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滴灌施肥条件下土壤水分和硝态氮的分布规律
引用本文:王虎,王旭东,赵世伟.滴灌施肥条件下土壤水分和硝态氮的分布规律[J].西北农业学报,2008,17(6):309-314.
作者姓名:王虎  王旭东  赵世伟
作者单位:1. 西北农林科技大学,资源环境学院,陕西杨凌,712100;杨凌职业技术学院,陕西杨凌,712100
2. 西北农林科技大学,资源环境学院,陕西杨凌,712100
3. 西北农林科技大学,资源环境学院,陕西杨凌,712100;中国科学院、水利部水土保持研究所,陕西杨凌,712100
基金项目:国家高技术研究发展计划(863计划) , 西北农林科技大学科研专项基金  
摘    要:用硝态氮含量为258 mg/L的肥料溶液在土上进行滴灌施肥试验,研究不同滴头流量(2,4,6L/h)、不同灌水施肥量(8,16,24 L)条件下,水分和硝态氮在土中的运移分布规律。结果表明,灌水施肥量为8 L时,随滴头流量增大,滴头周围地表积水区半径增大,水分径向运移距离增大、竖向入渗水量减小;当滴头流量为2 L/h时,随灌水施肥量增大,水分径向和竖向运移距离增大,径向运移距离增大幅度较竖向明显。滴灌施肥条件下硝态氮在土壤中的运移受对流作用控制;湿润体内土壤硝态氮含量随距滴头径向距离增大而减小,随距滴头竖向距离增大而增大,在竖向湿润锋附近有硝态氮累积现象;随滴头流量增大,硝态氮在土壤中的径向运移距离增大,0~25 cm土层滴头径向25 cm范围土壤硝态氮平均含量增大;随灌水施肥量增大,滴头径向15 cm范围0~15 cm土层土壤硝态氮含量增大1、7.5~30 cm土层硝态氮含量减小,过度增大灌水施肥量会导致土壤湿润锋附近硝态氮淋溶下渗。

关 键 词:滴灌施肥  滴头流量  灌水施肥量  土壤硝态氮分布  水分分布
收稿时间:2008/4/17 0:00:00
修稿时间:2008/5/25 0:00:00

Distribution of Soil Water and Nitrate in Lou Soil under Drip Fertigation
WANG Hu,WANG Xu-dong and ZHAO Shi-wei.Distribution of Soil Water and Nitrate in Lou Soil under Drip Fertigation[J].Acta Agriculturae Boreali-occidentalis Sinica,2008,17(6):309-314.
Authors:WANG Hu  WANG Xu-dong and ZHAO Shi-wei
Institution:College of Resource and Environment, Northwest A&F University, Yangling Shaanxi 712100, China;Yangling Vocational and Technical College, Yangling Shaanxi 712100, China;College of Resource and Environment, Northwest A&F University, Yangling Shaanxi 712100, China;College of Resource and Environment, Northwest A&F University, Yangling Shaanxi 712100, China;Institute of Soil and Water Conservation, Chinese Academy of Sciences and Ministry of Water Resource, Yangling Shaanxi 712100, China
Abstract:Put some quantity of NH4NO3 fertilizer in water,confect fertilizer liquor,the NO3--N density is 258 mg/L,use the fertilizer liquor to do fertigation test,the distributions of water and NO3--N in Lou soil were investigated under the controlled condition such as dripping end rate at 2,4,6 L/h and fertigation volume at 8,16,24 L/h.The results showed that as fertigation volume was 8 L/h,with dripping rate increased,surface catchment radius around tip increased and more water trans-ported horizontally,while less water transported vertically.As dripping rate was 2 L/h,with irrigation volume increased,dripped water transporting to horizontal and vertical direction are all increased.But water increased more in horizontal direction than in vertical direction.NO3--N moving belongs to "convectio ncontrol" style;as the level distance increased,NO3--N density decreased,as the soil layer depth increased, NO3--N density increased firstly,and then reduced later,cumulate NO3--N emerged round soil wetness peak in vertical;dripping end flow increased,NO3--N moving distance in horizontal in soil increased,NO3--N density increased in level of 25 cm and 0-25 cm in vertical in soil;irrigation and fertilization volume increased,NO3--N density increased in the scope of 15cm in level and 0-15 cm in vertical,decreased in the scope of 30 cm in level and 17.5~30 cm in vertical, fertigation increased more NO3--N around soil wetness peak would shower and leakage down.
Keywords:Dripping fertigation  Flow rate of dripping end  Irrigation volume  Nitrate distribution  Water distribution
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