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1

da Silva, A. P., B. D. Kay, and E. Perfect. "Characterization of the Least Limiting Water Range of Soils." Soil Science Society of America Journal 58, no. 6 (1994): 1775. http://dx.doi.org/10.2136/sssaj1994.03615995005800060028x.

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2

Pulido‐Moncada, Mansonia, and Lars J. Munkholm. "Limiting Water Range: A Case Study for Compacted Subsoils." Soil Science Society of America Journal 83, no. 4 (2019): 982–92. http://dx.doi.org/10.2136/sssaj2019.01.0023.

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3

da Silva, Alvaro Pires, and B. D. Kay. "Effect of Soil Water Content Variation on the Least Limiting Water Range." Soil Science Society of America Journal 61, no. 3 (1997): 884–88. http://dx.doi.org/10.2136/sssaj1997.03615995006100030024x.

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4

Leão, Tairone Paiva. "Water retention and penetration resistance equations for the least limiting water range." Scientia Agricola 76, no. 2 (2019): 172–78. http://dx.doi.org/10.1590/1678-992x-2017-0280.

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5

Rodrigues, Tallyta Ramalho, Derblai Casaroli, Adão Wagner Pêgo Evangelista, and José Alves Júnior. "Water availability to soybean crop as a function of the least limiting water range and evapotranspiration1." Pesquisa Agropecuária Tropical 47, no. 2 (2017): 161–67. http://dx.doi.org/10.1590/1983-40632016v4743746.

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ABSTRACT Irrigation management aimed at optimal production has been based only on the water factor. However, in addition to the water potential of the soil, factors such as soil penetration resistance and soil O2 diffusion rate also affect plant growth and interfere with water absorption, even if moisture is within the available water range. This study aimed at quantifying the least limiting water range and demonstrating its potential in soil and water management in irrigated agriculture. In order to determine the least limiting water range, soil water retention curves and soil resistance to p
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6

Kahlon, Meharban S., and Karitika Chawla. "Effect of tillage practices on least limiting water range in Northwest India." International Agrophysics 31, no. 2 (2017): 183–94. http://dx.doi.org/10.1515/intag-2016-0051.

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Abstract Tillage practices affect mechanical and hydrological characteristics of soil and subsequently the least limiting water range. This quality indicator under the wheat-maize system of northwest India has not been studied yet. The treatments included four tillage modes, namely conventional tillage, no-tillage without residue, no-tillage with residue, and deep tillage as well as three irrigation regimes based on the irrigation water and pan evaporation ratio i.e. 1.2, 0.9, and 0.6. The experiment was conducted in a split plot design with three replications. At the end of cropping system, t
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7

Calonego, Juliano Carlos, and Ciro Antonio Rosolem. "Least limiting water range in soil under crop rotations and chiseling." Revista Brasileira de Ciência do Solo 35, no. 3 (2011): 759–71. http://dx.doi.org/10.1590/s0100-06832011000300012.

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Soil water availability to plants is affected by soil compaction and other variables. The Least Limiting Water Range (LLWR) comprises soil physical variables affecting root growth and soil water availability, and can be managed by either mechanical or biological methods. There is evidence that effects of crop rotations could last longer than chiseling, so the objective of this study was to assess the effect of soil chiseling or growing cover crops under no-till (NT) on the LLWR. Crop rotations involving triticale (X Triticosecale) and sunflower (Helianthus annuus) in the fall-winter associated
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8

Leao, Tairone Paiva, Alvaro Pires da Silva, Ed Perfect, and Cassio Antonio Tormena. "An Algorithm for Calculating the Least Limiting Water Range of Soils." Agronomy Journal 97, no. 4 (2005): 1210–15. http://dx.doi.org/10.2134/agronj2004.0229.

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9

de Oliveira, Ingrid Nehmi, Zigomar Menezes de Souza, Lenon Henrique Lovera, et al. "Least limiting water range as influenced by tillage and cover crop." Agricultural Water Management 225 (November 2019): 105777. http://dx.doi.org/10.1016/j.agwat.2019.105777.

