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长期施肥和耕作下紫色土坡耕地径流TN和TP流失特征
摘要点击 2461  全文点击 759  投稿时间:2020-09-22  修订日期:2020-11-17
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中文关键词  施肥  耕作  氮、磷流失  地表径流  紫色土
英文关键词  fertilization  cultivation  nitrogen and phosphorus loss  surface runoff  purple soil
作者单位E-mail
吴小雨 西南大学资源环境学院, 三峡库区生态环境教育部重点实验室, 重庆 400715 292386599@qq.com 
李天阳 西南大学资源环境学院, 三峡库区生态环境教育部重点实验室, 重庆 400715  
何丙辉 西南大学资源环境学院, 三峡库区生态环境教育部重点实验室, 重庆 400715 hebinghui@swu.edu.cn 
中文摘要
      为探究长期施肥和耕作对坡耕地径流率及随径流流失的氮、磷元素的影响,在紫色土坡耕地设置5个处理:顺坡耕作无施肥(CK)、顺坡耕作有机肥与化肥配施(T1)、顺坡耕作单施化肥(T2)、顺坡耕作单施化肥增量(T3)和横坡垄作单施化肥(T4),分析了2008~2019年间共104场侵蚀性降雨事件下,各处理的径流率,总氮(TN)、总磷(TP)流失浓度及其流失率的变化特征.结果表明,各施肥处理间径流率差异不显著(P>0.05),但均低于CK(P<0.05).CK处理的TN流失浓度显著高于其他施肥处理(P<0.05),T2、T3和T4处理间TN流失浓度差异不显著(P>0.05),但均显著高于T1(P<0.05).T1、T2和T3处理的TP流失浓度显著高于CK(P<0.05),但T4处理的TP流失浓度显著低于CK(P<0.05).各施肥处理间TN流失率差异不显著(P>0.05),但均显著低于CK(P<0.05);各顺坡耕作处理间TP流失率差异不显著(P>0.05),但均显著高于横坡耕作(P<0.05).CK、T1及T2处理下,径流率与TN、TP流失浓度间的关系不显著,在T3处理下上述关系表现为显著的线性负相关(P<0.05),在T4处理下则为显著的线性正相关(P<0.05).研究结果可为紫色土区坡耕地农业面源污染防治提供科学指导.
英文摘要
      To elucidate the effects of long-term fertilization and cultivation on runoff rates and runoff-related nitrogen (N) and phosphorus (P) losses, the following five treatments were established on sloping purple soil cropland:① no fertilizer with downslope tillage (CK), ② combined application of manure and fertilizer with downslope tillage (T1), ③ chemical fertilizers with downslope tillage (T2), ④ chemical fertilizer with increasing fertilization with downslope tillage (T3), and ⑤ chemical fertilizer with contour tillage (T4). The runoff rate, runoff-related total N (TN), and total P (TP) concentrations and their loss rates from 104 erosive rainfall events were determined for the period 2008-2019. Results showed that although runoff rates were not significantly different among the fertilization treatments (P>0.05), runoff was markedly lower in fertilization treatments than in the CK treatment (P<0.05). Runoff-related TN concentrations were significantly higher in the CK compared to the fertilization treatments (P<0.05), while there were no significant differences among the T2, T3, and T4 treatments, which had higher concentrations than the T1 treatment. Runoff-related TP concentrations were significantly higher from the T1, T2, and T3 treatments than the CK treatment (P<0.05), and were significantly lower in the T4 than the CK treatment (P<0.05). TN loss rates were not significantly different among the fertilization treatments (P>0.05), but were all lower than the CK treatment (P<0.05). Furthermore, TP loss rates were not significantly different among the downslope treatments (P>0.05), but were all higher than the contour treatment (P<0.05). Runoff rates showed no significant relationships with TN and TP concentrations in the CK, T1, and T2 treatments but were significantly negatively linearly correlated in T3 (P<0.05) and significantly positively linearly correlated in T4 (P<0.05). These results potentially provide scientific guidance for the prevention and control of agricultural non-point source pollution on sloping croplands in the purple soil area.

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