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Concentration profiles for (a) Masa <span class="search-highlight">loamy</span> <span class="search-highlight">sand</span> and NaCl, (b) Masa <span class="search-highlight">loamy</span> san...

Concentration profiles for (a) Masa loamy sand and NaCl, (b) Masa loamy san...

in Effect of a Salt Crust on Evaporation from a Bare Saline Soil > Vadose Zone Journal

Published: 01 November 2006

Fig. 8. Concentration profiles for (a) Masa loamy sand and NaCl, (b) Masa loamy sand and KCl, and (c) Toyoura sand and NaCl.

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Mounding height in <span class="search-highlight">sand</span> and <span class="search-highlight">loamy</span> <span class="search-highlight">sand</span> soils for Cycle 1 (0.5 flooding days...

Mounding height in sand and loamy sand soils for Cycle 1 (0.5 flooding days...

in Application of a Coupled Overland Flow–Vadose Zone Model to Rapid Infiltration Basin Systems > Vadose Zone Journal

Published: 01 May 2012

Fig. 6. Mounding height in sand and loamy sand soils for Cycle 1 (0.5 flooding days and 6.5 drying days, C1) and Cycle 2 (three flooding days and four drying days, C2). Upper bounds indicate the mounding height after flooding, lower bounds indicate mounding height after drying, and the bar

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Simulated water-table fluctuations for coarse <span class="search-highlight">sand</span>, <span class="search-highlight">loamy</span> <span class="search-highlight">sand</span>, loam, and s...

Simulated water-table fluctuations for coarse sand, loamy sand, loam, and s...

in Simulating Water, Solute, and Heat Transport in the Subsurface with the VS2DI Software Package All rights reserved. No part of this periodical may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopying, recording, or any information storage and retrieval system, without permission in writing from the publisher. > Vadose Zone Journal

Published: 01 May 2008

F ig . 8. Simulated water-table fluctuations for coarse sand, loamy sand, loam, and silt textures (from Loheide et al., 2005 ).

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Water content vs. count ratio for sandy loam, <span class="search-highlight">loamy</span> <span class="search-highlight">sand</span>, <span class="search-highlight">sand</span>, and their c...

Water content vs. count ratio for sandy loam, loamy sand, sand, and their c...

in Neutron Probe Calibration in a Vertically Stratified Vadose Zone > Vadose Zone Journal

Published: 01 November 2004

Fig. 5. Water content vs. count ratio for sandy loam, loamy sand, sand, and their corresponding least squares fitted straight lines.

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Heave rate as a function of the temperature gradient for <span class="search-highlight">loamy</span> <span class="search-highlight">sand</span> when ∇ ...

Heave rate as a function of the temperature gradient for loamy sand when ∇ ...

in Heave and Heaving Pressure in Freezing Soils: A Unifying Theory > Vadose Zone Journal

Published: 01 February 2013

Fig. 4. Heave rate as a function of the temperature gradient for loamy sand when ∇ T is calculated either across the frozen fringe (open circles, dashed line) or between the soil surface and the zero-degree isotherm, that is, the overall temperature gradient (filled circles, solid line).

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Measured water content spatial distribution in the <span class="search-highlight">loamy</span> <span class="search-highlight">sand</span> field at Beso...

Measured water content spatial distribution in the loamy sand field at Beso...

in Impact of Water Regime and Growing Conditions on Soil–Plant Interactions: From Single Plant to Field Scale > Vadose Zone Journal

Published: 01 August 2012

Fig. 3. Measured water content spatial distribution in the loamy sand field at Besor in the morning after pulsed irrigation began but before daily applications started (emitter is located at x = 0, z = 0).

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Mounding height in <span class="search-highlight">loamy</span> <span class="search-highlight">sand</span> for two application cycles (C1, 0.5 flooding ...

Mounding height in loamy sand for two application cycles (C1, 0.5 flooding ...

in Application of a Coupled Overland Flow–Vadose Zone Model to Rapid Infiltration Basin Systems > Vadose Zone Journal

Published: 01 May 2012

Fig. 9. Mounding height in loamy sand for two application cycles (C1, 0.5 flooding days and 6.5 drying days; C2, three flooding days and four drying days) and two boundary conditions: overland flow or constant flux. Upper bounds indicate the mounding height after flooding, lower bounds indicate

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These soil profiles and radar records are from areas of Windsor <span class="search-highlight">loamy</span> <span class="search-highlight">sand</span> ...

