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Artykuły w czasopismach na temat „Tension infiltrometer”

Autor: Grafiati

Data publikacji: 4 czerwca 2021

Data aktualizacji: 6 lutego 2022

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1

Hunter, A. E., H. W. Chau, and B. C. Si. "Impact of tension infiltrometer disc size on measured soil water repellency index." Canadian Journal of Soil Science 91, no. 1 (February 2011): 77–81. http://dx.doi.org/10.4141/cjss10033.

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Hunter, A. E., Chau, H. W. and Si, B. C. 2011. Impact of tension infiltrometer disc size on measured soil water repellency index. Can. J. Soil Sci. 91: 77–81. Accurate measurement of soil water repellency (or hydrophobicity) is important for assessing the hydraulic properties of soils. Water repellency index (RI), a measure of soil water repellency, can be determined using the tension infiltrometer. Little is known about the effects of different infiltrometer disc sizes on measured RI. Furthermore, the impact of method selection in the context of site assessment is unknown. The objective of th

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2

Schwärzel, Kai, and Jürgen Punzel. "Hood Infiltrometer-A New Type of Tension Infiltrometer." Soil Science Society of America Journal 71, no. 5 (September 2007): 1438–47. http://dx.doi.org/10.2136/sssaj2006.0104.

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3

Ankeny, M. D., T. C. Kaspar, and R. Horton. "Design for an Automated Tension Infiltrometer." Soil Science Society of America Journal 52, no. 3 (May 1988): 893–96. http://dx.doi.org/10.2136/sssaj1988.03615995005200030054x.

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4

McKenzie, N. J., H. P. Cresswell, H. Rath, and D. Jacquier. "Measurement of unsaturated hydraulic conductivity using tension and drip infiltrometers." Soil Research 39, no. 4 (2001): 823. http://dx.doi.org/10.1071/sr99136.

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We investigated differences between constant flux and constant potential methods for determining unsaturated hydraulic conductivity in the laboratory. A cheap and robust method was required. The constant flux drip infiltrometer has been used with large intact cores on a wide range of Australian soils. However, the method can be simplified by replacing the drip infiltrometer with a constant potential tension infiltrometer (disc permeameter). We conducted a series of measurements using 9 soil cores to determine whether the measured hydraulic conductivity differed with each method at matric poten

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5

Gordon, Dennis C., and Paul D. Hallett. "An automated microinfiltrometer to measure small-scale soil water infiltration properties." Journal of Hydrology and Hydromechanics 62, no. 3 (September 1, 2014): 248–52. http://dx.doi.org/10.2478/johh-2014-0023.

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Abstract We developed an automated miniature constant-head tension infiltrometer that measures very small infiltration rates at millimetre resolution with minimal demands on the operator. The infiltrometer is made of 2.9 mm internal radius glass tube, with an integrated bubbling tower to maintain constant negative head and a porous mesh tip to avoid air-entry. In the bubbling tower, bubble formation and release changes the electrical resistance between two electrodes at the air-inlet. Tests were conducted on repacked sieved sands, sandy loam soil and clay loam soil, packed to a soil bulk densi

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6

Casey, Francis X. M., and Nathan E. Derby. "Improved design for an automated tension infiltrometer." Soil Science Society of America Journal 66, no. 1 (2002): 64. http://dx.doi.org/10.2136/sssaj2002.0064.

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7

Casey, Francis X. M., and Nathan E. Derby. "Improved design for an automated tension infiltrometer." Soil Science Society of America Journal 66, no. 1 (January 2002): 64–67. http://dx.doi.org/10.2136/sssaj2002.6400.

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8

FELTON, GARY K. "SOIL WATER RESPONSE BENEATH A TENSION INFILTROMETER." Soil Science 154, no. 1 (July 1992): 14–24. http://dx.doi.org/10.1097/00010694-199207000-00003.

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9

Logsdon, S. D., J. K. Radke, and D. L. Karlen. "Comparison of alternative farming systems. I. Infiltration techniques." American Journal of Alternative Agriculture 8, no. 1 (March 1993): 15–20. http://dx.doi.org/10.1017/s0889189300004860.

