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聚湫和淤地坝地土壤微生物生物量和群落结构垂直分布特征及其影响因素

发布时间:2018-03-15 20:38

  本文选题:微生物 切入点:群落结构 出处:《南京农业大学》2015年硕士论文 论文类型:学位论文


【摘要】:土壤微生物种类和生物量可以反映土壤生态环境所发生的变化。目前对淤地坝地土壤微生物的研究主要集中在表层土壤,对微生物在土壤剖面中分布规律的研究较少。为了弄清黄土高原土壤微生物生物量和群落结构特征的主要影响因素,本文以天然聚湫坝地和人工淤地坝地为实例,研究了微生物生物量和群落结构在土壤剖面中的垂直分布特征,讨论了它们与化学成分和机械组成之间的相关性。在此基础上,得出以下初步结论:(1)根据机械组成数据,聚漱坝地土壤剖面在垂直方向上可划分出5个沉积旋回,而淤地坝地土壤剖面可划分出25个沉积旋回。聚湫坝地土壤以砂粒为主(平均含量56.62%),淤地坝地土壤以粉砂粒为主(平均含量46.39%)。(2)聚湫坝地SOC、TN、MBC和MBN含量在垂直方向上的分布与粘粒含量基本一致,在水平方向上呈现A剖面B剖面C剖面的分布规律。淤地坝地的SOC、TN、MBC和MBN含量均呈现细颗粒层粗颗粒层的规律。(3)在聚揪坝地和淤地坝地土壤样品中分别检测出17种和20种PLFA。无论是聚湫坝地还是淤地坝地,土壤微生物均以细菌为主(分别占微生物总量的65%~75%和60%~7-J%),其次为放线菌(分别为15%~25%和10%~25%)和真菌(分别为5%-10%和12%~20%)。(4)从微生物生物量来看,聚湫坝地土壤在垂直方向上可区分出3个高值区(分别位于0-50cmm、120-140cm和220-260cm段)和3个低值区,在水平方向上则表现为A剖面B剖面C剖面。淤地坝地土壤微生物总量、细菌、真菌和放线菌生物量均呈现细颗粒层粗颗粒层的规律。(5)聚湫坝地土壤微生物多样性指数(Shannon指数、Simpson指数和Pielou指数)的变化趋势基本一致。在垂直方向上,微生物生物量高值区的Shannon指数、Simpson指数和Pielou指数基本上都高于其下的低值区。在水平方向上,三个指数均表现为A剖面B剖面C剖面。淤地坝地土壤的三个微生物多样性指数均表现为细颗粒层粗颗粒层。(6)粘粒组分是影响聚湫和淤地坝地土壤微生物生物量和群落结构的主要因素。土壤微生物总量、细菌生物量和真菌生物量与粘粒含量均具有显著的正相关关系。对于聚湫,相关性系数r分别为 0.58、0.57 和 0.62(P0.05);对于淤地坝,r 则分别为 0.94、0.97 和 0.98(P0.001)。
[Abstract]:The species and biomass of soil microorganisms can reflect the changes of soil ecological environment. In order to find out the main influencing factors of soil microbial biomass and community structure, this paper takes natural accumulation and artificial silt dam field as examples. The vertical distribution characteristics of microbial biomass and community structure in soil profile were studied, and their correlation with chemical composition and mechanical composition were discussed. In the vertical direction of soil profile, five sedimentary cycles can be divided. The soil profile of silt dam can be divided into 25 sedimentary cycles. The soil of Qiqiu dam land is mainly composed of sand (average content is 56.62%), and the soil of silt sand is the main content of silt grain (average content is 46.39%) and the content of MBN is in the vertical direction. The distribution is basically the same as the clay content. In horizontal direction, the distribution law of section C in section A, section B, and the contents of MBN and MBN in silt dam are the same as those of coarse granular layer in fine grained layer, respectively. 17 species were detected in soil samples of Ju-Pu dam area and silt dam field respectively. And 20 kinds of PLFA. whether it's the Puqiu dam or the silt dam, Most of the soil microbes were bacteria (65% and 60% of the total amount of microbes, respectively), followed by actinomycetes (15% and 10%) and fungi (5% -10% and 12% respectively) from the microbial biomass point of view. In the vertical direction, three high value areas (located between 0-50 cm ~ 140 cm and 220-260 cm) and three low value areas can be distinguished from the soil of Puqiu dam land. In the horizontal direction, they can be seen as section A, section B, section C, the total amount of soil microbes and bacteria in the silt dam. The biomass of fungi and actinomycetes showed the rule of coarse granular layer in fine grained layer. The variation trend of soil microbial diversity index Shannon index Simpson index and Pielou index was basically the same in vertical direction. The Shannon index and Pielou index in the high value area of microbial biomass are basically higher than those in the low value area under them. The three indices are all A profile B section C section and the three microbial diversity indices of silt dam soil are all shown as fine granular layer coarse granular layer. 6) the clay component is the influence of accumulation and silt dam soil microbial biomass. Major factors in community structure. Total soil microbes, There was a significant positive correlation between bacterial biomass and fungal biomass and clay content, the correlation coefficient r was 0. 58 0. 57 and 0. 62% P 0. 05, respectively, and for silt dam, r was 0. 94 0. 97 and 0. 98 P0. 001, respectively.
【学位授予单位】:南京农业大学
【学位级别】:硕士
【学位授予年份】:2015
【分类号】:S154.3

【参考文献】

相关期刊论文 前10条

1 王金成;井明博;周天林;王鑫;;黄土高原沟壑区人工沙棘林生长年限对土壤微生物组成的影响[J];干旱地区农业研究;2015年02期

2 颜艳;岳大鹏;陈宝群;李奎;刘鹏;;陕北黄土洼天然淤地坝沉积物粒度特征与降雨关系研究[J];干旱地区农业研究;2014年06期

3 李晨华;张彩霞;唐立松;熊正琴;王保战;贾仲君;李彦;;长期施肥土壤微生物群落的剖面变化及其与土壤性质的关系[J];微生物学报;2014年03期

4 弥智娟;穆兴民;赵广举;;黄土高原水蚀风蚀交错区小流域泥沙粒径的分形分析[J];水土保持研究;2014年01期

5 刘鹏;岳大鹏;李奎;;陕北黄土洼淤地坝粗颗粒沉积与暴雨关系探究[J];水土保持学报;2014年01期

6 张翔;李占斌;李鹏;;淤地坝土壤水来源与分布研究[J];西安理工大学学报;2013年01期

7 褚雅红;毕如田;刘秀珍;刘庚;;黄土丘陵沟壑区坝地土壤养分的空间变异性[J];山西水土保持科技;2012年03期

8 薛凯;杨明义;张风宝;孙喜军;;利用淤地坝泥沙沉积旋^囱菪×饔蚯质蠢穂J];核农学报;2011年01期

9 毕慈芬;左仲国;冉大川;沈梅;王略;;黄河中游淤地坝淤积泥沙级配组成分析[J];人民黄河;2011年01期

10 李莉;李聚方;孙维营;黄静;陈江南;史学建;;韭园沟流域典型淤地坝淤粗排细作用研究[J];中国水土保持;2010年09期

相关博士学位论文 前1条

1 包耀贤;黄土高原坝地和梯田土壤质量特征及评价[D];西北农林科技大学;2008年

相关硕士学位论文 前1条

1 闵红;黄土丘陵区生态恢复过程土壤微生物及酶活性演变特征[D];西北农林科技大学;2007年



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