These soil profiles and radar records are from areas of Windsor loamy sand ...

in Revised Ground-Penetrating Radar Soil Suitability Maps > Journal of Environmental and Engineering Geophysics

Published: 01 September 2010

Figure 3 These soil profiles and radar records are from areas of Windsor loamy sand (3A), Fairview sandy loam (3B) and Putnam silt loam (3C) soils. Windsor, Fairview, and Putnam soils are representative of soils with GPR suitability indices of 1, 3, and 4, respectively.

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Soil profiles of the <span class="search-highlight">loamy</span> <span class="search-highlight">sand</span> (LS) soil at the Kaldenkirchen field site (...

Soil profiles of the loamy sand (LS) soil at the Kaldenkirchen field site (...

in Comparison of Heterogeneous Transport Processes Observed with Electrical Resistivity Tomography in Two Soils All rights reserved. No part of this periodical may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopying, recording, or any information storage and retrieval system, without permission in writing from the publisher. > Vadose Zone Journal

Published: 01 May 2010

Fig. 1. Soil profiles of the loamy sand (LS) soil at the Kaldenkirchen field site (left) and the silty soil (S1/S2) at the Merzenhausen field site (right).

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Boundary conditions for the <span class="search-highlight">loamy</span> <span class="search-highlight">sand</span> (LS) soil (left) and the silty soil ...

Boundary conditions for the loamy sand (LS) soil (left) and the silty soil ...

Published: 01 May 2010

Fig. 3. Boundary conditions for the loamy sand (LS) soil (left) and the silty soil (S1 and S2) (right); EC tracer = electrical conductivity of the applied tracer, EC w = solute electrical conductivity.

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Observed and fitted soil-water retention curves (SWRCs) for a <span class="search-highlight">loamy</span> <span class="search-highlight">sand</span> (L...

Observed and fitted soil-water retention curves (SWRCs) for a loamy sand (L...

in Performance Evaluation of Models That Describe the Soil Water Retention Curve between Saturation and Oven Dryness All rights reserved. No part of this periodical may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopying, recording, or any information storage and retrieval system, without permission in writing from the publisher. > Vadose Zone Journal

Published: 01 February 2008

F ig . 4. Observed and fitted soil-water retention curves (SWRCs) for a loamy sand (LS), a silt loam (SiL), and a clay (C). Models are: Campbell and Shiozawa (CS); Rossi and Nimmo four-parameter sum (RN1); Rossi and Nimmo three-parameter junction (RN2); Fayer and Simmons modified Brooks–Corey

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Temporal change in the evaporation rate for (a) Masa <span class="search-highlight">loamy</span> <span class="search-highlight">sand</span> and NaCl (b...

Temporal change in the evaporation rate for (a) Masa loamy sand and NaCl (b...

in Effect of a Salt Crust on Evaporation from a Bare Saline Soil > Vadose Zone Journal

Published: 01 November 2006

Fig. 6. Temporal change in the evaporation rate for (a) Masa loamy sand and NaCl (b) Masa loamy sand and KCl, and (c) Toyoura sand and NaCl. In (a), numerical solutions are for Column 3; r sc is the resistivity of the salt crust; half and quarter dispersivity is in reference

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Experimental results for the <span class="search-highlight">loamy</span> <span class="search-highlight">sand</span> soil at 28°C using two different in...

Experimental results for the loamy sand soil at 28°C using two different in...

in Characterization of Nitrogen Transformations, Sorption and Volatilization Processes In Urea Fertilized Soils > Vadose Zone Journal

Published: 01 May 2005

Fig. 6. Experimental results for the loamy sand soil at 28°C using two different initial levels of urea. Squares represent volatilized amounts of ammonia for experiments using an initial urea concentration of 2 g/kg, and circles represent volatilized amounts of ammonia for experiments using

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The measured and estimated soil water retention curves of Troup <span class="search-highlight">loamy</span> <span class="search-highlight">sand</span> ...