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AbstractQuantitative data are needed to understand how alternative farming practices affect surface infiltration of water and associated surface soil properties. We used a rainfall simulator, double ring infiltrometer, small single ring infiltrometers, and tension infiltrometers to measure water infiltration for Clarion loam (fine-loamy, mixed, mesic Typic Hapludoll) and for Webster silty clay loam (fine-loamy, mixed, mesic Typic Haplaquoll) soils located on a conventionally-managed and an alternatively-managed farm in central Iowa. Steady-state measurements suggested that infiltration rates w

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10

Reynolds, W. D., B. T. Bowman, R. R. Brunke, C. F. Drury, and C. S. Tan. "Comparison of Tension Infiltrometer, Pressure Infiltrometer, and Soil Core Estimates of Saturated Hydraulic Conductivity." Soil Science Society of America Journal 64, no. 2 (March 2000): 478–84. http://dx.doi.org/10.2136/sssaj2000.642478x.

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11

Si, Bing Cheng, and Waduwawatte Bodhinayake. "Determining Soil Hydraulic Properties from Tension Infiltrometer Measurements." Soil Science Society of America Journal 69, no. 6 (November 2005): 1922–30. http://dx.doi.org/10.2136/sssaj2005.0022.

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12

Reynolds, W. D., and D. E. Elrick. "Determination of Hydraulic Conductivity Using a Tension Infiltrometer." Soil Science Society of America Journal 55, no. 3 (May 1991): 633–39. http://dx.doi.org/10.2136/sssaj1991.03615995005500030001x.

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13

Reynolds, W. D., and W. D. Zebchuk. "Use of contact material in tension infiltrometer measurements." Soil Technology 9, no. 3 (September 1996): 141–59. http://dx.doi.org/10.1016/s0933-3630(96)00009-8.

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14

Fallico, C., E. Migliari, and S. Troisi. "Characterization of the field saturated hydraulic conductivity on a hillslope: measurement techniques, data sensitivity analysis and spatial correlation modelling." Hydrology and Earth System Sciences Discussions 2, no. 4 (July 28, 2005): 1247–98. http://dx.doi.org/10.5194/hessd-2-1247-2005.

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Abstract. In the context of studies aiming at the estimation of effective parameters for unsaturated zone modelling, this work tackles the problem of experimental data quality, considering the large collection of data gathered at an experimental site equipped for unsaturated zone hydraulic monitoring in the alluvial basin of a Calabrian river, in the South of Italy. Focusing attention on field saturated hydraulic conductivity, the in-site measurement techniques by tension disc and pressure ring infiltrometers are considered, pointing out the main indications for the correct use of each measuri

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15

Walker, C., H. S. Lin, and D. D. Fritton. "Is the Tension Beneath a Tension Infiltrometer What We Think It Is?" Vadose Zone Journal 5, no. 3 (August 2006): 860–66. http://dx.doi.org/10.2136/vzj2005.0096.

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16

Špongrová, Kamila, Cedric Kechavarzi, Marc Dresser, Svatopluk Matula, and Richard J. Godwin. "Development of an Automated Tension Infiltrometer for Field Use." Vadose Zone Journal 8, no. 3 (August 2009): 810–17. http://dx.doi.org/10.2136/vzj2008.0135.

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17

Zhang, Y., G. L. Butters, G. E. Cardon, and R. E. Smith. "Analysis and Testing of a Concentric-Disk Tension Infiltrometer." Soil Science Society of America Journal 63, no. 3 (May 1999): 544–53. http://dx.doi.org/10.2136/sssaj1999.03615995006300030017x.

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18

LIN, H. S., and K. J. MCINNES. "WATER FLOW IN CLAY SOIL BENEATH A TENSION INFILTROMETER." Soil Science 159, no. 6 (June 1995): 375–82. http://dx.doi.org/10.1097/00010694-199506000-00002.

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19

Kechavarzi, Cedric, Kamila Špongrová, Marc Dresser, Svatopluk Matula, and Richard J. Godwin. "Laboratory and field testing of an automated tension infiltrometer." Biosystems Engineering 104, no. 2 (October 2009): 266–77. http://dx.doi.org/10.1016/j.biosystemseng.2009.06.014.

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20

Latorre, B., D. Moret-Fernández, M. N. Lyons, and S. Palacio. "Smartphone-based tension disc infiltrometer for soil hydraulic characterisation." Journal of Hydrology 600 (September 2021): 126551. http://dx.doi.org/10.1016/j.jhydrol.2021.126551.

