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黄淮海平原集约化种植条件下的土壤剖面硝态氮变化
引用本文:赵炳梓,张佳宝. 黄淮海平原集约化种植条件下的土壤剖面硝态氮变化[J]. 土壤, 2007, 39(5): 760-765
作者姓名:赵炳梓  张佳宝
作者单位:封丘农业生态国家实验站,土壤与农业可持续发展国家重点实验室(中国科学院南京土壤研究所),南京,210008
基金项目:中国科学院知识创新工程项目;国家重点基础研究发展计划(973计划);中国科学院基金
摘    要:通过田间试验研究玉米-冬小麦轮作系统下,两种不同水平的N肥施用量对NO3--N在黄淮海平原土壤剖面的分布及其动态变化规律的影响,并评估其对环境的潜在污染能力.土壤NO3--N监测为每间隔20 cm至剖面深180 cm.结果表示:作物收获后土壤剖面0~180 cm的残留NO3--N含量为107~443 kg/hm2,年际间和不同作物间的变异性较大.土壤剖面NO3--N含量随着施肥量的增加有增加的趋势,但差异不显著.当前当地农民常规施肥量处理和为常规施肥量2倍处理在试验期间出现的土壤剖面NO3--N含量峰值均在2003年的玉米生长季节,分别为688 kg/hm2和881 kg/hm2,但该玉米生长季节出现的大雨导致占0~180 cm土层50%左右的NO3--N积累在100~180 cm土层深处,该深度的NO3--N比较容易通过淋洗迁移出作物-土壤系统,也有可能是潜在的作物N素来源.由于类似大雨在当地出现的频率比较高,因此,即使在当前当地农民的传统耕作管理措施下,土壤NO3--N可能存在对环境的污染威胁,但程度如何,尚需进一步研究.

关 键 词:N肥施用水平  土壤NO3--N  剖面分布  动态变化  黄淮海平原

Variation of Soil NO3--N in Content and Its Distribution in Soil Profile under Intensive Agriculture in the North China Plain
ZHAO Bing-zi and ZHANG Jia-bao. Variation of Soil NO3--N in Content and Its Distribution in Soil Profile under Intensive Agriculture in the North China Plain[J]. Soils, 2007, 39(5): 760-765
Authors:ZHAO Bing-zi and ZHANG Jia-bao
Affiliation:State Experimental Station for Agro-Ecology, State Key Laboratory of Soil and Sustainable Agriculture(Institute of Soil Science, Chinese Academy of Sciences), Nanjing 210008, China and State Experimental Station for Agro-Ecology, State Key Laboratory of Soil and Sustainable Agriculture(Institute of Soil Science, Chinese Academy of Sciences), Nanjing 210008, China
Abstract:A field experiment was conducted in the North China Plain to investigate effect of N application rate on soil NO3--N and its distribution in the soil profile under a maize-winter-wheat cropping system.The potential hazard of soil NO3--N to the environment was also evaluated.Soil NO3--N contents were measured of soil layers,20 cm each,of a 180-cm deep soil profile.After the crops were harvested soil NO3--N residues in the profile varied greatly from year to year and from crop to crop in the field experiment with values ranging from 107 to 443 kg/hm2.A general trend of soil NO3--N content increasing with N application rate was observed,while significant difference was hardly observed.During the experiment,a peak soil NO3--N content of 688 and 881 kg/hm2 for present local farmers'' traditional N rate and 2 times the traditional N rate, respectively,was observed in the growth period of maize in 2003.It is generally considered that the soil NO3--N within the layer of 100~180 cm could easily transport by leaching to the environment that beyond the bottom of the plant-soil system or be regarded as potential N source for subsequent crop growth.About 50% of the soil NO3--N content at layers of 0~180 cm was accumulated in the deeper layers of 100~180 cm during the growth period of maize in 2003,mainly caused by the heavy rainfall occurred concurrently.It was reported that such kind of heavy rainfall occurred with high frequency.Therefore,potential contamination with NO3--N might occur even with local farmers'' traditional management strategy. Further research is required to investigate the contamination degree.
Keywords:N fertilization rate   Soil NO3--N   Profile distribution   Dynamics   Huang-Huai-Hai Plain
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