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10

Ferreira, Camila Jorge Bernabé, Lincoln Zotarelli, Cássio Antonio Tormena, Libby R. Rens, and Diane L. Rowland. "Effects of water table management on least limiting water range and potato root growth." Agricultural Water Management 186 (May 2017): 1–11. http://dx.doi.org/10.1016/j.agwat.2017.02.020.

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11

Klein, Claudia, and Vilson Antonio Klein. "Least limiting water range under no-tillage system and maize grain yield." Científica 43, no. 2 (2015): 179. http://dx.doi.org/10.15361/1984-5529.2015v43n2p179-187.

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12

da Silva, Alvaro Pires, and B. D. Kay. "Estimating the Least Limiting Water Range of Soils from Properties and Management." Soil Science Society of America Journal 61, no. 3 (1997): 877–83. http://dx.doi.org/10.2136/sssaj1997.03615995006100030023x.

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13

Sato, Michel Keisuke, Herdjania Veras de Lima, Raphael Leone da Cruz Ferreira, Sueli Rodrigues, and Álvaro Pires da Silva. "Least limiting water range for oil palm production in Amazon region, Brazil." Scientia Agricola 74, no. 2 (2017): 148–56. http://dx.doi.org/10.1590/1678-992x-2015-0408.

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14

Mishra, Amit Kumar, Pramila Aggarwal, Ranjan Bhattacharyya, T. K. Das, A. R. Sharma, and Ravender Singh. "Least limiting water range for two conservation agriculture cropping systems in India." Soil and Tillage Research 150 (July 2015): 43–56. http://dx.doi.org/10.1016/j.still.2015.01.003.

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15

De Vares Rossetti, Karina, and José Frederico Centurion. "Least limiting water range in Oxisols under different levels of machine traffic." Comunicata Scientiae 8, no. 2 (2018): 337–46. http://dx.doi.org/10.14295/cs.v8i2.2423.

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This work aimed, to evaluate the structural behavior of Oxisols based on the least limiting water range (LLWR) and establish relations with corn crop. The experiment was carried out in a randomized block design with five treatments and four replications. Soil samples collected at the layer of 0-0.20 m depth in a Haplustox (LVd) and an Eutrustox (LVef) were used. The compaction treatments consisted of T0= no additional compaction; T1 and T2= two and four passes with a 4 t tractor, respectively; T3 and T4 = two and four passes with a 10 t tractor, respectively. The range of LLWR variation in the
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16

van Lier, Quirijn de Jong, and Paulo Ivonir Gubiani. "BEYOND THE “LEAST LIMITING WATER RANGE”: RETHINKING SOIL PHYSICS RESEARCH IN BRAZIL." Revista Brasileira de Ciência do Solo 39, no. 4 (2015): 925–39. http://dx.doi.org/10.1590/01000683rbcs20140596.

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As opposed to objective definitions in soil physics, the subjective term “soil physical quality” is increasingly found in publications in the soil physics area. A supposed indicator of soil physical quality that has been the focus of attention, especially in the Brazilian literature, is the Least Limiting Water Range (RLL), translated in Portuguese as "Intervalo Hídrico Ótimo" or IHO. In this paper the four limiting water contents that define RLLare discussed in the light of objectively determinable soil physical properties, pointing to inconsistencies in the RLLdefinition and calculation. It
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17

Safadoust, A., P. Feizee, A. A. Mahboubi, B. Gharabaghi, M. R. Mosaddeghi, and B. Ahrens. "Least limiting water range as affected by soil texture and cropping system." Agricultural Water Management 136 (April 2014): 34–41. http://dx.doi.org/10.1016/j.agwat.2014.01.007.

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18

Asgarzadeh, Hossein, Mohammad Reza Mosaddeghi, Ali Akbar Mahboubi, Akram Nosrati, and Anthony Roger Dexter. "Soil water availability for plants as quantified by conventional available water, least limiting water range and integral water capacity." Plant and Soil 335, no. 1-2 (2010): 229–44. http://dx.doi.org/10.1007/s11104-010-0410-6.

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19

Zou, C., R. Sands, G. Buchan, and I. Hudson. "Least limiting water range: a potential indicator of physical quality of forest soils." Soil Research 38, no. 5 (2000): 947. http://dx.doi.org/10.1071/sr99108.