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21

Klípa, Vladimír, Michal Sněhota, and Michal Dohnal. "New automatic minidisk infiltrometer: design and testing." Journal of Hydrology and Hydromechanics 63, no. 2 (June 1, 2015): 110–16. http://dx.doi.org/10.1515/johh-2015-0023.

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Abstract Soil hydraulic conductivity is a key parameter to predict water flow through the soil profile. We have developed an automatic minidisk infiltrometer (AMI) to enable easy measurement of unsaturated hydraulic conductivity using the tension infiltrometer method in the field. AMI senses the cumulative infiltration by recording change in buoyancy force acting on a vertical solid bar fixed in the reservoir tube of the infiltrometer. Performance of the instrument was tested in the laboratory and in two contrasting catchments at three sites with different land use. Hydraulic conductivities de

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22

Nachabe, Mahmood H., and Tissa Illangasekare. "Use of Tension Infiltrometer Data with Unsaturated Hydraulic Conductivity Models." Ground Water 32, no. 6 (November 1994): 1017–21. http://dx.doi.org/10.1111/j.1745-6584.1994.tb00941.x.

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23

Smettem, K. R. J., P. J. Ross, R. Haverkamp, and J. Y. Parlange. "Three-Dimensional Analysis of Infiltration from the Disk Infiltrometer: 3. Parameter Estimation Using a Double-Disk Tension Infiltrometer." Water Resources Research 31, no. 10 (October 1995): 2491–95. http://dx.doi.org/10.1029/95wr01722.

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24

Orfánus, T., Z. Bedrna, Ľ. Lichner, D. Hallett P, K. Kňava, and M. Sebíň. "Spatial variability of water repellency in pine forest soil." Soil and Water Research 3, Special Issue No. 1 (June 30, 2008): S123—S129. http://dx.doi.org/10.17221/11/2008-swr.

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The variability of water repellency of pine-forest arenic regosols and its influence on infiltration processes were measured in southwest Slovakia. The water drop penetration time (WDPT) tests of soil water repellency and infiltration tests with a miniature tension infiltrometer (3 mm diameter) were performed. Large differences in infiltration were observed over centimetre spatial resolution, with WDPT tests suggesting water repellency varying from extreme to moderate levels. For soils with severe to extreme water repellency determined with WDPT, steady state infiltration was not reached in te

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25

Fouli, Ymène, Barbara J. Cade-Menun, and Herb W. Cutforth. "Freeze–thaw cycles and soil water content effects on infiltration rate of three Saskatchewan soils." Canadian Journal of Soil Science 93, no. 4 (September 2013): 485–96. http://dx.doi.org/10.4141/cjss2012-060.

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Fouli, Y., Cade-Menun, B. J. and Cutforth, H. W. 2013. Freeze–thaw cycles and soil water content effects on infiltration rate of three Saskatchewan soils. Can. J. Soil Sci. 93: 485–496. Many soils at high latitudes or elevations freeze and thaw seasonally. More frequent freeze–thaw cycles (FTCs) may affect ecosystem diversity and productivity because freeze–thaw cycles cause changes in soil physical properties and affect water movement in the landscape. This study examined the effects of FTCs (0, 1, 5, and 10) and antecedent soil water content [at soil water potentials (SWP) −1.5, −0.033 and −

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26

C. J. Everts and R. S. Kanwar. "Interpreting Tension-infiltrometer Data for Quantifying Soil Macropores: Some Practical Considerations." Transactions of the ASAE 36, no. 2 (1993): 423–28. http://dx.doi.org/10.13031/2013.28354.

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27

Meshgi, Ali, and Ting Fong May Chui. "Analysing tension infiltrometer data from sloped surface using two-dimensional approximation." Hydrological Processes 28, no. 3 (November 20, 2012): 744–52. http://dx.doi.org/10.1002/hyp.9621.

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28

Šimůnek, Jiří, Ole Wendroth, and Martinus T. van Genuchten. "Estimating unsaturated soil hydraulic properties from laboratory tension disc infiltrometer experiments." Water Resources Research 35, no. 10 (October 1999): 2965–79. http://dx.doi.org/10.1029/1999wr900179.

