| 黄土丘陵区生物结皮条件下土壤有机质及 氮素的累积特征 |
| 姚春竹1,2; 赵允格2; 王媛1,2; 张培培2,3
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| 2014
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发表期刊 | 西北农林科技大学学报(自然科学版)
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卷号 | 42期号:6页码:197-204 |
摘要 | 【目的】研究生物结皮条件下土壤有机质及不同形态氮素含量的变化,明确生物结皮养分积累及培
肥土壤的作用,为其潜在的环境风险评价提供依据。【方法】采用野外调查结合室内分析的方法,调查黄土丘陵区不
同发育年限生物结皮的样地,分层采集样地的土壤样品,同时以同一区域退耕1年以内的撂荒地为对照(CK),测定生
物结皮层以及0~2,2~5,5~10cm土层有机质、全氮及碱解氮、硝态氮、铵态氮含量。【结果】1)生物结皮条件下,结
皮层土壤全氮和有机质的积累过程可分为快速增长和趋于稳定2个阶段,这2个阶段以生物结皮发育13年为界限。
结皮发育13年时,结皮层土壤全氮含量达到1.34g/kg,是对照的3.72倍;有机质含量为25.41g/kg,是对照的5.05
倍。2)生物结皮明显增加了结皮层土壤碳氮比,结皮发育15年时,结皮层土壤的碳氮比最高,为11.8,但碳氮比与发
育年限无关。3)结皮层土壤碱解氮含量及其占全氮的比例明显高于0~10cm土壤和对照,碱解氮含量在生物结皮发
育15年时达到最大值(94.89mg/kg),是对照的6.51倍,之后趋于稳定。4)生物结皮增加了结皮层土壤硝态氮和铵
态氮的含量以及硝铵比。【结论】生物结皮可以明显提高结皮层土壤氮素含量,增加土壤肥力,对土壤表层氮素积累
有重要作用,与此同时,生物结皮也有可能增加氮素的流失风险。 |
其他摘要 | 【Objective】This study explored the changes of soil organic matter and nitrogen with biological
soil crusts(BSCs),to understand the nutrient accumulation and the soil fertility ability of the BSCs,
and provide reference for assessing the potential environmental risks.【Method】Through field survey combined
with laboratory analysis,soil samples from crusts,and soil layers of 0-2cm,2-5cm,and 5-10cm
were collected from re-vegetated grasslands with BSCs at different ages in the Hilly Loess Plateau Region.
Samples from the re-vegetated grassland with age of less than one year(fresh re-vegetated grassland)were
also collected as control.Contents of soil organic matter,total nitrogen and different nitrogen componentswere measured.【Result】1)With BSCs,the accumulation of soil organic matter and total nitrogen had two
stages.After 13years of rehabilitation,the content of total nitrogen(1.34g/kg)and soil organic matter
(25.41g/kg)were 3.72and 5.05times of those of the control,respectively.Starting from 13years,the accumulation
tended to be stable.2)Soil C/N ratio was increased by BSCs with a maximum of 11.8after 15
years of rehabilitation.But the ratio was independent from the ages of BSCs.3)The content of soil alkalihydrolyzable
nitrogen,and its ratio to total nitrogen in BSCs were higher than those in soil layer of 0-10
cm and the control.After 15years of rehabilitation,the content of alkali-hydrolyzable nitrogen reached the
maximum of 94.89mg/kg,which was 6.51times of that of the control.4)Both the contents of nitrate nitrogen
and ammonium nitrogen and the ratio of nitrate nitrogen to ammonium nitrogen in BSCs were significantly
increased.【Conclusion】Biological soil crusts significantly improved soil nitrogen contents in the
crust layers,increased soil fertility,and played an important role in the nitrogen accumulation in topsoil.
However,BSCs may increase the risk of nitrogen losses in the slope land on the Hilly Loess Plateau. |
关键词 | 生物结皮
土壤氮素
有机质
累积特征
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收录类别 | 中文核心期刊要目总览
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语种 | 中文
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文献类型 | 期刊论文
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条目标识符 | sbir.nwafu.edu.cn/handle/361005/9604
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专题 | 水保所知识产出(1956---)
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作者单位 | 1.西北农林科技大学资源环境学院黄土高原土壤侵蚀与旱地农业国家重点实验室 2.中国科学院大学 3.西北农林科技大学水土保持研究所黄土高原土壤侵蚀与旱地农业国家重点实验室
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推荐引用方式 GB/T 7714 |
姚春竹,赵允格,王媛,等. 黄土丘陵区生物结皮条件下土壤有机质及 氮素的累积特征[J]. 西北农林科技大学学报(自然科学版),2014,42(6):197-204.
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APA |
姚春竹,赵允格,王媛,&张培培.(2014).黄土丘陵区生物结皮条件下土壤有机质及 氮素的累积特征.西北农林科技大学学报(自然科学版),42(6),197-204.
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MLA |
姚春竹,et al."黄土丘陵区生物结皮条件下土壤有机质及 氮素的累积特征".西北农林科技大学学报(自然科学版) 42.6(2014):197-204.
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黄土丘陵区生物结皮条件下土壤有机质及氮素的累积特征_姚春竹.pdf
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