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机构地区:[1]日本鹿见岛大学农学部植物营养实验室,日本鹿见岛890-0065 [2]广东省生态环境与土壤研究所//广东省农业环境综合治理重点实验室,广东广州510650
出 处:《生态环境》2008年第1期368-376,共9页Ecology and Environmnet
摘 要:为研究水田土壤中氮的行为,施给^15NH4^+或^15NO3^-标记的硝胺(NH4^15NO3或^15NH4NO3)的沙壤土(Shirasu soil)添充在根箱里,对Japonica水稻(品种Hinohikari)进行温室栽培6周。收割后,水稻植株分地上部和根部,对各自的全氮,^15N atom%进行测定。根箱各区域的土壤按着鲜土形态进行采取后,对此全氮,NO3-N,水溶性NH4-N,KCl抽出NH4-N和其各自的^15N atom%进行测定。研究结果表明,土壤全氮含量与栽培前相比,在非根际明显降低,但在根际比非根际要高,保持了与栽培前相同的水平。土壤NO3-N浓度从非根际到根际递增,但与其栽培前相比显著地降低,在整个根箱里,施给NO3-N的79%为因脱氮而损失。土壤中NO3-N的大部分来自于土壤氮化合物,来自施肥的比例却较低,尤其是在根际。反而,施给NO3-N的残存率约仅为16%左右,但其中有机态氮所占的比率在非根际里55%~86%,在根际却达到了93%。土壤水溶性NH4-N和KCl抽出NH4-N浓度靠近根际逐渐降低,而且在非根际两者匀由1:10的比例存在,但在根际里水溶性NH4-N没被检索到。在非根际里,土壤KCl抽出NH4-N的35%~66%为来自施肥,但其比例在根际里却降到15%左右。在土壤中残存的来自施给NH4-N的氮化合物之中,有机态氮所占的比例在非根际里约为11%~65%,但在根际却达到了92%。以上结果表明,在水稻根际,氮的无机化和有机化的活性比非根际显著。Behavior of N in the rhizosphere of rice (Oryza sativa L.) plant was investigated using a rhizobox system filled with a shirasu soil applied with NH4^15NO3 or ^15NH4NO3. The rhizobox consisted of one 2-mm width center compartment(CC), five 1-mm width compartments, and one bulk compartment( BC ) on both sides of CC. Rice was sowed and grown in CC. After 6th weeks after clutivation, the soil from each compartment were collected and analyzed for contents and ^15N excess% of the soil total-N, water-soluble NO3-N, NH4-N and KCl-extractable NH4-N. The obtained results were summarized as follows: 1) The total-N content of soil decreased in all the compartments except CC compared with that before cultivation, but that of CC did not change. 2) The water-soluble NO3-N content of soil decreased remarkably in all the compartments compared with that before cultivation, and about 79% of applied NO3-N was lost from soil due to denitrification. The NO3-N content of soil slightly increased from BC toward CC. The most of NO3-N were derived from the soil N especially in the CC. 3) The contents of water-soluble NH4-N and KCl-extractable NH4-N decreased from BC toward CC and the ratio of water-soluble NH4-N to KCl-extractable NH4-N are 1:10 in all the compartments except CC which water-soluble NH4-N was not detected. 4) Mineralization of soil-N and immobilizaition of fertilizer-N were more actively at CC than in the other compartments.
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