Variation in the relationship between nitrification and acidification of subtropical soils as affected by the addition of urea or ammonium sulfate

被引:63
|
作者
Zhao, Xu [2 ]
Xing, Guang-xi [1 ]
机构
[1] Chinese Acad Sci, Inst Soil Sci, State Key Lab Soil & Sustainable Agr, Nanjing 210008, Peoples R China
[2] Chinese Acad Sci, Inst Soil Sci, Key Lab Soil Environm & Pollut Remediat, Nanjing 210008, Peoples R China
来源
SOIL BIOLOGY & BIOCHEMISTRY | 2009年 / 41卷 / 12期
关键词
Acidification; NH4+ input; Nitrification; Subtropics; NITROGEN TRANSFORMATIONS; ECOSYSTEM CONSEQUENCES; ISOTOPIC FRACTIONATION; FOREST SOIL; PH; DEPOSITION;
D O I
10.1016/j.soilbio.2009.08.022
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
The effects on nitrification and acidification in three subtropical soils to which (NH4)(2)SO4 or urea had been added at rate of 250 mg N kg(-1) was studied using laboratory-based incubations. The results indicated that NH4+ input did not stimulate nitrification in a red forest soil, nor was there any soil acidification. Unlike red forest soil, (NH4)(2)SO4 enhanced nitrification of an upland soil, whilst urea was more effective in stimulating nitrification, and here the soil was slightly acidified. For another upland soil, NH4+ input greatly enhanced nitrification and as a result, this soil was significantly acidified. We conclude that the effects of NH4+ addition on nitrification and acidification in cultivated soils would be quite different from in forest soils. During the incubation, N isotope fractionation was closely related to the nitrifying capacity of the soils. (C) 2009 Elsevier Ltd. All rights reserved.
引用
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页码:2584 / 2587
页数:4
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