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内蒙古典型草原不同放牧强度下土壤微生物与土壤肥力关系的研究
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摘要
本文以位于内蒙古自治区赤峰市克什克腾旗西部,达里诺尔自然保护区内的典型草原为研究对象,将典型草原划分为四个不同放牧强度,分析了草原生态系统中主要土壤微生物类群数量、微生物生物量、土壤酶活性和土壤理化因子等的季节动态变化、它们之间的相关性以及放牧强度对他们的影响。旨在为草地土壤肥力科学评价提供微生物方面的科学依据。主要研究结果如下:
     1.内蒙古典型草原土壤中各类群微生物数量有一定差异,其数量关系是细菌﹥氨化菌﹥自生固氮菌﹥放线菌﹥反硝化细菌﹥真菌﹥硝化细菌;对照区、轻牧区、中牧区土壤微生物总数在各季节均高于重牧区;土壤微生物总数的大小顺序为:8月(夏)>10月(秋)>5月(春)>3月(冬)。
     2.土壤微生物生物量受放牧强度和季节变化影响很明显。轻牧区微生物生物量碳、氮含量均高于其它样区,微生物生物量碳、氮的含量在8月(夏)、10月(秋)相对较高。
     3.各种酶活性的变化受放牧强度和季节的综合影响。对照区和轻度放牧区降低了土壤多酚氧化酶的活性,而保持较高的脲酶、过氧化氢酶、蛋白酶活性。重度放牧则增加了多酚氧化酶活性,而脲酶、过氧化氢酶、蛋白酶活性明显降低。
     4.不同放牧强度下土壤呼吸强度整体上表现出随着放牧强度的增加而减小的趋势,且差异极显著。
     5.随着放牧强度的增大,土壤含水量降低,pH值升高,有机质、速效氮含量降低。
     6.相关性分析表明,不同放牧强度下微生物总数、各类群微生物数量分别与土壤微生物生物量碳、氮呈显著或极显著正相关,表明土壤微生物是土壤质量评价中的一项重要指标。另外,土壤生态系统中土壤微生物与土壤酶、土壤养分之间相互依存,相互影响。
The paper studies on the typical steppe inside Dalinuoer National Nature Reserve, west of Keshenketeng County in ChiFeng Inner Mongolian. The typical grassland shall be divided into four parts with different grazing intensities; this study analyses the seasonal change , inter-relationship and over-grazing impacts on the specimen quantity of main soil microorganism, soil microbial biomass of microorganism, activity of soil enzyme and soil physical-chemical factors etc in grassland ecosystem. Its aim is to provide the scientific basis in microorganism respect for the grassland soil fertility scientific assessment.
     1. The quantity of various microorganism varies to some extent in the Inner Mongolia steppe, their quantity relationship ranks as bacteria﹥ammonifier﹥nitrogen fixating bacteria﹥actinomyces﹥Denitrifying bacteria﹥fungi﹥nitrobacteria; The total quantity of soil microorganism in control area, light grazing, and heavy grazing is more than that of heavy grazing area; the total quantity of soil microorganism ranks as August(Summer)>October(Autumn)>May(Spring)>March(Winter).
     2. The soil microbial biomass has the distinct reaction under the impact of grazing intensity and seasonal change. The soil microbial biomass in light grazing area has higher percentage of soil microbial biomass carbon and soil microbial biomass nitrogen than that in other areas. The percentage of soil microbial biomass carbon and soil microbial biomass nitrogen is relatively high in August (summer) and October (winter).
     3. The soil enzymatic activities are diverse under the comprehensive impacts of grazing intensity and seasonal change. The control area and light grazing area is with low activity of oil polyphenol oxidase and high activity of soil urease, catalase, and protease. However, heavy grazing area is with increased polyphenol oxidase activity and drastically reduced soil urease, catalase, and protease.
     4. Under different grazing intensity, soil respiration intensity represents the trend of decreasing as the increase of grazing intensity; in addition, the change is obvious.