The measured and estimated soil water retention curves of Troup loamy sand ...

in Estimating Soil Water Retention Curve from Particle-Size Distribution Data Based on Polydisperse Sphere Systems > Vadose Zone Journal

Published: 01 November 2004

Fig. 12. The measured and estimated soil water retention curves of Troup loamy sand (code no. 1012) (a) with fitted α and (b) with theoretical α. The fitted α value is higher than the theoretical one. TIS, totally impenetrable spheres model; FPS, fully penetrable spheres model; and VG, van

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Soil water retention curve for Masa <span class="search-highlight">loamy</span> <span class="search-highlight">sand</span> and Tohaku loam.

Soil water retention curve for Masa loamy sand and Tohaku loam.

in A Transient Evaporation Method for Determining Soil Hydraulic Properties at Low Pressure > Vadose Zone Journal

Published: 01 August 2003

Fig. 5. Soil water retention curve for Masa loamy sand and Tohaku loam.

Journal Article

Assessing Changes in Elemental Mass as a Result of Chemical Weathering of Granodiorite in a Mediterranean (Hot Summer) Climate

Gary H. Girty, Jeffrey Marsh, Aron Meltzner, Jessica R. McConnell, Damon Nygren, Joanna Nygren, Gail M. Prince, Kesler Randall, Diane Johnson, Brett Heitman, Jennifer Nielsen

Journal: Journal of Sedimentary Research

Publisher: SEPM Society for Sedimentary Geology

Published: 01 May 2003

Journal of Sedimentary Research (2003) 73 (3): 434–443.

DOI: https://doi.org/10.1306/091802730434

... coarse loamy sand make up a well developed weathering profile that developed on a Cretaceous granodiorite lying within a Mediterranean (hot summer) climatic belt in the Peninsular Ranges of southern California, U.S.A. Textural, modal, and chemical data indicate that in the friable granodiorite...

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Trench exposures in Tory and Arshan fault scarps, logged by Belousov and De...

in FAULT SCARPS AND PREHISTORIC EARTHQUAKES IN THE TUNKA FAULT ( southwestern Baikal region ) > Russian Geology and Geophysics

Published: 01 June 2003

Fig. 4. Trench exposures in Tory and Arshan fault scarps, logged by Belousov and Del’yansky (T7, T6, T11, 1990), Chipizubov, Smekalin, and Del’yansky (ZT3, 1997), Smekalin, Ruzhich, and Del’yansky (A2, A3, 1997). 1 — modern topsoil; 2 — buried organic-bearing loam and loamy sand; 3 — loam

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Simplified sections of trench sides. 1 – soil and vegetative cover; 2 –...

in FAULT SCARPS AND THE CAUSATIVE PREHISTORIC EARTHQUAKES IN THE MAIN SAYAN FAULT ZONE > Russian Geology and Geophysics

Published: 01 June 1999

Fig. 5. Simplified sections of trench sides. 1 – soil and vegetative cover; 2 – cultural layer; 3, 4 – deeply ( 3 ) and moderately ( 4 ) buried soils; 5 – sand and loamy sand; 6 – loamy sand and detritus; 7 – clay and sandy loam; 8 – loamy sand and sandy loam; 9 – debris

Journal Article

Impact of Water Regime and Growing Conditions on Soil–Plant Interactions: From Single Plant to Field Scale

S. Assouline, M. Möller, A Furman, K Narkis, A. Silber

Journal: Vadose Zone Journal

Publisher: Soil Science Society of America

Published: 01 August 2012

Vadose Zone Journal (2012) 11 (3): vzj2012.0006.

DOI: https://doi.org/10.2136/vzj2012.0006

...Fig. 3. Measured water content spatial distribution in the loamy sand field at Besor in the morning after pulsed irrigation began but before daily applications started (emitter is located at x = 0, z = 0). ...

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Journal Article

Comparison of Heterogeneous Transport Processes Observed with Electrical Resistivity Tomography in Two Soils All rights reserved. No part of this periodical may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopying, recording, or any information storage and retrieval system, without permission in writing from the publisher.

S. Garré, J. Koestel, T. Günther, M. Javaux, J. Vanderborght, H. Vereecken

Journal: Vadose Zone Journal

Publisher: Soil Science Society of America

Published: 01 May 2010

Vadose Zone Journal (2010) 9 (2): 336–349.

DOI: https://doi.org/10.2136/vzj2009.0086

...Fig. 1. Soil profiles of the loamy sand (LS) soil at the Kaldenkirchen field site (left) and the silty soil (S1/S2) at the Merzenhausen field site (right). ...

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