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29

Simůnek, Jirí, and Martinus Th van Genuchten. "ESTIMATING UNSATURATED SOIL HYDRAULIC PROPERTIES FROM MULTIPLE TENSION DISC INFILTROMETER DATA." Soil Science 162, no. 6 (June 1997): 383–98. http://dx.doi.org/10.1097/00010694-199706000-00001.

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30

Lin, H. S., K. J. McInnes, L. P. Wilding, and C. T. Hallmark. "Low tension water flow in structured soils." Canadian Journal of Soil Science 77, no. 4 (November 1, 1997): 649–54. http://dx.doi.org/10.4141/s96-061.

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Water transport through structured clayey soils may be prone to by-pass flow, a mechanism that may lead to rapid transport of contaminants to ground water. To quantify the significance of low-tension water flow in structured soils, apparent steady-state infiltration rates at water potentials from −0.24 to 0 m were measured using tension infiltrometers on 18 soils of varying texture and structure. Each infiltration measurement was conducted sequentially at −0.24, −0.12, −0.06, −0.03, −0.02, −0.01, and 0 m supply potentials (Ψsupply), all at the same soil location, to separate different size por

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31

Reynolds, W. D. "Tension Infiltrometer Measurements: Implications of Pressure Head Offset due to Contact Sand." Vadose Zone Journal 5, no. 4 (November 2006): 1287–92. http://dx.doi.org/10.2136/vzj2006.0098c.

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32

Bodhinayake, Waduwawatte, Bing Cheng Si, and Chijin Xiao. "New Method for Determining Water-Conducting Macro- and Mesoporosity from Tension Infiltrometer." Soil Science Society of America Journal 68, no. 3 (2004): 760. http://dx.doi.org/10.2136/sssaj2004.0760.

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33

Bodhinayake, Waduwawatte, Bing Cheng Si, and Chijin Xiao. "New Method for Determining Water-Conducting Macro- and Mesoporosity from Tension Infiltrometer." Soil Science Society of America Journal 68, no. 3 (May 2004): 760–69. http://dx.doi.org/10.2136/sssaj2004.7600.

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34

Watson, K. W., and R. J. Luxmoore. "Estimating Macroporosity in a Forest Watershed by use of a Tension Infiltrometer." Soil Science Society of America Journal 50, no. 3 (May 1986): 578–82. http://dx.doi.org/10.2136/sssaj1986.03615995005000030007x.

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35

K. R. Close, G. Frasier, G. H. Dunn, and J. C. Loftis. "TENSION INFILTROMETER CONTACT INTERFACE EVALUATION BY USE OF A POTASSIUM IODIDE TRACER." Transactions of the ASAE 41, no. 4 (1998): 995–1004. http://dx.doi.org/10.13031/2013.17272.

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36

Moret-Fernández, David, César González-Cebollada, and Borja Latorre. "Microflowmeter-tension disc infiltrometer – Part I: Measurement of the transient infiltration rate." Journal of Hydrology 466-467 (October 2012): 151–58. http://dx.doi.org/10.1016/j.jhydrol.2012.07.011.

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37

Castiglione, Paolo, Peter J. Shouse, Binayak Mohanty, David Hudson, and Martinus Th van Genuchten. "Improved Tension Infiltrometer for Measuring Low Fluid Flow Rates in Unsaturated Fractured Rock." Vadose Zone Journal 4, no. 3 (August 2005): 885–90. http://dx.doi.org/10.2136/vzj2004.0135.

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38

Ramos, T. B., M. C. Gonçalves, J. C. Martins, M. Th van Genuchten, and F. P. Pires. "Estimation of Soil Hydraulic Properties from Numerical Inversion of Tension Disk Infiltrometer Data." Vadose Zone Journal 5, no. 2 (May 2006): 684–96. http://dx.doi.org/10.2136/vzj2005.0076.

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39

Angulo-Jaramillo, R., J. L. Thony, G. Vachaud, F. Moreno, E. Fernandez-Boy, J. A. Cayuela, and B. E. Clothier. "Seasonal Variation of Hydraulic Properties of Soils Measured using a Tension Disk Infiltrometer." Soil Science Society of America Journal 61, no. 1 (January 1997): 27–32. http://dx.doi.org/10.2136/sssaj1997.03615995006100010005x.