     5. With the increase of grazing intensity, the water percentage in soil will decrease with corresponding increasing of PH and decreasing of soil organic matter content and alkaline-N.
     6. The relative analysis shows that under different grazing intensity, the total quantity of soil microorganism, the quantity of various microorganisms has obvious and much obvious relationship with soil microbial biomass carbon and soil microbial biomass nitrogen respectively. Moreover, soil microorganism and soil enzyme in soil ecosystem is inter-independent and interact ional.
引文
[1]侯扶江,杨中艺.放牧对草地的作用[J].生态学报,2006,26(1):244-250.
    [2]龙章富,刘世贵,葛绍荣.退化草地土壤生化活性研究[J].草地学报,1994,2(2):59-62.
    [3]王娟谷,雪景,赵吉.羊草草原土壤酶活性对土壤肥力的指示作用[J].农业环境科学学报,2006,25(4):934-938.
    [4]高雪峰,韩国栋,张功.荒漠草原不同放牧强度下土壤酶活性及养分含量的动态研究[J].农业环境科学学报,2007,24(2):11-13.
    [5]陈佐忠,汪诗平等.中国典型草原生态系统[M].北京:科学出版社,2000,155-161.
    [6]田有国.基于 GIS 的全国耕地质量评价方法及应用[D].武汉:华中农业大学,2003:
    [7]赵其国.发展与创新现代土壤科学[J].土壤学报,2005,40(3):321-324.
    [8]安韶山.黄土丘陵区土壤肥力质量对植被恢复的响应及其演变[D] .陕西:西北农林科技大学,2004:
    [9]孟立君.设施不同种植年限土壤酶活性及其与土壤肥力关系的研究[D].哈尔滨:东北农业大学,2004:
    [10]刘晓冰,邢宝山.土壤质量及其评价指标[J].农业系统科学与综合研究,2002,18(2):109-111.
    [11]孙波,赵其国.红壤退化中的土壤质量评价指标及评价方法[J].地理科学进展,1999,18(2):199-122.
    [12]何跃军,钟章成,刘济明.石灰岩退化生态系统不同恢复阶段土壤酶活性研究[J].应用生态学报,2005,16(6):1077-1080.
    [13]吕秀华.东北羊草草原不同生境土壤微生物与土壤理化性质关系研究[D].哈尔滨:东北师范大学,2003:
    [14]郭继勋,祝廷成.羊草草原土壤微生物的数量和生物量[J].生态学报,1997,17(1):79-81.
    [15]ColeL C. Protect the friendly microbes,Fragilebreathoflife[M].1966:46~47.
    [16]Clark F Eand Pawl EA.The microfloraof grassland,Adv Agron[J],1970,22:375~435.
    [17]马爽.陇东典型草原不同载畜量下土壤微生物与草地退化相关性研究[D] .兰州:甘肃农业大学,2004:
    [18]王海英,宫渊波,龚伟.不同林分土壤微生物、酶活性与土壤肥力的关系研究综述[J].四川林勘设计,2005,3:9-12.
    [19]樊军,郝明德.长期轮作施肥对土壤微生物碳氮的影响[J].水土保持研究,2003,10(1):85-86.
    [20]Nannipieri,P.,Pedrazzini,F.,Arcara,P.G. and Piovanelli, C. Changes in amino acids, enzyme activities and biomass during soil microbial growth[J].Soil Sci.1979,127:26-34.
    [21]程东娟.冀西北高原土壤酶活性及肥力因素动态变化研究[D].保定:河北农业大学,2001:
    [22]季立声,王一川.山东省主要土壤酶活性与土壤肥力[J].山东农业大学学报,1990,21(2):37-42.
    [23]曹慧,孙辉.土壤酶活性及其对土壤质量的指示研究进展[J].应用与环境生物学报,2003,9(1):105-109.
