15N交叉标记有机与无机肥料氮的转化与残留
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国家科技支撑计划项目(2007BAD87B11);中国科学院知识创新工程项目(KZCX3-SW-441); 湖南省重点学科-环境科学学科建设项目,中南林业科技大学人才引进计划项目


Nitrogen transformation and its residue in pot experiments amended with organic and inorganic 15N cross labeled fertilizers
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    摘要:

    有机无机肥配施能够培肥土壤,改善土壤氮素供给,但目前有机无机肥配施主要集中在化肥氮的研究,忽略秸秆氮对化肥氮转化的影响。为了解秸秆还田对不同氮源转化和残留的影响,采用15N对尿素和水稻秸秆进行交叉标记,在两种不同肥力水稻土 (粘土矿物类型为1 ∶ 1型红黄泥和2 ∶ 1型紫潮泥) 进行水稻盆栽试验。设置对照(CK),单施尿素(15NU)、标记尿素与稻草配施(15NU-S) 和标记稻草与尿素配施(15NS-U)4个处理。结果表明,水稻吸收的氮素60%以上来自土壤氮,土壤氮素肥力相对较低的红黄泥较之紫潮泥对肥料氮的依赖更强;水稻生长期间微生物同化的尿素氮占标记底物的百分数红黄泥为1.8%-8.3%,紫潮泥为1.8%-19.2%;微生物同化的秸杆氮占标记底物的百分数红黄泥为1.7%-5.0%,紫潮泥为2.0%-6.2%。而粘土矿物固持的尿素氮占标记底物的百分数,红黄泥为0.3%-2.1%,紫潮泥为3.5%-18.7%;粘土矿物固持的秸杆氮红黄泥为0.2%-0.9%,紫潮泥为1.7%-5.0%。水稻成熟期尿素氮的残留率,红黄泥15NU处理、15NU+S分别为14.5%和17.0%,紫潮泥分别为16.9%和17.1%。秸秆氮的残留率分别为红黄泥38.8%、紫潮泥41.5%;有机无机肥配施提高了微生物同化化肥氮的能力,降低了粘土矿物晶格固持化肥氮的水平。有机无机配施提高了化肥氮利用率同时,提高了有机形态氮残留,降低了无机形态氮(矿质氮+固定态铵)的残留。

    Abstract:

    Application of chemical fertilizer incorporated with rice straw can improve soil fertility and N supply. In most of such experiments, however, attention was mainly paid to the function of chemical fertilizers while the effect of the straw N on the transformation of N from chemical fertilizers was to certain extent neglected. In order to investigate the effect of rice straw application on the transformation and residue of N from different fertilizers, pot experiments with two different types of soils (Reddish yellow clayey soil, 1 ∶ 1 type, low fertility level and Purple alluvial clayey soil, 2:1 type, high fertility level) were conducted by applying the 15N cross labeled technique with urea and rice straw as the N sources. The designed experiments included four treatments and 8 replications (total 64 pots including pots for sampling): the control (CK with no N application), labeled urea (15NU), combination of labeled urea and rice straw powder (15NU-S) and the combination of labeled rice straw power and urea (15NS-U). The results obtained from the experiments indicated that the uptake rate of the soil native N by rice exceeded 60% while that of the applied N in the low fertility level soil (Reddish clayey soil) was higher than in the high fertility level soil (Purple alluvial soil). During the rice growth period, the assimilation percentages of the labeled urea N by microorganism in reddish clayey and purple alluvial soils were 1.8%-8.3% and 1.8%-19.2%, respectively, while those of the labeled rice straw N in these two types of soils were 1.7%-5.0% and 2.0%-6.2%, respectively. The fixation percentages of the labeled urea N by soil clay were 0.3%-2.1% and 3.5%-18.7% while those of the labeled rice straw N were 0.2%-0.9% and 1.7%-5.0% in reddish clayey and purple alluvial soils, respectively,. The residue percentages of the labeled urea N of 15NU in reddish clayey soil and purple alluvial soil and were 14.5% and 16.9% respectively; while those of 15NU+S in both soils were 17%. The residue percentage of the rice straw N in reddish clayey soil and purple alluvial soil were 38.8% and 41.5%, respectively. In conclusion, the combined application of urea and rice straw increased the assimilation rate of urea N by microorganism and decreased the fixation level of urea N by soil clay. In addition, the combined application increased both the N uptake rate by crops and the residue quantity of organic N from exogenous N associated with decreased inorganic N residue from exogenous N.

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彭佩钦,仇少君,侯红波,李恩尧,丘亚群.15N交叉标记有机与无机肥料氮的转化与残留.生态学报,2011,31(3):858~865

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