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不同耕作方式下土壤氮素矿化和硝化特征研究
引用本文:余泺,高明,慈恩,王子芳,魏朝富,徐畅.不同耕作方式下土壤氮素矿化和硝化特征研究[J].生态环境,2010,19(3):733-738.
作者姓名:余泺  高明  慈恩  王子芳  魏朝富  徐畅
作者单位:西南大学资源环境学院,重庆,北碚,400716
基金项目:国家科技支撑计划项目 
摘    要:为探讨长期定位试验田不同耕作方式下土壤氮素矿化和硝化特征,采用室内恒温通气培养法,保持土壤田间持水量在65%条件下,测定不同耕作方式下表层土壤(0~20cm)在不同温度下的NH4^+和NO3^-含量,并计算氮素矿化量和硝化率。结果表明,随着温度的升高,土壤氮素矿化和硝化作用均增强,几种耕作方式下土壤氮素矿化和硝化作用均表现为35℃〉30℃〉25℃。保护性耕作与水旱轮作和常规平作之间的矿化量存在显著的差异,垄作免耕〉厢作免耕〉水旱轮作〉常规平作。土壤氮素最终硝化率达到了60%~80%,表现为常规平作最高,水旱轮作次之,厢作免耕最低。矿化率与土壤有机质、碱解氮和速效磷对数均成显著正相关,相关系数分别为r^2=0.99,r^2=0.97,r^2=0.96,pH是影响硝化作用的重要因素,硝化率与土壤pH成显著正相关,r^2=0.991。

关 键 词:矿化  硝化  免耕  水旱轮作  常规平作

Study on the characteristics of mineralization and nitrification in different cultivation modes
YU Luo,GAO Ming,CI En,WANG Zhifang,WEI Chaofu,XU Chang.Study on the characteristics of mineralization and nitrification in different cultivation modes[J].Ecology and Environmnet,2010,19(3):733-738.
Authors:YU Luo  GAO Ming  CI En  WANG Zhifang  WEI Chaofu  XU Chang
Institution:(College of Resources and Environment, Southwest Agricultural University, Chongqing 400716, China)
Abstract:To explore the difference of soil nitrogen mineralization and nitrification between the no-tillage and conventional tillage soils in long-term experimental fields, an indoor heated aerobic incubation experiment was conducted to investigate the NH_4~+ and NO_3~- of the protection of surface soil (0~20 cm) at different temperatures, with 65% water holding capacity, and also calculate the nitrogen mineralization and nitrification rates. Result showed that with the increasing of temperature, soil mineralization and nitrifi-cation were increased. Soil mineralization aad nitrification were expressed as 35 ℃> 30 ℃> 25℃.At the same time, there was sig-nificantly difference between conservation tillage and farming methods in soil mineralization, no-tillage and ridge culture > no-tillage and plain culture > Paddy-Upland rotation > conventional flatten culture. The final nitrification rate reached 60%~80%, conventional flatten culture > Paddy-Upland rotation > no-tillage and ridge culture > no-tillage and plain culture. Mineralization rate of soil was significantly related to soil organic matter content, soil mineral N content and soil available P, r~2 = 0.99, r~2= 0.97, r~2 = 0.96, soil pH was an important factor to influence soil nitrification, nitrification rate of soil was significantly correlated with soil pH, r~2=0.991.
Keywords:mineralization  nitrification  no-tillage  Paddy-Upland Rotation  conventional flatten culture
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