    [24]杨芳.川西亚高山森林土壤微生物和酶活性分布特征研究[D].重庆:西南农业大学,2004:
    [25]Zhang J-E. scope and content of study on soil biodiversity and its sustainable exploitation. Chin Biodivers, 1999,7(2):140-144.
    [26]Holt J A,Hodgen M J,Lamb D.,Soil respiration in the seasonally dry tropics near Townsville,North Queensland.,Aust.J.Soil Res,1990,28:737-745.
    [27]Hendriksen N B,Edwards C A.,Earthworm effects on respiratory activity in a dung soil system [J].Soil Biol.,1997,29(3-4):347-351.
    [28]Laura E.,Scott-Denton,et al.,Spatial and temporal controls of soil respiration of soil respiration rate in a high-elevation,subalpine forest[J].Soil Biology & Biochemistry,2003,35:525-534.
    [29]张金霞,曹广民,周党卫.草毡寒冻雏形土 CO2 释放特征[J].生态学报,2001,21(4):544-549.
    [30]王娓,周晓梅,郭继勋.东北羊草草原两种主要群落环境因素对土壤呼吸贡献量的影响[J].草业学报,2002,01:12-16.
    [31]李凌浩,陈佐忠,草地群落的土壤呼吸[J].生态学杂志,1998,17(4):45-51.
    [32]David C,Mark D,John H.Soil respiration from four aggrading forested watersheds measured over a quarter century[J].Forest Ecology and Management,2002,157:247-253.
    [33]高安社.羊草草原放牧地生态系统健康评价[D].呼和浩特:内蒙古农业大学,2005:
    [34]Smith Stanley D,Travis E.Huxman,et al.Elevated CO2 increases productivity and invasive speciessuccess in an arid ecosystem[J].Nature,2000,408:79~81.
    [35]Priess J A,Koning G H J de Veldkamp A. Assessment of interactions between land in change andcarbon and nutrient fluxes in Ecuador[J].Ecosystems & Environment,2001,85:269~279.
    [36]王艳芬,陈佐忠,Larry TT.人类活动对锡林郭勒地区主要草原土壤有机碳分布的影响[J].植物生态学报,1998,22(6):545-551.
    [37]阮晓红,张瑛,黄林楠.微生物在湿地氮循环系统的效应分析[J].水资源保护,2004,6:3-5.
    [38]周志华,肖化云,刘从强.土壤氮素生物地球化学循环的研究现状与进展[J].地球与环境,2004,32(3-4):21-24.
    [39]李金花,李镇,任继周.放牧对草原植物的影响[J].草业学报,2002,11(1):4-8.
    [40] 王 岩 , 沈 其 荣 , 史 瑞 和 . 土 壤 微 生 物 生 物 量 及 其 生 态 效 应 [J] 南 . 京 农 业 大 学 学报,1996,19(4):45~51.
    [41]裴海昆.不同放牧强度对土壤养分及质地的影响[J].青海大学学报,2004,22(4):29-31.
    [42]杨智明.不同放牧强度对荒漠草原植被影响的研究[D].银川:宁夏大学,2004:
    [43] 王 东 波 , 陈 丽 . 放 牧 对 草 地 生 态 系 统 土 壤 理 化 性 质 的 影 响 [J]. 内 蒙 古 科 技 与 经济,2006,6:105-106.
    [44]高英志,韩兴国,汪诗平.放牧对草原土壤的影响[J].生态学报,2004,(24):79-83.
    [45]曹成有,朱丽辉,富瑶.科尔沁沙质草地沙漠化过程中土壤生物活性的变化[J].生态学杂志,2007,26(5):622-625.
    [46] 赵哈林 , 赵学勇 , 张铜会.2002. 北方农牧交错区沙漠化的生物过程研究 [J].中国沙漠,22(4):309-316.
    [47]赵哈林.科尔沁沙地两种主要群落的沙漠化演变特征研究[J].中国沙漠,1993,13(3):47-52.
    [48]赵吉、刘萍、邵玉琴.人为因素对草原土壤微生物和生物活性的影响[J].内蒙古大学学报,1996,27(4):568-572.