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The interactions of the 4 basic soil physical properties—volumetric water content, matric potential, soil strength, and air-filled porosity—were investigated over a range of contrasting textures and for 3 compaction levels of 4 forest soils in New Zealand, using linear and non-linear regression methods. Relationships among these properties depended on texture and bulk density. Soil compaction increased volumetric water contents at field capacity, at wilting point, and at the water contents associated with restraining soil strength values, but decreased the water content when air-filled porosit
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20

Passos, Renato Ribeiro, Liovando Marciano da Costa, Igor Rodrigues de Assis, et al. "Least limiting water range of Udox soil under degraded pastures on different sun-exposed faces." International Agrophysics 31, no. 3 (2017): 393–400. http://dx.doi.org/10.1515/intag-2016-0066.

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AbstractThe efficient use of water is increasingly important and proper soil management, within the specificities of each region of the country, allows achieving greater efficiency. The South and Caparaó regions of Espírito Santo, Brazil are characterized by relief of ‘hill seas’ with differences in the degree of pasture degradation due to sun exposure. The objective of this study was to evaluate the least limiting water range in Udox soil under degraded pastures with two faces of exposure to the sun and three pedoenvironments. In each pedoenvironment, namely Alegre, Celina, and Café, two area
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21

Stöven, T., T. Tanhua, M. Hoppema, and J. L. Bullister. "Perspectives of transient tracer applications and limiting cases." Ocean Science 11, no. 5 (2015): 699–718. http://dx.doi.org/10.5194/os-11-699-2015.

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Abstract. Currently available transient tracers have different application ranges that are defined by their temporal input (chronological transient tracers) or their decay rate (radioactive transient tracers). Transient tracers range from tracers for highly ventilated water masses such as sulfur hexafluoride (SF6) through tritium (3H) and chlorofluorocarbons (CFCs) up to tracers for less ventilated deep ocean basins such as argon-39 (39Ar) and radiocarbon (14C). In this context, highly ventilated water masses are defined as water masses that have been in contact with the atmosphere during the
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22

Tavanti, Renan F. R., Onã da S. Freddi, Tauan R. Tavanti, Adriel Rigotti, and Wellington de A. Magalhães. "PEDOFUNCTIONS APPLIED TO THE LEAST LIMITING WATER RANGE TO ESTIMATE SOIL WATER CONTENT AT SPECIFIC POTENTIALS." Engenharia Agrícola 39, no. 4 (2019): 444–56. http://dx.doi.org/10.1590/1809-4430-eng.agric.v39n4p444-456/2019.

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23

Lima, Claudia Liane, Luis Akiyoshi Suzuki, Dalvan José Reinert, and José Miguel Reichert. "Least limiting water range and degree of compactness of soils under no- tillage." Bioscience Journal 31, no. 4 (2015): 1071–80. http://dx.doi.org/10.14393/bj-v31n4a2015-26218.

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24

Gonçalves, Wainer Gomes, Eduardo da Costa Severiano, Fabiano Guimarães Silva, Kátia Aparecida de Pinho Costa, Wellingthon da Silva Guimarães-Junnyor, and Gabriel Bressiani Melo. "Least limiting water range in assessing compaction in a Brazilian Cerrado latosol growing sugarcane." Revista Brasileira de Ciência do Solo 38, no. 2 (2014): 432–43. http://dx.doi.org/10.1590/s0100-06832014000200008.

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In the south-central region of Brazil, there is a trend toward reducing the sugarcane inter-harvest period and increasing traffic of heavy harvesting machinery on soil with high water content, which may intensify the compaction process. In this study, we assessed the structural changes of a distroferric Red Latosol (Oxisol) by monitoring soil water content as a function of the Least Limiting Water Range (LLWR) and quantified its effects on the crop yield and industrial quality of the first ratoon crop of sugarcane cultivars with different maturation cycles. Three cultivars (RB 83-5054, RB 84-5
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25

CHEN Xuewen, 陈学文, 王农 WANG Nong, 时秀焕 SHI Xiuhuan, et al. "Evaluating tillage practices impacts on soil organic carbon based on least limiting water range." Acta Ecologica Sinica 33, no. 9 (2013): 2676–83. http://dx.doi.org/10.5846/stxb201201180112.

