文章摘要
高晶波,路永莉,陈竹君,周建斌.猕猴桃园氮素投入特点及硝态氮累积和迁移特性研究[J].农业环境科学学报,2016,35(2):322-328.
猕猴桃园氮素投入特点及硝态氮累积和迁移特性研究
Nitrogen inputs and nitrate accumulation and movement in soil of kiwifruit orchards
投稿时间:2015-08-28  
DOI:10.11654/jaes.2016.02.016
中文关键词: 秦岭北麓  猕猴桃园  硝态氮累积  雨季  硝态氮迁移
英文关键词: northern slope region of Qinling Mountains  kiwifruit orchard  NO3--N accumulation  rainy season  NO3--N movement
基金项目:国家"十二五"科技支撑计划项目课题(2012BAD15B04);高等学校学科创新引智计划(B12007)资助项目
作者单位E-mail
高晶波 西北农林科技大学资源环境学院, 陕西 杨凌 712100
农业部西北植物营养与农业环境重点实验室, 陕西 杨凌 712100 
 
路永莉 西北农林科技大学资源环境学院, 陕西 杨凌 712100
农业部西北植物营养与农业环境重点实验室, 陕西 杨凌 712100 
 
陈竹君 西北农林科技大学资源环境学院, 陕西 杨凌 712100
农业部西北植物营养与农业环境重点实验室, 陕西 杨凌 712100 
 
周建斌 西北农林科技大学资源环境学院, 陕西 杨凌 712100
农业部西北植物营养与农业环境重点实验室, 陕西 杨凌 712100 
jbzhou@nwsuaf.edu.cn 
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中文摘要:
      为指导果园科学施肥及合理评价施肥对环境的影响,2014年对该区域的陕西省周至县俞家河小流域氮素投入状况进行了调查,并采集猕猴桃园土壤样品进行测定,评价了猕猴桃园土壤硝态氮(NO3--N)累积及降雨对坡地猕猴桃园NO3--N迁移特性的影响。结果表明:该区域猕猴桃园氮素投入量过高,盈余量高达1195 kg·hm-2,0~200 cm土壤剖面NO3--N累积量高达827 kg·hm-2,且52.1%的NO3--N累积在100~200 cm土层;对于坡地猕猴桃园,坡下部0~200 cm土壤剖面NO3--N累积量明显高于坡上部,在经过一个雨季后,0~200 cm土壤剖面NO3--N发生明显的向深层土壤淋溶现象且坡下部与坡上部0~200 cm土壤剖面NO3--N累积量差异增大。俞家河小流域猕猴桃园大量氮素盈余,造成土壤NO3--N过分累积,在集中降雨条件下,NO3--N出现明显的向深层土壤淋溶且可能存在顺坡向下迁移的趋势,不仅造成氮肥的损失,而且对地表及地下水环境构成潜在威胁。
英文摘要:
      The northern slope region of the Qinling Mountains is the main growing area of kiwifruit in Shaanxi Province. However, inadequate application of nitrogen(N) in kiwifruit orchard is very common. Therefore, studying N plant utilization and movement in soil is of great significance for achieving balanced fertilization and evaluating the effect of N fertilization on the environment in this region. A survey was conducted in Yujiahe catchment in 2014 to assess the status of N inputs. Soil profile samples in 0~200 cm depth from mature kiwifruit orchards were collected to examine the accumulation and movement of NO3--N in the soil profiles of sloping kiwifruit orchard. Excessive applications of N were very severe in the catchment. The surplus of N applied was high up to 1195 kg·hm-2 with residual NO3--N being 827 kg·hm-2 in the 0~200 cm soil profile, of which 52% of N was accumulated in 100~200 cm soil profile. The accumulation of NO3-N in the 0~200 cm soil profile was dependent on the locations within an orchard:more NO3-N was accumulated in the lower part than in the upper one of a slope. After a rainy season, NO3-N was leached to deeper part of the soil profile. It is concluded that excessive additions of N to kiwifruit orchard in Yujiahe catchment results in high accumulation of NO3--N in the soil. The NO3-N leaching in soil profiles during the rainy season is also severe. Nitrate leaching not only wastes N fertilizer resource, but also increases potential risk to the quality of both surface and groundwater.
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