亚洲免费av电影一区二区三区,日韩爱爱视频,51精品视频一区二区三区,91视频爱爱,日韩欧美在线播放视频,中文字幕少妇AV,亚洲电影中文字幕,久久久久亚洲av成人网址,久久综合视频网站,国产在线不卡免费播放

        ?

        Influence of Gradient on Stability of Soil Slope Containing Roots

        2015-01-18 02:50:18HailiZHUYantingLILuSONG
        Agricultural Science & Technology 2015年10期
        關(guān)鍵詞:固土北京林業(yè)大學(xué)護(hù)坡

        Haili ZHU ,Yanting LI ,Lu SONG

        1.Department of Geological Engineering,Qinghai University,Xining 810016,China;

        2.Qinghai Institute of Salt Lakes,Chinese Academy of Sciences,Xining 810008,China

        Responsible editor:Tingting XU Responsible proofreader:Xiaoyan WU

        Alarge number of domestic and foreign researches have shown that the presence of plants plays an important role in preventing water and soil erosion in slope and shallow landslides,reducing the cracking degree of slope soil,reducing the slope surface soil erosion and increasing slope stability[1].Plant roots spread across soil system,and they contact with soil particles,forming into natural root-soil composite[2].The strength size of root-soil composite plays an important role in slope stability[3-11],and it is also an important in dicator for assessing the contribution of root system to slope stability.Lin et al.[4]simulated the slope planted with Phyllostachys bambusoides in Taoyuan,Taiwan using three-dimensional finite element method(3D).The results showed that when the gradient ranged from 50° to 70°,Phyllostachys bambusoides showed insignificant effect on slope stability; when the gradient was less than 25° or higher than 40°,the contribution of Phyllostachys bambusoides to slope stability was greater.Xiao et al.[6]investigated the effects of Robinia pseudoacacia on slope stress and strain distribution within gradient range of 30°-40° using the finite element software ADINA.The results showed that Robinia pseudoacacia roots could improve the stress and strain distribution in shallow slope,so shallow slope tends to be more stable;the increased gradient would increase the stress in slope toe; tensile stress would be generated gradually in slope shoulder,and it became greater and greater; the concentrated region of shear strain was enlarged.Thomas et al.[11]investigated the effects of three kinds of root types (horizontal root,scattered root and main taproot) on stabilities of slopes with gradients of 0°,5°,35°and 45°by the Monte Carlo method.They found that the taproot type had greater contribution to stability of slope with gradient of 45°,and the shear strength of root-soil composite was 15.08 kPa.At present,there are many studies showing that vegetation enhances shear strength of slope soil and improves slope stability.However,there are rare quantitative researches on effect of gradient on stability of slope containing plant roots.Therefore,an indoor triaxial shear test was conducted to measure the shear strengths of root-free slope soil and root-soil composite,and the effect of gradient on slope stability was analyzed using limit equilibrium method,thereby providing a theoretical basis for the gradient design of ecological protection slope.

        Materials and Methods

        Materials

        The soil samples were collected from the surveyed area located in Xiaozhai Village,Yunjiakou Town,Chendong District,Xining City.The collected soil was silty clay soil,and its physical properties were shown in Table1.The roots of Caragana kor

        shinskii and Atriplex canescens were also collected from the survey area.The roots of the two kinds of shrub are characterized by strong cold and drought resistance and developed root system.Caragana korshinskii and Atriplex canescens are two dominant shrub species for reducing wind and stabilizing sand and maintaining soil and water in Qinghai-Tibet Plateau.

        Methods

        The shear strengths of the sampled soil and root-soil composites were measured using a triaxial apparatus(TCK-1,Nanjing Soil Instrument Co.,Ltd.).The measured samples had diameter of 61.8 mm,height of 125 mm,moisture content of 12.8% and wet density of 1.58 g/cm3.For the preparation of soil samples containing roots,the roots were added vertically and horizontally.In each root-soil composite,total four shrub taproots with average length of 120 mm and diameter of 1.66 mm were added vertically; total three layers of shrub lateral roots with average diameter of 0.48 mm and uniform length of 50 mm were divided evenly and horizontally in the sample,and there was 0.235 g of roots in each layer.In order to simulate the actual situation,the used root materials were all fresh.There were four replicates for each treatment,and the measurement was conducted under confining pressure of 10,20,30 and 40 kPa,respectively.For the samples in a same treatment,Mohr’s stress circles were drawn on a τ-σ stress plan.In addition,the envelope curves of stress circles at failure under different confining pressures were drawn.Thus the cohesions(c)and internal friction angles(φ)reflecting shear strengths of soil and root-soil composite samples were obtained.

