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东灵山油松纯林和油松-辽东栎针阔混交林土壤氮素矿化/硝化作用研究 被引量:62
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作者 苏波 韩兴国 +1 位作者 渠春梅 黄建辉 《植物生态学报》 CAS CSCD 北大核心 2001年第2期195-203,共9页
利用 PVC顶盖埋管原位培育法测定了北京东灵山地区一个油松纯林和一个油松 -辽东栎落叶阔叶混交林生态系统土壤无机氮库、氮素净矿化 /硝化速率的季节动态以及年度净矿化 /硝化量。结果发现 :1)两个生态系统的土壤无机氮库和氮素净矿化 ... 利用 PVC顶盖埋管原位培育法测定了北京东灵山地区一个油松纯林和一个油松 -辽东栎落叶阔叶混交林生态系统土壤无机氮库、氮素净矿化 /硝化速率的季节动态以及年度净矿化 /硝化量。结果发现 :1)两个生态系统的土壤无机氮库和氮素净矿化 /硝化速率都存在比较明显且比较一致的季节动态 ,但个别时期也存在较大差异 ;2 )纯林与混交林土壤 NH+ 4 - N浓度在各月都没有显著差异 ,而 NO- 3 - N浓度 ,除了 1995年 11月和 1996年 8月纯林显著高于混交林外 ,其它月份也都差异不显著 ;3)无论是年度净矿化总量 (纯林 ,2 2 .7kg· hm- 2 ;混交林 ,5 5 .5 kg·hm- 2 )及其占总全 N量的百分比 (纯林 ,0 .6 94% ;混交林 ,2 .12 8% ) ,还是年度净硝化总量 (纯林 ,2 6 .7kg· hm- 2 ;混交林 ,44 .6 kg· hm- 2 )及其占总全 N量 (纯林 ,0 .815 % ;混交林 ,1.70 7% )的百分比 ,油松针阔混交林生态系统均显著大于油松纯林 ,高达后者的两倍左右 ,而净硝化氮占净矿化氮的百分比则相反 ,油松纯林 (10 0 % )显著高于油松 -辽东栎混交林 (80 .2 % )。上述结果表明 :油松 -辽东栎针阔混交林生态系统土壤的氮素有效性 (即土壤的供氮能力 )以及维持土壤中植物可利用氮素的能力都显著高于油松纯林。物种构成及在其影响下所产生的林下微? 展开更多
关键词 东灵山 油松 针阔混交林 矿化/硝化作用 季节动态 土壤 氮素
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科尔沁沙地不同生境土壤氮矿化/硝化作用研究 被引量:23
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作者 李玉强 赵哈林 +2 位作者 李玉霖 崔建垣 左小安 《中国沙漠》 CSCD 北大核心 2009年第3期438-444,共7页
利用顶盖埋管原位培育法测定了科尔沁沙地不同生境(丘间低地、固定、半固定、半流动和流动沙丘)土壤氮素矿化/硝化速率的月际动态及净矿化/硝化量。结果表明:①沙地土壤无机氮主要以NO3--N的形式存在,各类生境土壤NH4+-N平均含量比N... 利用顶盖埋管原位培育法测定了科尔沁沙地不同生境(丘间低地、固定、半固定、半流动和流动沙丘)土壤氮素矿化/硝化速率的月际动态及净矿化/硝化量。结果表明:①沙地土壤无机氮主要以NO3--N的形式存在,各类生境土壤NH4+-N平均含量比NO3--N低58.2%~79.7%;②土壤氮素矿化/硝化速率随植被与土壤条件的恶化呈现递减的趋势,从丘间低地到流动沙丘,净矿化速率分别为61.0、43.4、29.1、5.3 mg.m-2.d-1和2.7mg.m-2.d-1,净硝化速率分别为61.8、46.2、30.1、6.2 mg.m-2.d-1和3.4 mg.m-2.d-1;③从丘间低地到固定、半固定、半流动和流动沙丘,矿化氮总量分别减少28.8%、52.3%、91.4%和95.5%,硝化总量分别减少25.3%、51.3%、90.0%和94.5%;④不同类型生境土壤净硝化氮占净矿化氮的比例都为100%,表明沙地土壤中植物可利用氮素易于淋溶或氨挥发损失。 展开更多
关键词 土壤氮素 矿化/硝化作用 科尔沁沙地
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Effect of Fluctuating Temperatures on Forest SoilNitrogen Mineralization 被引量:3
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作者 LIAOLIPING P.INESON 《Pedosphere》 SCIE CAS CSCD 1997年第1期31-34,共4页
Nitrogen mineralization in forest soil was studied in laboratory by incubating undisturbed soil cores enclosed within PVC columns at different temperatures to compare the effect of fluctuating temperature with that of... Nitrogen mineralization in forest soil was studied in laboratory by incubating undisturbed soil cores enclosed within PVC columns at different temperatures to compare the effect of fluctuating temperature with that of constant temperature, and to find out whether soil nitrification shows linearity over time. The results showed that there was no significant difference between soil nitrification at fluctuating temperature and that at constant temperature, and suggested that it must be careful to make the conclusion that soil nitrification has linearity over time. 展开更多
关键词 fluctuating temperature LINEARITY nitrogen mineralization
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Effects of adding water on seasonal variation of soil nitrogen availability under sandy grasslands in semi-arid region
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作者 黄晓星 于占源 +2 位作者 钱伟 徐大勇 艾桂艳 《Journal of Forestry Research》 SCIE CAS CSCD 2007年第4期287-290,共4页
Water is usally thought of a limiting factor for the restoration of semi-arid ecosystem. In the growing season of 2006, a study was conducted to determine the effects of modeling precipitation on seasonal patterns in ... Water is usally thought of a limiting factor for the restoration of semi-arid ecosystem. In the growing season of 2006, a study was conducted to determine the effects of modeling precipitation on seasonal patterns in concentrations of soil-available nitrogen and to describe the seasonal patterns in soil nitrogen availability and seasonal variation in the rates of net nitrogen mineralization of topsoil at Daqinggou ecological station in Keerqin sand lands, Inner Mongolia Autonomous Region, China. Manipulation of water (80 mm) was designed to be added to experiment plots of sandy grasslands in dry season. Water addition (W) treatment and control (CK) treatment were separately taken in six replications and randomly assigned in 12 plots (4 m×4 m for each) with 2-m buffers betweens. Results showed that the content of soil inorganic nitrogen and net nitrogen mineralization rate were not affected by adding water in sandy grassland of Keerqin sand lands. Net ni- trogen mineralization rates ranged from 0.5μg·g^-1,month^-1 to 4 μg.g^-1.month^-1. The highest values of soil inorganic nitrogen and net nitrogen mineralization occurred on October 15 in control plots. The seasonal changes of soil inorganic nitrogen contents exhibited "V" shape pattern that was related to seasonal patterns of soil ammonium-N (ascending trend) and nitrate-N transformation (descending trend). 展开更多
关键词 Nitrogen mineralization Inorganic nitrogen GRASSLAND Keerqin sand lands NITRIFICATION
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