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典型红壤丘陵区土壤氮素含量及其分布的演变规律
引用本文:刘守龙,黄道友,吴金水,黄敏,肖和艾,宋变兰,苏以荣.典型红壤丘陵区土壤氮素含量及其分布的演变规律[J].植物营养与肥料学报,2006,12(1):12-17.
作者姓名:刘守龙  黄道友  吴金水  黄敏  肖和艾  宋变兰  苏以荣
作者单位:1.华中农业大学资源与环境学院 湖北武汉430070;
基金项目:中国科学院知识创新工程项目;国家高技术研究发展计划(863计划)
摘    要:通过对湖南省桃源县典型区域高密度采样分析和历史资料调研,探明了红壤丘陵区不同土地利用类型13年来(19902~2003)土壤氮素含量及其分布的变化:1)典型区域2003年的稻田氮素含量为1.94±0.02.g/kg,比1990年提高4.9%,主要分布区间由1990年的1.25~2.00.g/kg(分布频率为59.1%,下同)上升到2003年的1.50~2.25g/kg(77.1%),曲线图上呈近似正态分布向右偏态分布的演变趋势;2)旱土2003年的氮素含量为1.57±0.14.g/kg,比1990年提高18.0%,1990和2003年主要分布区间都为0.75~1.50.g/kg(58.2%~58.8%),但2003年分布在1.50~2.00.g/kg区间的频率为33.6%,比1990年的高出12.7个百分点,曲线图上由呈现左偏态分布向正态分布的演变趋势;3)以坡地橘园为主的林果地,2003年的氮素含量为1.15±0.02.g/kg,比1990年提高9.5%,两者的主要分布区间虽然均在0.75~1.50.g/kg之间,但2003年在此区间的分布频率为88.0%,比1990年的高出10.2个百分点,其演变趋势与稻田的基本一致;4)整个采样调研区域农业用地的土壤氮素含量,2003年的为1.58±0.03g/kg,比1990年提高3.3%。这表明在当前的施肥方式与经营管理条件下,红壤丘陵区农业用地的土壤氮素含量稳定并有增加的趋势。

关 键 词:土壤氮含量    变化趋势    红壤丘陵区
文章编号:1008-505X(2006)01-0012-06
收稿时间:2005-1-23
修稿时间:2005年1月23日

Evolution pattern of soil total N content and its distribution in typical hilly red soil regions
LIU Shou-long,HUANG Dao-you,WU Jin-shui,HUANG Min,XIAO He-ai,SONG Biah-lan,SU Yi-rong.Evolution pattern of soil total N content and its distribution in typical hilly red soil regions[J].Plant Nutrition and Fertilizer Science,2006,12(1):12-17.
Authors:LIU Shou-long  HUANG Dao-you  WU Jin-shui  HUANG Min  XIAO He-ai  SONG Biah-lan  SU Yi-rong
Institution:1.College of Resour.and Envir.;Huazhong Agric.Univ.;Wuhan 430070;China;
Abstract:Taking Taoyuan city as research target area,the evolution pattern of soil N content and its distribution during the last 13 years(1979—2003) under different land uses in hilly red soil regions was investigated.The results showed as follows: 1) The content of total N of paddy soil in typical area in 2003 was 1.94±0.02 g/kg.This represented a 4.9% increase compared to that in 1990.The main distribution range increased from 1.25—2.00 g/kg(distribution frequency was 59.1%,The same below) in 1990 to 1.50—2.25 g/kg(77.1%)in 2003,showing a tendency from the quasi normal distribution to right excursion distribution on the diagram of curves.2) The content of total N of dry land soil in 2003 was 1.57±0.14 g/kg,which represented a 18.0% increase compared to that in 1990.Main distribution range was 0.75—1.50 g/kg(58.2%—58.8%)both in 1990 and 2003;however,the distribution frequency ranged in 1.50—2.00 g/kg in 2003 was 33.6%,which was 0.9% higher(increased by 60.8%) than that in 1990.The distribution curve shifted from left excursion distribution to normal distribution.3) The content of total N in orchard soil(orange in slope land) was 1.15±0.02 g/kg in 2003,which represented a 9.5% increase compared to that in 1990. Main distribution range in 1990 and 2003 was similarly being 0.75—1.50 g/kg,but the distribution frequency in this range area in 2003 was 88.0%,higher than that in 1990 being 77.8%,the evolution trend of the content of N in orchard soil was similar with that in paddy soil.4)The average total N content of farmland in investigated area was 1.58±0.03 g/kg in 2003,compared to that in 1990,increased by 3.3%.This indicated that the current fertilization and management increased the content of total N in farmland soils steadily in hilly red soil regions.
Keywords:soil total N content  changing trend  hilly red soil regions
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