        Correlation between stability coefficient and gradient of slope

        Definition of slope stability coefficientIn the limit equilibrium method,the stability coefficient(K)is defined as follows:

        When Mohr-Coulomb condition is taken into account,the calculation formula of stability coefficient(K)is transformed as follows:

        In the Equation (2),c represents the actual cohesion of soil;φrepresents the actual internal friction angle of soil; ccrepresents the cohesion in the critical state;φcrepresents the internal friction angle of soil in the critical state;σrepresents the actual normal stress component.

        Example calculation of stability coefficient of slope containing roots

        It is assumed that on the surface of a shallow slope,there is a soil system with thickness of h,length of l and slope angle ofα.The soil volume weight was assumed asγ.The weight(Q)of the soil system can be calculated according to the following formula:

        Q=γhl.

        The root-containing slopes were all soil slopes planted with Caragana korshinskii or Atriplex canescens.Considering the action depth of roots in surface soil system of certain slope,the thickness of soil system (h)is assumed as 1 m.Thus,the Equation (2)can be transformed as follows:

        The Equation (3) is applicable to both root-free and root-containing slopes.Due to the reinforcement effect of root system on slope,the cohesion c is increased,and the internal friction anglesφis also increased,thus the stability coefficient difference ΔK is increased.It is assumed that cr represents the cohesion of soil system on the surface of root-containing slope,c0represents the cohesion of soil system on the surface of root-free slope,φrrepresents the internal friction angle of soil system on the surface of root-containing slope,φ0represents the internal friction angle of soil system on the sur-face of root-free slope,γrrepresents the volume weight of soil system on the surface of root-containing system,γ0represents the volume weight of soil system on the surface of root-free slope,Krrepresents the stability coefficient of soil system on the surface of root-containing slope and K0represents the stability coefficient of soil system on the surface of root-free slope,thus the ΔK can be calculated as follows:

        Table1 Physical properties of soil in surveyed area

        Table2 Calculation results of slope stability parameters

        Table3 Stability coefficient increments of slopes with varying gradients

        Results and Analysis

        By triaxial compression test and routine physical tests,the shear strength indexes and volumes of sampled root-free soil and root-soil composites were obtained (Table2).Soil shear strength is produced by the soil cohesion and internal friction angle.Many studies have shown that the increased shear strength of reinforced soil is entirely due to produced cohesion,instead of variation in internal friction angle[14-15].The results of this study showed that the internal friction angles of root-soil composites were almost the same as that of pure soil;compared with that in pure soil,the increase in cohesion of root-soil composite was more obvious,and the cohesion of root-soil composite in the Atriplex canescens-planted slope was greater than that in the Caragana korshinskii-planted slope.

        According to the Equation (4),the stability coefficient increments of slopes with gradients ranging from 10°to 90° were calculated (Table3).The stability coefficient increments of the two slopes planted with Caragana kor

        shinskii and Atriplex canescens were all increased with the increase in slope gradient,and the stability coefficient increment of Atriplex canescens-planted slope was larger than that of Caragana korshinskii-planted slope,indicating greater reinforcement effect of

        Atriplex canescens on shallow slope.Based on the calculation results,the relationship between ΔK andαwas fitted(Fig.2).

        Fig.2 showed that when the gradient was less than 25°,the stability coefficient of root-containing slope was two times higher than that of root-free slope.The root-free slope and rootcontaining slope were all stable,and their surface soil systems all could reach a stable state without protection of plant roots.Vegetation was of great significance in greening environment and preventing rainwater erosion.When the gradient ranged from 25° to 50°,the stability coefficient of Atriplex canescens-planted slope was higher than that of pure slope by 0.80-1.38,and of Caragana korshinskii-planted slope was higher than that of pure slope by 0.56 -1.03.The root-free slope was secondary stable,and it needed the protection of vegetation.When vegetation in surface soil system grows well,its intricate root system plays an important role in reinforcing entire soil system.Under the turgor pressure of roots,axial pressure is generated between roots and surface soil particles,closely binding plant roots and soil particles.In addition,the contact area between roots and soil is enlarged,so that the frictional resistance between the roots and the surface soil system is increased.This explains why the stability coefficient of surface soil system of root-containing slope was higher than that of root-free slope.When the gradient exceeded 55°,the stability coefficients of the slopes planted with two kinds of shrub were higher than that of the pure slope by 0.55 in average.The slope stability varied insignificantly with the increase in gradient,which is consistent with the study result of Lin et al[4].In short,when slope gradient was less than 55°,plant root system played an important role in improving soil strength.

