期刊文献+

土壤质地及容重和含水率对其导气率影响的实验研究 被引量:11

Effects of soil texture,bulk density and moisture content on soil air permeability
下载PDF
导出
摘要 在室内利用一维瞬态法对重新装填的棕壤土、土、黄绵土和盐碱土等四种土壤的导气率进行了测量,分析了容重、含水率及冰冻等因素对土壤导气率的定量影响,以明确土壤类型、容重、含水率、冰冻与土壤导气率的关系。实验结果表明:土壤质地和结构对导气率有明显的影响,同一容重条件下土和棕壤土导气率接近,均显著高于黄绵土,在所设的四个容重条件下盐碱土导气率均为最低,仅为土和棕壤土导气率的3%~4%;四种土壤的导气率均随着容重的增加而减小,同种土壤最大容重(1.5 g.cm-3)下的导气率较之最小容重(1.2 g.cm-3)下降75%~85%,并且导气率与容重之间存在显著的指数函数关系;其他因素一致的条件下,土壤导气率随着含水率的增加而减小,导气率与含水率之间亦存在显著的指数函数关系;冰冻后土壤导气率较冰冻前显著降低,在本实验条件下含水率越低冻结后导气率下降越显著。 In laboratory,air permeability of reload brunisolic soil,lou soil,loessal soil and saline-alkali soil are measured by the one-dimensional transient method,soil bulk density,moisture content,frozen and other factors’ quantitative impact on the air permeability are analyzed,which are to make clear the relationship among the soil type,bulk density,moisture content,frozen and soil air permeability.Experimental results show that: soil texture and structure have a significant effect on the rate of air conductivity, in the same bulk density conditions,the air permeability of lou soil is close to that of brunisolic soil,and the air permeability of the two kinds of soil above are significantly higher than that of loessal soil.Saline-alkali soil air permeability are the lowest in the four bulk density,only 3% to 4% of the rate of lou soil and brunisolic soil;The air permeability of the four kinds of soil decreases with the increase of bulk density,the air permeability in maximum bulk density(1.5 g·cm-3) decreases by 75% to 85% compared to the minimum bulk density(1.2 g·cm-3) of the same kind of soil,and there is a significant exponential relationship between air permeability and bulk density;With other factors in the same conditions,the soil air permeability decreases with the increase of moisture content,there is also a significant exponential relationship between air permeability and moisture content;The frozen soil air permeability is much lower than that before freezing,the air permeability declines more significant in lower moisture content under given experimental conditions.
出处 《干旱地区农业研究》 CSCD 北大核心 2013年第2期116-121,共6页 Agricultural Research in the Arid Areas
基金 国家自然科学基金(41271236) 国家高技术研究发展计划(863计划)(2011AA100504) 山东省优秀中青年科学家科研奖励基金(BS2011HZ004) 烟台市科技计划(2011065)
关键词 土壤 导气率 容重 含水率 冰冻 soil air permeability bulk density moisture content frozen
  • 相关文献

参考文献15

  • 1王卫华,王全九,樊军.原状土与扰动土导气率、导水率与含水率的关系[J].农业工程学报,2008,24(8):25-29. 被引量:31
  • 2Minsdny B, McBratney A B. The efficiency of various approaches to obtaining estimates of soil hydraulic properties [ J ]. Geoderma, 2002, 107 : 55-70.
  • 3Iversen B V, Moldrup P, Schjonning P, et al. Air and water Perme- ability in differently-textured soil at two measurement scales [ J ]. Soil Sci, 2001, 166:643-659.
  • 4Aljibury F K, Evans D D. Water Permeability of saturated soil as re- lated to air Permeability at different moisture tensions[J]. Soil Sci Soe Am Proe, 1965,29 : 366-369.
  • 5Brook R H, Corey A T. Properties of porous media affecting fluid flow [J]. Journal of Irrigation and Division, 1996,92:61-89.
  • 6Ball B C. Modeling of soil pores as tubes using gas permeabilities, gas diffusivities and water release[J]. Journal of Soil Science, 1981,32 (4) :465-481.
  • 7McCarthy K P, Brown K W. Soil gas permeability as influenced by soil gas-filled porosity[ J]. Soil Science Society of American Journal, 1992, 56(4) :997-1003.
  • 8Moldrup P, Yoshikawa S, Olesen T, et al. Air permeability in undis- turbed volcanic ash soil:Predictive model test and soil structure finger- print[J]. Soil Sci Soc Am J,2003,67:32-40.
  • 9Mira Stone Olson. Comparison of three techniques to measrue unsatu- rate&zone air permeability at Picatinny Atsenal [ J]. NJ Journal of Contaminant Hydrology ,2001,53 : 1-9.
  • 10Atac Tuli, Hopmans J W, Rolston D E, et al. Comparison of air and water permeability between disturbed and undisturbed soil [ J]. Soil Sci, 2005,69 : 1361-1371.

二级参考文献27

  • 1Reynolds W D, Elriek D E, Youngs E G, et al. Saturated and field-saturated water flow parameters. Field methods (vadose and saturat- ed zone techniques)[C]//In j H Dane, G C Topp (ed.) Methods of soil analysis. Part4. SSSA Book Set. 5. SSSA, Madison, WI, 2002: 817-843.
  • 2Blackwell P S, Ringrose-Voase A J, Jayawardane N S, et al. The use of air-filled porosity and intrinsic permeability to air to characterize structure of macropore space and saturated hydraulic conductivity of clay soils[J]. J Soil Sci. 1990, 41:215 -228.
  • 3Moldrup P, Olesen T, Komatsu T, et al. Tortuosity, diffusivity, and permeability in the soil liquid and gaseous phases[J]. Soil Sci Soc Am J, 2001, 65:613-623.
  • 4Iversen B V, Moldrup P, Schjonning P, et al. Air and water permeability in differently-textured soils at two measurement scales[J].Soil Sci, 2001, 166:643-659.
  • 5Loll P, Moldrup P, Sehjonning P, et al. Predicting saturated hydraulic conductivity from air permeability: Applicatio in stochastic water infiltration modeling[J]. Water Resour Res, 1999, 35 : 2 387 - 2 400.
  • 6Moldrup P, Yoshikawa S, Olesen T, et al. Air permeability in undisturbed volcanic ash soils~ Predictive model test and soil structure fingerprint[J]. Soil Sei Soe Am J, 2003, 67:32 - 40.
  • 7Minasny B, McBratney A B: The efficiency of various approaches to obtaining estimates of soil hydraulic properties[J]. Geoderma, 2002, 107:55 - 70.
  • 8Jury W A, Horton R. Soil Physics [M]. John Wiley and Sons, Inc, 2004.
  • 9同延安,王全九.土壤-植物-大气连续体系中水运移理论与方法[M].西安:陕西科学技术出版社,2002.
  • 10Hillel D. Environmental soil physics[M]. Academic Press, 1998.

共引文献32

同被引文献171

引证文献11

二级引证文献57

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部