥田面水pH降低3.16%~4.48%.田面水平均全氮（TN）质量浓度介于19.05~25.23 mg·L-1，生物炭配施控释肥和稳定性肥田面水TN质量浓度显著降低4.75%~6.58%.田面水无机氮素以铵态氮（NH4+-N）为主，NH4+-N和硝态氮（NO3--N）平均质量浓度分别介于0.01~17.26 mg·L-1和0.24~3.11 mg·L-1.与单施控释肥相比，各处理田面水NH4+-N和NO3--N质量浓度分别显著降低35.89%~48.78%和20.54%~37.01%.生物炭配施稳定性肥显著降低了田面水NH4+-N和NO3--N质量浓度，有效减少无机氮素径流流失风险.TN、NH4+-N、NO3--N径流流失量分别介于16.24~18.09、1.76~2.22、0.76~1.38 kg·hm-2.与单施控释肥相比，各处理TN、NH4+-N、NO3--N径流流失均有不同程度削减.生物炭配施控释肥和稳定性肥显著削减了氮素径流流失，有效降低区域稻田氮素面源污染风险. |
| 英文摘要 |
| Field experiments were conducted to investigate the effects of four fertilization treatments, that is, controlled-release fertilizer (CRF), biochar combined with controlled-release fertilizer (BC+ CRF), biochar combined with stabilized fertilizer (BC+ SF), and biochar combined with controlled-release fertilizer and stabilized fertilizer (BC+ CRF+ SF), on the dynamics of the pH and nitrogen mass concentration and runoff losses of nitrogen in paddy field surface water in the Taihu Lake Basin. The results show that the average pH of the surface water decreases by 3.16%-4.48% for BC+ CRF+ SF and is in the range of 5.64-8.15. The average total nitrogen (TN) mass concentration of surface water ranges from 19.05 to 25.23 mg·L-1. A significant decrease of 4.75%-6.58% in the TN mass concentration of surface water was observed for BC+ CRF+ SF. The average ammonium (NH4+-N) and nitrate (NO3--N) mass concentration of the surface water vary from 0.01-17.26 mg·L-1 and from 0.24-3.11 mg·L-1, respectively. Inorganic nitrogen is dominated by NH4+-N in surface water. Compared with individual CRF, other treatments significantly reduce the NH4+-N mass concentration of surface water by 35.89%-48.78% and the NO3--N mass concentration of surface water by 20.54%-37.01%. The BC+ SF combination shows a significant reduction in the NH4+-N and NO3--N mass concentration of the surface water, which greatly lowers the risk of inorganic nitrogen loss via runoff. The runoff losses of TN, NH4+-N, and NO3--N are in the range of 16.24-18.09, 1.76-2.22 and 0.76-1.38 kg·hm-2, respectively. Compared with the individual CRF, the runoff loss of TN, NH4+-N, and NO3--N of other treatments is reduced. The BC+ CRF+ SF combination shows a significant reduction in the runoff losses of nitrogen, which greatly lowers the risk of nitrogen nonpoint source pollution from paddy fields. |
|
|
|