        Conclusions

        Based on the preparation of remodeling samples,the effect of plant roots on slope stability was investigated by triaxial compression test.The results showed that internal friction angles of root-soil composites of Atriplex canescens-planted slope and Caragana korshinskii-planted slope were almost the same as that of pure slope; compared with that of pure slope,the cohesions of the two kinds of root-soil composites were increased significantly,and the cohesion of rootsoil composite of Atriplex canescensplanted slope was higher than that of Caragana korshinskii-planted slope.

        The calculation and analysis showed that the stability coefficient increments of the two kinds of root-soil composites were all decreased with the increase in slope gradient,and the stability coefficient increment of Atriplex canescens-planted slope was larger than that of Caragana korshinskii-planted slope.

        When the slope gradient exceeded 55°,the reinforcement effect of roots of the two kinds of shrub on shallow slope basically reached a limit,suggesting that plant roots play a role in improving slope stability when the slope gradient was less than 55°.

        [1]GARY DH,ANDREW TL.Biotechnical slope protection and erosion control[M].New York:Van Nostrand Reinhold Company,1982.

        [2]YANG YC (楊亞川),MO YJ (莫永京),WANG ZF (王芝芳),et al.Experiment study on anti-water erosion and shear strength of soil-root composite (土體-草本植物根系復(fù)合體抗水蝕強(qiáng)度與抗剪強(qiáng)度的試驗(yàn)研究)[J].Journal of China Agricultural University (中國(guó)農(nóng)業(yè)大學(xué)學(xué)報(bào)),1996,1(2):31-38.

        [3]ZHOU XJ(周錫九),ZHAO XF(趙曉鋒).Strengthening role of plants on shallow slope (坡面植草防護(hù)的淺層加固作用)[J].Journal of North Jiaotong University(北方交通大學(xué)學(xué)報(bào)),1995,19(2):143-146.

        [4]LIN DG,HUANG BS,LIN SH.3-D numerical investigations into the shear strength of the soil-root system of Makino bamboo and its effect on slope stability [J].Ecological Engineering,2010,36:992-1006.

        [5]LI GR (李國(guó)榮),HU XS (胡夏嵩),MAO XQ(毛小青),et al.Numerical simulation of shrub roots for slope protection effects on loess area of northeast Qinghai-Tibetan Plateau(青藏高原東北部黃土區(qū)灌木植物根系護(hù)坡效應(yīng)的數(shù)值模擬) [J].Chinese Journal of Rock Mechanics and Engineering(巖石力學(xué)與工程學(xué)報(bào)),2010,29(9):1877-1884.

        [6]XIAO BL (肖本林),LUO SL (羅壽龍),CHEN J (陳軍),et al.Finite element analysis of eco-protection slope through roots (根系生態(tài)護(hù)坡的有限元分析)[J].Rock and Soil Mechanics (巖土力學(xué)),2011,32(6):1881-1885.

        [7]RAJESH RB,SHRIVASTVA K.Biological stabilization of mine dumps:shear strength and numerical simulation approach with special reference to Sisam tree[J].Environment Earth Sci,2007,12(4):1121-1142.

        [8]JI JN (及金楠).Analysis of root-soil mechanical interaction to study tree anchorage and soil reinforcement by roots(基于根-土相互作用機(jī)理的根錨固作用研究)[D].Beijing:Beijing Forestry University(北京:北京林業(yè)大學(xué)),2007.

        [9]JIANG ZQ (姜志強(qiáng)),SUN SL (孫樹(shù)林),CHENG LF (程龍飛).Soil-reinforcing effect of roots and slope stability under protection of plants (根系固土作用及植物護(hù)坡穩(wěn)定性分析)[J].Site Investigation Science and Technology(勘察科學(xué)技術(shù)),2005,4:12-14.