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26

Betz, C. L., R. R. Allmaras, S. M. Copeland, and G. W. Randall. "Least Limiting Water Range: Traffic and Long-term Tillage Influences in a Webster Soil." Soil Science Society of America Journal 62, no. 5 (1998): 1384–93. http://dx.doi.org/10.2136/sssaj1998.03615995006200050034x.

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27

da Silva, Alvaro Pires, and B. D. Kay. "Linking process capability analysis and least limiting water range for assessing soil physical quality." Soil and Tillage Research 79, no. 2 (2004): 167–74. http://dx.doi.org/10.1016/j.still.2004.07.005.

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28

Leão, Tairone Paiva, and Alvaro Pires da Silva. "A simplified Excel® algorithm for estimating the least limiting water range of soils." Scientia Agricola 61, no. 6 (2004): 649–54. http://dx.doi.org/10.1590/s0103-90162004000600013.

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The least limiting water range (LLWR) of soils has been employed as a methodological approach for evaluation of soil physical quality in different agricultural systems, including forestry, grasslands and major crops. However, the absence of a simplified methodology for the quantification of LLWR has hampered the popularization of its use among researchers and soil managers. Taking this into account this work has the objective of proposing and describing a simplified algorithm developed in Excel® software for quantification of the LLWR, including the calculation of the critical bulk density, at
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29

Moreira, Wagner Henrique, Cássio Antônio Tormena, Edner Betioli Junior, Getulio Coutinho Figueiredo, Álvaro Pires da Silva, and Neyde Fabíola Balarezo Giarola. "Quantification of the least limiting water range in an oxisol using two methodological strategies." Revista Brasileira de Ciência do Solo 38, no. 6 (2014): 1772–83. http://dx.doi.org/10.1590/s0100-06832014000600012.

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The least limiting water range (LLWR) has been used as an indicator of soil physical quality as it represents, in a single parameter, the soil physical properties directly linked to plant growth, with the exception of temperature. The usual procedure for obtaining the LLWR involves determination of the water retention curve (WRC) and the soil resistance to penetration curve (SRC) in soil samples with undisturbed structure in the laboratory. Determination of the WRC and SRC using field measurements (in situ ) is preferable, but requires appropriate instrumentation. The objective of this study w
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30

Lapen, D. R., G. C. Topp, E. G. Gregorich, and W. E. Curnoe. "Least limiting water range indicators of soil quality and corn production, eastern Ontario, Canada." Soil and Tillage Research 78, no. 2 (2004): 151–70. http://dx.doi.org/10.1016/j.still.2004.02.004.

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31

Olibone, D., A. P. Encide-Olibone, and C. A. Rosolem. "Least limiting water range and crop yields as affected by crop rotations and tillage." Soil Use and Management 26, no. 4 (2010): 485–93. http://dx.doi.org/10.1111/j.1475-2743.2010.00301.x.

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32

Keller, T., A. P. da Silva, C. A. Tormena, et al. "SoilFlex-LLWR: linking a soil compaction model with the least limiting water range concept." Soil Use and Management 31, no. 2 (2015): 321–29. http://dx.doi.org/10.1111/sum.12175.

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33

Haghighi Fashi, Fereshte, Manouchehr Gorji, and Forood Sharifi. "Least limiting water range for different soil management practices in dryland farming in Iran." Archives of Agronomy and Soil Science 63, no. 13 (2017): 1814–22. http://dx.doi.org/10.1080/03650340.2017.1308688.

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34

Beutler, Amauri Nelson, José Frederico Centurion, Alvaro Pires da Silva, Maria Aparecida Pessôa da Cruz Centurion, Cristian Luarte Leonel, and Onã da Silva Freddi. "Soil compaction by machine traffic and least limiting water range related to soybean yield." Pesquisa Agropecuária Brasileira 43, no. 11 (2008): 1591–600. http://dx.doi.org/10.1590/s0100-204x2008001100019.