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40

Šimůnek, J., and M. T. van Genuchten. "Estimating Unsaturated Soil Hydraulic Properties from Tension Disc Infiltrometer Data by Numerical Inversion." Water Resources Research 32, no. 9 (April 1996): 2683–96. http://dx.doi.org/10.1029/96wr01525.

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41

Holden, J., T. P. Burt, and N. J. Cox. "Macroporosity and infiltration in blanket peat: the implications of tension disc infiltrometer measurements." Hydrological Processes 15, no. 2 (2001): 289–303. http://dx.doi.org/10.1002/hyp.93.

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42

Bagarello, V., M. Castellini, M. Iovino, and A. Sgroi. "Testing the concentric-disk tension infiltrometer for field measurement of soil hydraulic conductivity." Geoderma 158, no. 3-4 (September 2010): 427–35. http://dx.doi.org/10.1016/j.geoderma.2010.06.018.

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43

Casanova, Manuel, Ingmar Messing, and Abraham Joel. "Influence of aspect and slope gradient on hydraulic conductivity measured by tension infiltrometer." Hydrological Processes 14, no. 1 (January 2000): 155–64. http://dx.doi.org/10.1002/(sici)1099-1085(200001)14:1<155::aid-hyp917>3.0.co;2-j.

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44

Kodešová, Radka, Jiří Šimůnek, Antonín Nikodem, and Veronika Jirků. "Estimation of the Dual-Permeability Model Parameters using Tension Disk Infiltrometer and Guelph Permeameter." Vadose Zone Journal 9, no. 2 (May 2010): 213–25. http://dx.doi.org/10.2136/vzj2009.0069.

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45

BONSU, M. "Field determination of sorptivity as a function of water content using a tension infiltrometer." Journal of Soil Science 44, no. 3 (September 1993): 411–15. http://dx.doi.org/10.1111/j.1365-2389.1993.tb00463.x.

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46

Silva Junior, João José da, Alberto Colombo, Geraldo Cézar Oliveira, Bruno Montoani Silva, and José Eduardo Juliaci Eugênio. "Estimation of tropical soils’ hydraulic properties with inverse method and tension infiltrometer field data." Ambiente e Agua - An Interdisciplinary Journal of Applied Science 15, no. 3 (May 15, 2020): 1. http://dx.doi.org/10.4136/ambi-agua.2503.

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In the last few years, many studies have been published by authors from several countries offering approximations and use of the inverse method. However, the unique environmental conditions and distinct properties of the tropical soils in Brazil require extra considerations and the need to adjust these methods to tropical soil conditions. Considering the above, this determined the parameters of the van Genuchten (1980) model (θs, θr, α, n) of the water retention curve in the soils. It also determined the parameter (Ks) of the soil’s hydraulic conductivity curve by solving an inverse problem us

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47

Moret-Fernández, David, Borja Latorre, and César González-Cebollada. "Microflowmeter–tension disc infiltrometer: Part II – Hydraulic properties estimation from transient infiltration rate analysis." Journal of Hydrology 466-467 (October 2012): 159–66. http://dx.doi.org/10.1016/j.jhydrol.2012.04.047.

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48

Matula, S., M. Miháliková, J. Lufinková, and K. Báťková. "The role of the initial soil water content in the determination of unsaturated soil hydraulic conductivity using a tension infiltrometer." Plant, Soil and Environment 61, No. 11 (June 6, 2016): 515–21. http://dx.doi.org/10.17221/527/2015-pse.

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49

V. Bagarello, M. Castellini, and M. Iovino. "INFLUENCE OF THE PRESSURE HEAD SEQUENCE ON THE SOIL HYDRAULIC CONDUCTIVITY DETERMINED WITH TENSION INFILTROMETER." Applied Engineering in Agriculture 21, no. 3 (2005): 383–91. http://dx.doi.org/10.13031/2013.18457.

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50

Yoon, Youngman, Jeong-Gyu Kim, and Seunghun Hyun. "Estimating soil water retention in a selected range of soil pores using tension disc infiltrometer data." Soil and Tillage Research 97, no. 1 (November 2007): 107–16. http://dx.doi.org/10.1016/j.still.2007.09.003.

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