        [10]LIU XP(劉秀萍).Finite element method numerical simulation of forest roots reinforcement(林木根系固土有限元數(shù)值模擬)[D].Beijing:Beijing Forestry University(北京:北京林業(yè)大學(xué)),2008.

        [11]THOMAS RE,POLLEN-BANKHEAD N.Modeling root-reinforcement with a fiber-bundle model and Monte Carlo simulation [J].Ecological Engineering,2010,36(1):47-61.

        [12]Northwest Institute of Plateau Biology of Chinese Academy of Sciences(中國(guó)科學(xué)院西北高原生物研究所).Qinghai Flora(Volume II)(青海植物志(第2 卷)[M].Xining:Qinghai People’s Publishing House(西寧:青海人民出版社),1997.

        [13]CHEN ZY(陳仲頤),ZHOU JX(周景星),WANG HJ(王洪瑾).Soil Mechanics(土力學(xué))[M].Beijing:Tsinghua University Press(北京:清華大學(xué)出版社),1994.

        [14]LIU XL (劉秀萍),CHEN LH (陳麗華),SONG WF (宋維峰).Study on the shear strength of forest root-loess composite (林木根系與黃土復(fù)合體的抗剪強(qiáng)度試驗(yàn)研究)[J].Journal of Beijing Forestry University(北京林業(yè)大學(xué)學(xué)報(bào)),2006,28(5):67-72.

        [15]XIE WL(謝婉麗),WANG JD(王家鼎),WANG YL ( 王亞玲).Triaxial tests study on deformation and strength characteristics of reinforced loess (加筋黃土變形和強(qiáng)度特性的三軸試驗(yàn)研究)[J].Advance in Earth Sciences (地球科學(xué)進(jìn)展),2004,19(plus):333-339.

        猜你喜歡
        固土北京林業(yè)大學(xué)護(hù)坡
        公路邊坡防護(hù)生態(tài)輕型樁最優(yōu)間距分析
        歡迎訂閱2023年《北京林業(yè)大學(xué)學(xué)報(bào)(社會(huì)科學(xué)版)》
        《北京林業(yè)大學(xué)學(xué)報(bào)(社會(huì)科學(xué)版)》2022年總目次
        生態(tài)護(hù)坡技術(shù)在河道治理中的應(yīng)用探究
        How to Understand the Story of an Hour Using Id, Ego and Superego
        新疆經(jīng)濟(jì)林生態(tài)系統(tǒng)保育土壤功能及價(jià)值評(píng)估
        Pilot Study for The Relationship Between Politeness and Prosodic Features
        生態(tài)混凝土護(hù)坡在水利工程中的應(yīng)用
        農(nóng)村河道護(hù)坡治理模式及生態(tài)護(hù)坡應(yīng)用探討
        森林生態(tài)系統(tǒng)固土保肥功能探析
        色婷婷久久综合中文蜜桃| 日本一极品久久99精品| 美女裸体自慰在线观看| 久久精品国产99精品国偷| 欧洲国产成人精品91铁牛tv| 国产精品不卡无码AV在线播放| 人妻无码一区二区19P| 91热久久免费频精品99| 人妻少妇精品视频一区二区三| av网站在线观看大全| 国产av熟女一区二区三区| 风情韵味人妻hd| 亚洲av无码片vr一区二区三区| 亚洲色成人www永久在线观看| а天堂中文在线官网| 亚洲av无码专区国产乱码不卡| 色94色欧美sute亚洲线路二| 国产成人亚洲综合无码DVD| 人妻中文字幕av有码在线| 亚洲国产精品美女久久久| 亚洲一区二区三区厕所偷拍| 在线视频免费自拍亚洲| 夜夜爽夜夜叫夜夜高潮| 久久精品国产成人| 久久午夜无码鲁丝片直播午夜精品| 暖暖免费 高清 日本社区在线观看| 无码一区东京热| 丰满人妻无套内射视频| 国产久久久自拍视频在线观看| 女同av一区二区三区| 邻居少妇张开腿让我爽了一夜| 免费看又色又爽又黄的国产软件 | 人人妻人人添人人爽日韩欧美| 伊人网视频在线观看| 亚洲欧洲久久久精品| 精品人妻中文字幕一区二区三区| 加勒比一本大道大香蕉| 久久精品国产白丝爆白浆| 日本一区二区三区清视频| 色欲一区二区三区精品a片| 国产专区国产av|