山東省部分地區(qū)麥田土壤成分分析
[Abstract]:Soil is the main body of the earth's surface, which is formed by long-term natural erosion of rocks. It is mainly composed of many layers of minerals with different thickness. The exchange of energy in growth and ecological cycles provides abundant nutrients and water. Soils from different sources have different characteristics because they are constantly affected by physical, chemical and biological factors such as climate, early texture, microbial environment and human activities. Heterosexuality. Soil is closely related to human activities and has been used in the early years of forensic science as trace micro-evidence to analyze and judge the case. Soil has become one of the five main forms of forensic tracking evidence because of its complex and obvious regional characteristics. At present, the study of soil as trace evidence of forensic medicine has been relatively simple abroad, but no relevant research report has been found in China. This paper judges the soil by analyzing the soil composition of wheat fields in some areas of Shandong Province. Soil samples were collected from 87 wheat fields in Shandong Province before sowing in autumn. The physical, chemical and biological aspects of soil samples were studied and analyzed. The corresponding data were obtained and classified step by step. Finally, the source of soil samples was identified. Samples (blind selection), physical, chemical and biological analysis and identification, according to the data obtained from the exploratory experiment as a comparison standard, step by step to analyze the blind samples to determine whether the source of the soil samples can be accurately identified. This research method and idea can be applied to soil analysis and identification under more detailed conditions, such as wheat field soil composition analysis in different seasons, different topography and more types of soil composition in Shandong Province, thus providing a reliable method basis and method for establishing soil database covering the vast majority of Shandong Province. The main experimental methods involved in this paper are as follows: (1) Apparent method is used to analyze the properties of soil samples, mainly aiming at the color and texture of soil samples. 87 soil samples in the research system can be divided into: red: 19, yellow: 31, black 37. According to the soil texture classification of each color sample: 1. There are 10 colored sandy soils, 6 red loam soils, 3 red clay soils, 17 yellow sandy soils, 12 yellow loam soils, 2 yellow clay soils, 12 black sandy soils, 19 black loam soils and 6 black clay. The size of the sample was found to be in the range of 100-700 micron 2. Therefore, six classifications of A, B, C, D, E and F were worked out and continued to classify. (3) The chemical elements in soil samples were quantitatively analyzed by energy dispersive spectroscopy. The main chemical elements were Na, Mg, Al, Fe and so on. According to the characteristics of element content in the samples, the samples were analyzed and identified. Qualitative analysis of compounds in soil samples was carried out by means of infrared spectrogram. The chemical properties of the compounds were determined by the location of the special chemical groups in the samples. (5) The community structure, properties and functions of the microorganisms in soil samples were analyzed by T-RFLP, and the different sources were further determined. Soil samples from different sources have certain differences in the types of components and the content and quality of each component. When the victim or the criminal is accompanied by a small amount of soil on the crime scene, the method explored in this experiment is used to separate the soil samples. Analyzing and identifying the differences of soil stability as trace trace evidence will link the victim or suspect with the scene of the crime to prove the related criminal activities.
【學(xué)位授予單位】:濟(jì)南大學(xué)
【學(xué)位級別】:碩士
【學(xué)位授予年份】:2015
【分類號】:S151.9
【共引文獻(xiàn)】
相關(guān)期刊論文 前2條
1 薛慧君;申向東;鄒春霞;周海龍;田曉敏;;寒區(qū)復(fù)合低摻量水泥加固紅土抗凍性試驗研究[J];材料導(dǎo)報;2014年18期
2 胡治華;馬艷榮;楊偉;王延奇;;松遼盆地北部泉三段河流相層序地層界面識別研究[J];西部探礦工程;2011年02期
相關(guān)博士學(xué)位論文 前1條
1 張?zhí)蚁?中國東部地帶性土壤中大腸桿菌O157:H7存活和吸附機(jī)制的研究[D];浙江大學(xué);2014年
相關(guān)碩士學(xué)位論文 前10條
1 姚莉;江漢平原部分土系認(rèn)證[D];華中農(nóng)業(yè)大學(xué);2011年
2 馬瑤;貧營養(yǎng)條件下微生物種群結(jié)構(gòu)的演替與分析[D];天津大學(xué);2012年
3 吳殿龍;遼寧地區(qū)古紅土微量和稀土元素地球化學(xué)特征研究[D];沈陽農(nóng)業(yè)大學(xué);2009年
4 李誠;江漢平原人為土基層分類制圖研究[D];華中師范大學(xué);2009年
5 羅丹;北京森林土壤系統(tǒng)分類[D];北京林業(yè)大學(xué);2012年
6 黃佳鳴;閩北地區(qū)代表性土壤的發(fā)生與系統(tǒng)分類研究[D];浙江大學(xué);2013年
7 崔政武;黑土膠散復(fù)合體的粘粒礦物組成及其表面形貌研究[D];吉林農(nóng)業(yè)大學(xué);2013年
8 李吉;懷牛膝連作對根際土壤微生物群落結(jié)構(gòu)和功能多樣性的影響[D];福建農(nóng)林大學(xué);2013年
9 孫仲秀;遼寧朝陽鳳凰山基準(zhǔn)剖面古土壤類型判定研究[D];沈陽農(nóng)業(yè)大學(xué);2013年
10 秦聰;江漢平原典型水耕人為土土系劃分及其有機(jī)質(zhì)垂直分布規(guī)律研究[D];華中農(nóng)業(yè)大學(xué);2013年
,本文編號:2203797
本文鏈接:http://sikaile.net/kejilunwen/nykj/2203797.html