首页 | 本学科首页   官方微博 | 高级检索  
     

土壤剖面硝态氮浓度分布的随机-对流传递函模模拟
引用本文:任理,袁福生,张福锁.土壤剖面硝态氮浓度分布的随机-对流传递函模模拟[J].水利学报,2002,33(2):0054-0061.
作者姓名:任理  袁福生  张福锁
作者单位:1. 中国农业大学,资源与环境学院,北京,100094黄土高原土壤侵蚀与旱地农业国家重点实验室,陕西,杨凌,712100
2. 中国农业大学,资源与环境学院,北京,100094
基金项目:国家重点基础研究发展规划项目 (G19990 1180 3),北京市自然科学基金重大项目 ( 6 980 0 0 1),黄土高原土壤侵蚀与旱地农业国家重点实验室基金课题
摘    要:依据地中渗透计出流口处观测的硝态氮通量平均浓度动态, 建立土壤硝态氮迁移时间的概率密度函数, 由随机-对流假设, 得出某一时刻土壤剖面不同埋深处硝态氮迁移距离的驻留概率密度函数, 以其作为响应函数构造对流对数正态传递函数模型, 仿真拟稳定流条件下田间土壤剖面硝态氮的驻留浓度分布. 经与实测资料对比, 表明模拟值与实测值有着较好的一致性.

关 键 词:土壤  硝态氮  驻留浓度  传递函数  随机-对流模型  初值问题
文章编号:0559-9350(2002)02-0054-07
修稿时间:2000年9月19日

A stochastic-convective transfer function model simulating resident nitrate-nitrogen concentration distribution in soil profile
REN Li,YUAN Fu-sheng,ZHANG Fu-suo.A stochastic-convective transfer function model simulating resident nitrate-nitrogen concentration distribution in soil profile[J].Journal of Hydraulic Engineering,2002,33(2):0054-0061.
Authors:REN Li  YUAN Fu-sheng  ZHANG Fu-suo
Affiliation:1.China Agricultural University 2.State Key Laboratory of Soil Erosion and Dryland Farming on Loess Plateau
Abstract:The flux-averaged concentration of nitrate-nitrogen at the reference depth is obtained from the experimental data monitored by non-weighting lyimeters. The probability density functions of nitrate-ni-trogen travel time are deduced. Based on the stochastic-convective assumption, the resident probability density functions(PDFS)for nitrate-nitrogen with depth are derived from the flux PDFS and then the convective lognormal transfer function model(CLT)can be established. The initial value problem of stachastic-convective model is solved. The validity of the model is verified by the experimental data.
Keywords:soil  nitrate-nitrogen  resident concentration  transfer function  stochastic-convective model  initial value problem
本文献已被 CNKI 维普 万方数据 等数据库收录!
点击此处可从《水利学报》浏览原始摘要信息
点击此处可从《水利学报》下载全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号