img

Wechat

  • CN 62-1070/P
  • ISSN 1000-694X
  • Bimonthly 1981
Adv search

Effects of Vegetation Restoration on Soil Microbial Biomass and Activity in Desert Area

  • Shi Wanli ,
  • Wang Hui ,
  • Ma Weiwei
Expand
  • Forestry College, Gansu Agricultural University, Lanzhou 730070, China

Received date: 2016-11-05

  Revised date: 2017-01-13

  Online published: 2017-05-20

Abstract

Soil microbes play a key role in the functioning and nutrients cycling of ecosystem, and soil microbial parameters are commonly used as indicators of soil quality changes after revegetation of degraded lands. The dynamics processes and seasonal patterns of soil microbial biomass and activity were investigated based on a chronosequence sampling, the results showed that: soil microbial biomass carbon (MBC) and nitrogen (MBN) and basic respiration (BR) were greater in revegetation area than those in mobile sand dunes. In general, for the same soil layer, MBC, MBN and BR increased with the lapse of time after revegetation, while for the same vegetation age, they decreased with the increase of soil depth. Soil microbial metabolic quotient (qCO2) showed a declining trend as time goes on, but increased with soil depth. MBC, MBN and BR showed distinctive seasonal patterns, they were in the order: summer> autumn> spring> winter, and the amplitudes of seasonal variation increased with the plantation age, which were the results of combined effects of several environmental factors. No statistical seasonally variations were found for qCO2. In comparison with soil physiochemical properties, soil microbial biomass and the activities recovered much more rapidly, which means that microbial parameters can reflect soil quality changes after restoration of desertified regions.

Cite this article

Shi Wanli , Wang Hui , Ma Weiwei . Effects of Vegetation Restoration on Soil Microbial Biomass and Activity in Desert Area[J]. Journal of Desert Research, 2017 , 37(3) : 507 -513 . DOI: 10.7522/j.issn.1000-694X.2017.00005

References

[1] 王少昆,赵学勇,张铜会,等.造林对沙地土壤微生物的数量、生物量碳及酶活性的影响[J].中国沙漠,2013,33(2):529-535.
[2] 国家林业局.中国荒漠化与沙化状况公报[R].2015.
[3] Li X J,Li X R,Wang X P,et al.Changes in soil organic carbon fractions after afforestation with xerophytic shrubs in the Tengger Desert, northern China[J].European Journal of Soil Science,2016,67(2):184-195.
[4] Mummey D L,Stahl P D,Buyer J S.Microbial biomarkers as an indicator of ecosystem recovery following surface mine reclamation[J].Applied Soil Ecology,2002,21(3):251-259.
[5] Wu Z T,Wu J J,Liu J H,et al.Increasing terrestrial vegetation activity of ecological restoration program in the Beijing-Tianjin Sand Source Region of China[J].Ecological Engineering,2013,52:37-50.
[6] Singh K,Pandey V C,Singh B,et al.Ecological restoration of degraded sodic lands through afforestation and cropping[J].Ecological Engineering,2012,43(3):70-80.
[7] An S S,Huang Y M,Zheng F L.Evaluation of soil microbial indices along a revegetation chronosequence in grassland soils on the Loess Plateau,Northwest China[J].Applied Soil Ecology,2009,41(3):286-292.
[8] 刘艳梅,杨航宇,李新荣.生物土壤结皮对荒漠区土壤微生物生物量的影响[J].土壤学报,2014,51(2):394-401.
[9] Chodak M,Pietrzykowski M,Niklinska M.Development of microbial properties in a chronosequence of sandy mine soils[J].Applied Soil Ecology,2009,41(3):259-268.
[10] 贾国梅,方向文,刘秉儒,等.黄土高原弃耕地自然恢复过程中微生物碳的大小和活性动态[J].中国沙漠,2006,26(4):580-584.
[11] 陈鸿洋,尚振艳,傅华,等.荒漠区不同大小灌丛周围土壤微生物生物量及活性特征[J].草业学报,2015,24(2):70-76.
[12] Vance E D,Brookes P C,Jenkinson D S.An extraction method for measuring soil microbial biomass C[J].Soil Biology & Biochemistry,1987,19(6):703-707.
[13] Blake G R,Hartge K H.Bulk density.Methods of Soil Analysis.Part 1.Physical and Mineralogical Methods[M]//Klute A.Agronomy Monograph.Madison,USA:American Society of Agronomy,1986:363-376.
[14] 王少昆,赵学勇,黄文达,等.科尔沁沙质草地纤维素分解菌的筛选、鉴定及其分解能力[J].中国沙漠,2015,35(6):1584-1591.
[15] 王晓朦,乌云娜,宋彦涛,等.放牧对克氏针茅(Stipa krylovii)草原土壤物理、化学及微生物性状的影响[J].中国沙漠,2015,35(5):1193-1199.
[16] 张云舒,范燕敏,武红旗,等.封育对山地荒漠土壤微生物量碳及养分的影响[J].草业科学,2014,31(5):797-802.
[17] 靳正忠,雷加强,徐新文,等.流沙区不同立地条件下防护林土壤微生物多样性分析[J].中国沙漠,2011,31(6):1430-1436.
[18] 李香真,曲秋皓.蒙古高原草原土壤微生物量碳氮特征[J].土壤学报,2002,39(1):97-104.
[19] 陈隆亨,李福兴,邸醒民.中国风砂土[M].北京:科学出版社,1998.
[20] 黄刚,赵学勇,苏延桂,等.科尔沁沙地樟子松人工林对微环境改良效果的评价[J].干旱区研究,2008,25(2):212-218.
[21] 王新平,李新荣,张景光,等.沙漠地区人工固沙植被对土壤温度与土壤导温率的影响[J].中国沙漠,2002,22(4):344-349.
[22] Wardle D A,Ghani A.A critique of the microbial metabolic quotient (qCO2) as a bioindicator of disturbance and ecosystem development[J].Soil Biology and Biochemistry,1995,27(12):1601-1610.
[23] 赵吉,杨劼,邵玉琴.退化草原土壤健康的微生物学量化评价[J].农业环境科学学报,2007,26(6):2090-2094.
[24] 管海英,王权,赵鑫,等.两种典型荒漠植被区土壤微生物量碳的季节变化及影响因素分析[J].干旱区地理,2015,38(1):67-75.
[25] 曹成有,陈家模,邵建飞,等.科尔沁沙地四中固沙植物群落土壤微生物量及酶活性的季节动态[J].生态学杂志,2011,30(2):227-233.
[26] Li X J,Li X R,Song W M,et al.Effects of crust and shrub patches on runoff,sedimentation,and related nutrient (C,N) redistribution in the desertified steppe zone of the Tengger Desert,Northern China[J].Geomorphology,2008,96:221-232.
[27] 杨涛,徐慧,李慧,等.樟子松人工林土壤养分、微生物及酶活性的研究[J].水土保持学报,2005,19(3):50-53.
Outlines

/