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应用Geoprobe对河北栾城土壤硝态氮含量进行计算
引用本文:李晓欣,胡春胜,雷玉平,张玉铭.应用Geoprobe对河北栾城土壤硝态氮含量进行计算[J].土壤通报,2006,37(5):906-908.
作者姓名:李晓欣  胡春胜  雷玉平  张玉铭
作者单位:1. 中科院,生态环境研究中心,北京,100085;中科院,研究生院,北京,100039
2. 中科院,遗传发育所农业资源研究中心,河北,石家庄,050021
摘    要:利用Geoprobe对土壤剖面取样,分析并计算了0~20.4m土层硝态氮的累积量,研究表明,施肥量的上升和地下水埋深的下降,使得多余的氮肥以硝态氮的形式存储在土壤剖面中,在传统的施肥制度下,0~20.4m剖面总累积的硝态氮量为1769kg hm-2,自地表至下,土壤硝态氮的分布存在三个累积层,分别为0~5.4m,7.2~12m,14.7~18.4m;而且三个层次累积的硝态氮量随深度呈递减的趋势。

关 键 词:Geoprobe  硝态氮  累积  分布
文章编号:0564-3945(2006)05-0906-03
修稿时间:2005年6月27日

Calculation for the Accumulation of Nitratenitrogen in a Luancheng Soil by Geoprobe
LI Xiao-xin,HU Chun-sheng,LEI Yu-ping,ZHANG Yu-ming.Calculation for the Accumulation of Nitratenitrogen in a Luancheng Soil by Geoprobe[J].Chinese Journal of Soil Science,2006,37(5):906-908.
Authors:LI Xiao-xin  HU Chun-sheng  LEI Yu-ping  ZHANG Yu-ming
Abstract:In this paper we analyzed the distribution of nitratenitrogen in different soil depth profiles in a field under traditional planting for years,and we also calculated the amount of nitratenitrogen accumulated in the Luancheng soil.The results showed: with the increasing fertilizer N input and soil water table,significant amounts of nitrate were lost from the soil,and there were 1769kg ha~(-1) nitratenitrogen accumulated in the soil from 0 to 20.4 meter depth.In the soil depth profile there were three nitrate accumulation layers: 0-5.4m,7.2-12m,14.7-18.4m,and with the depth increasing the content of nitrate decreased.
Keywords:Geoprobe
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