    [49]内蒙古农牧学院.草原管理学(第二版)[M].北京:农业出版社,1991:89-93.
    [50]内蒙古自治区统计局.内蒙古统计年鉴[M].北京:中国统计出版社,2000:203~227.
    [51]中国植被编辑委员会.中国植被[M].北京:科学出版社,1980:113-114.
    [52]中国科学院内蒙古宁夏综合考察队.内蒙古植被[M].北京:科学出版,1985:405-408.
    [53]沈萍,范秀容,李广武.微生物学实验[M].北京:高等教育出版社,1999:49-95.
    [54]鲁如坤.土壤农业化学分析方法[M].北京:中国农业科技出版社,1999:1-247.
    [55] 徐继荣 , 王友绍 , 孙松.海岸带地区的固氮、氨化、硝化与反硝化特征 [J].生态学报,2004,24(12):2908-2909.
    [56]徐选旺.氮循环浅析[J].生物学通报,2001,36(5):20.
    [57]山西省原平农业学校.农业微生物学[M].北京:农业出版社,1984:172-173.
    [58]窦新田.生物固氮[M].北京:农业出版社,1989,117.
    [59]徐平.氮循环与固氮[J].中学生物学,2005,21(3):11.
    [60]LilburnTG,KimKS,OstromNE,etal.Nitrogenfixationbysymbioticandfree2Livingspirochetes[J].Science,2001,292:2495~2498.
    [61]KarlD,LetellerR,TupasL,etal.TheroleofnitrogenfixationinbiogeochemicalcyclinginthesubtropicalNorthPacificOcean[J].Nature,1997,388:533~538.
    [62]SnoeckD,ZapataF,DomenachAM,etal.Isotopicevidenceofthetransferofnitrogenfixedbylegumestocoffeetrees[J].Biotechno.Agron.Soc.Environ,2000,4(2):95~100.
    [63]山西省原平农业学校.农业微生物学[M].北京:农业出版社,1984:187.
    [64]Zhou,C.P.&H. Ouyang.Temperature and moisture effects on soil nitrogen mineralization in deciduous broad-leaved forest. Acta Phyto ecological Since[J],2001,25:204~209.
    [65]Lin,B.Q.Liu,Y.Wu,H. He,Y.K.Qiao. Dynamics of litters in artificial restoration process of subalpine coniferous forest. Chinese Journal of Applied Ecology [J].2004,15(9):1491~1496.
    [66]Berg,MP,H.A.Verhoef,T.Bolger,J.M.Anderson,FBeese,M.M.Couteaux,P.Ineson,F.McCarthy,L.Palka,M.Raubuch,PSplatt & T.Willison. Effects of air pollutant-temperature interactions on mineral-Ndynamics and cation leaching in replicate forest soil transplantation experiments. Biogeochemistry[J].1997,39:295~326.
    [67]刘义.川西亚高山针叶林土壤的硝化和反硝化作用研究[D].成都:中国科学院成都生物研究所,2005:
    [68]关世英,常金宝,贾树海.草原栗钙土退化过程中的土壤性状及其变化规律的研究[J].中国草地,1997,(3):39-43.
    [69]姚爱兴,王培,夏景新等.不同放牧强度下奶牛对多年生黑麦草/白三叶草地土壤特性的影响[J].草地学报,1995,3(3):181-189.
    [70]付华,王彦荣,吴彩霞,塔拉腾.放牧对阿拉善荒漠草地土壤性状的影响[J].中国沙漠,2002,22(4):341-342.
    [71]李灵.不同退化林地土壤微生物生物量动态[D].福州:福建农业大学,2004:
    [72]David C,Mark D,John H.Soil respiration from four aggrading forested watersheds measured over a quarter century[J].Forest Ecology and Management,2002,157:247-253.
    [73]马丽萍.天祝高寒草地不同扰动生境土壤微生物数量时空动态研究[D].兰州:甘肃农业大学,2004:

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