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首页> 外文期刊>Fresenius Environmental Bulletin >EFFECT OF RECLAMATION ON MICROBIAL BIOMASS AND ACTIVITY IN PEAT MIRE SOIL AROUND XINGKAI LAKE IN NORTHEAST CHINA
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EFFECT OF RECLAMATION ON MICROBIAL BIOMASS AND ACTIVITY IN PEAT MIRE SOIL AROUND XINGKAI LAKE IN NORTHEAST CHINA

机译:复垦对东北兴凯湖周围泥质土壤微生物生物量和活性的影响

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摘要

Over the past few decades, many natural wetlands around Xingkai Lake have been converted to soybean or paddy fields; little is known about how such conversion affects soil microorganisms. This study investigated influence of reclaiming wetland to soybean or paddy field on microbial biomass and activity in peat mire soil around the lake. After reclamation, in 0-5 cm, 5-10 cm, 10-20 cm and 20-30 cm soil layers microbial biomass and activities decreased due to reclamation. MBC (Microbial Biomass Carbon), MBN (Microbial Biomass Nitrogen), MBC/MBN, BR (Basal Respiration) all decreased. But before and after reclamation, microbial biomass decreased with soil depth, seasonal variations of microbial biomass and MBC/MBN were similar, higher in May to June than those in July to September. In 0-5 cm and 5-10 cm topsoil layers in May to July, qCO(2)(Respiration Quotient-qCO(2)) was higher in soybean field than that in paddy field and wetland, both were in water logging; while in August and September logging water was drained up, qCO(2) in paddy field increased dramatically to be higher than that in soybean field and wetland. In 10-20 cm and 20-30 cm subsoil layers, qCO(2) were higher in wetland and paddy field than that in soybean filed from May to September. Changes of plant type, litter amount and quality derived from reclamation influenced the microbial biomass and activity seriously. Moreover, situation of water logging was found to be the key factor influencing microbial activity.
机译:在过去的几十年中,兴凯湖周围的许多自然湿地已经转变为大豆田或稻田。对于这种转化如何影响土壤微生物知之甚少。这项研究调查了开垦湿地对大豆或稻田对湖周围泥炭沼泽土壤微生物生物量和活性的影响。开垦后,由于开垦,在0-5 cm,5-10 cm,10-20 cm和20-30 cm的土壤层中,微生物生物量和活性下降。 MBC(微生物生物质碳),MBN(微生物生物质氮),MBC / MBN,BR(基础呼吸)均下降。但是在开垦前后,微生物量随土壤深度的增加而降低,微生物量和MBC / MBN的季节变化相似,5月至6月高于7月至9月。在5月至7月的0-5 cm和5-10 cm表土层中,大豆田的qCO(2)(呼吸商-qCO(2))高于稻田和湿地,都处于涝渍状态。而在8月和9月,排干了测井水,稻田的qCO(2)急剧增加,高于大豆田和湿地。在10-20厘米和20-30厘米的底土层中,湿地和稻田的qCO(2)高于5月至9月提交的大豆。开垦引起的植物类型,凋落物数量和质量的变化严重影响了微生物的生物量和活性。此外,发现涝灾情况是影响微生物活性的关键因素。

著录项

  • 来源
    《Fresenius Environmental Bulletin》 |2015年第3b期|1098-1107|共10页
  • 作者单位

    Minist Agr, Agroenvironm Protect Inst, Tianjin 300191, Peoples R China;

    Chinese Acad Sci, Northeast Inst Geog & Agr Ecol, Key Lab Wetland Ecol & Environm, Changchun 130012, Peoples R China;

    Chinese Acad Sci, Northeast Inst Geog & Agr Ecol, Key Lab Wetland Ecol & Environm, Changchun 130012, Peoples R China;

    Chinese Acad Sci, Northeast Inst Geog & Agr Ecol, Key Lab Wetland Ecol & Environm, Changchun 130012, Peoples R China;

  • 收录信息
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Microbial activity; Microbial biomass; Peat mire soil; Reclamation; Wetland;

    机译:微生物活性;微生物量;泥炭土;开垦;湿地;

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