首页> 外文期刊>Journal of Agriculture and Ecology Research International >The Effect of Soil Physical Properties and Soil Microclimate on Rodent Burrowsa€? Abundance and their Characteristics in Western Usambara Mountains, Tanzania
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The Effect of Soil Physical Properties and Soil Microclimate on Rodent Burrowsa€? Abundance and their Characteristics in Western Usambara Mountains, Tanzania

机译:土壤物理性质和小气候对啮齿类动物洞穴的影响坦桑尼亚西部乌桑巴拉山脉的丰度及其特征

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The present study was carried out between September 2009 and June 2013 in Western Usambara Mountains plague focus with the aim of establishing the influence of selected soil physical properties and soil microclimate on rodent burrows’ abundance, portal orientation and use. Two landscapes with high and medium plague frequencies in Lokome and Lukozi villages were studied. In the two landscapes data were collected from 117 and 200 observation sites respectively, using 100 m x 200 m quadrats. At each quadrat crossing, a sample quadrat of 20 m x 20 m was demarcated for scanning rodent burrows whereby burrows encountered were counted and their portal orientation and burrow use described. Within each sample quadrat, selected soil physical properties including thickness of the soil genetic horizons and soil dry consistence were determined. Soil samples were collected from each horizon for laboratory texture analysis. Temperature (surface and subsurface to a depth 10 cm) and relative humidity at a depth of 10 and 30 cm were collected using infrared, thermo-couple thermometers and i -Buttons. Descriptive statistics, ANOVA and logistic regression were used to analyse the data by R-software. There were significant ( P =.0001) differences between the two landscapes regarding topsoil depth, infrared temperature, relative humidity and rodent burrows’ abundance. In the high plague frequency landscape there was a significant influence ( P =.05) of topsoil horizon thickness on rodent burrows’ abundance and use. Results also indicate that soil temperature to a depth of 10 cm was significantly ( P =.05) correlated with rodent burrow use. Likewise, in the medium plague frequency landscape, soil physical properties and soil microclimate significantly ( P =.0001) discouraged rodent burrowing. It was concluded that soil physical and soil microclimate encouraged and discouraged burrowing in the high and the medium plague frequency landscapes, respectively. The landscape with high rodent burrows’ abundance corresponded with high plague frequency records.
机译:本研究于2009年9月至2013年6月在西部乌桑巴拉山脉鼠疫重点地区进行,目的是确定选定的土壤物理性质和土壤小气候对啮齿类动物洞穴的丰度,门户定位和使用的影响。研究了Lokome和Lukozi村庄中鼠疫频率高和中的两种景观。在这两个景观中,分别使用100 m x 200 m的四边形分别从117个和200个观察点收集了数据。在每个样方交叉处,划出一个20 m x 20 m的样方,以扫描啮齿类动物的洞穴,从而对遇到的洞穴进行计数,并描述其入口方向和洞穴的使用。在每个样方中,确定了选定的土壤物理特性,包括土壤遗传层的厚度和土壤干稠度。从每个视野收集土壤样品用于实验室质地分析。使用红外,热电偶温度计和i-Button收集温度(表面和地下深度为10厘米)和10和30厘米深度的相对湿度。描述性统计,ANOVA和逻辑回归用于通过R-software分析数据。在表层土壤深度,红外温度,相对湿度和啮齿动物洞穴的丰度方面,两个景观之间存在显着差异(P = .0001)。在鼠疫高频率的景观中,表土层的水平厚度对啮齿动物洞穴的丰度和利用有显着影响(P = .05)。结果还表明,土壤温度达到10 cm深度与啮齿类动物的洞穴使用量显着相关(P = .05)。同样,在中鼠疫频率景观中,土壤物理性质和土壤小气候显着(P = .0001)阻止了啮齿类动物的穴居。得出的结论是,在高和中鼠疫频率景观中,土壤物理和土壤小气候分别鼓励和抑制了洞穴的产生。啮齿类动物穴居丰富的地貌与鼠疫频密记录相吻合。

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