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The research aimed to evaluate machine traffic effect on soil compaction and the least limiting water range related to soybean cultivar yields, during two years, in a Haplustox soil. The six treatments were related to tractor (11 Mg weight) passes by the same place: T0, no compaction; and T1*, 1; T1, 1; T2, 2; T4, 4 and T6, 6. In the treatment T1*, the compaction occurred when soil was dried, in 2003/2004, and with a 4 Mg tractor in 2004/2005. Soybean yield was evaluated in relation to soil compaction during two agricultural years in completely randomized design (compaction levels); however, i
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35

Wilson, Marcelo Germán, María Carolina Sasal, and Octavio Pedro Caviglia. "Critical bulk density for a Mollisol and a Vertisol using least limiting water range:." Geoderma 192 (January 2013): 354–61. http://dx.doi.org/10.1016/j.geoderma.2012.05.021.

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36

McKenzie, D. C., and A. B. McBratney. "Cotton root growth in a compacted Vertisol (Grey Vertosol). I. Prediction using strength measurements and 'limiting water ranges'." Soil Research 39, no. 5 (2001): 1157. http://dx.doi.org/10.1071/sr99118.

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The shear strength of a Vertisol under a broad range of compaction conditions has been related to ‘non-limiting water range’ (NLWR), ‘partially limiting water range’ (PLWR), and ‘least-limiting water range’ (LLWR) estimates for the growth of cotton roots. These factors indicate the soil water content range that land managers should aim to maintain so that root growth limitations caused by excessive hardness and poor aeration are minimised. The proportion of macropores available for root extension as the bulk soil becomes too anaerobic and/or hard for their growth has been quantified via a re-a
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37

Chen, Guihua, Ray R. Weil, and Robert L. Hill. "Effects of compaction and cover crops on soil least limiting water range and air permeability." Soil and Tillage Research 136 (March 2014): 61–69. http://dx.doi.org/10.1016/j.still.2013.09.004.

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38

Fidalski, Jonez, Cássio Antonio Tormena, and Álvaro Pires da Silva. "Least limiting water range and physical quality of soil under groundcover management systems in citrus." Scientia Agricola 67, no. 4 (2010): 448–53. http://dx.doi.org/10.1590/s0103-90162010000400012.

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Machinery-based farming operations used for perennial fruit crops often damage soils, particularly if the soil is wet and prone to compaction. We hypothesized that perennial vegetation growing in the interrows of orange orchards can mitigate the soil physical degradation from machinery traffic. The objective of this study was to investigate the effects of different groundcover management systems on the soil physical quality indicators including the least limiting water range (LLWR). An experiment was started in 1993 in a Typic Paleudult to evaluate three groundcover management systems: Bahia g
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39

Jones, E. E., D. A. Bienkowski, and A. Stewart. "The importance of water potential range tolerance as a limiting factor onTrichodermaspp. biocontrol ofSclerotinia sclerotiorum." Annals of Applied Biology 168, no. 1 (2015): 41–51. http://dx.doi.org/10.1111/aab.12240.

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40

da Silva, Alvaro Pires, and B. D. Kay. "The sensitivity of shoot growth of corn to the least limiting water range of soils." Plant and Soil 184, no. 2 (1996): 323–29. http://dx.doi.org/10.1007/bf00010461.

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41

Filho, Oswaldo Julio Vischi, Zigomar Menezes de Souza, Gustavo Soares de Souza, Reginaldo Barbosa da Silva, José Luiz Rodrigues Torres, and Márcio Emanuel de Lima. "Physical attributes and limiting water range as soil quality indicators after mechanical harvesting of sugarcane." Australian Journal of Crop Science 11, no. 02 (2017): 169–76. http://dx.doi.org/10.21475/ajcs.17.11.02.p215.

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42

Steinhoff, H. J., A. Redhardt, K. Lieutenant, et al. "High Precision Measurements of the Permittivity of Water in the Microwave Range." Zeitschrift für Naturforschung A 45, no. 5 (1990): 677–86. http://dx.doi.org/10.1515/zna-1990-0515.

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Abstract A practical version of a homodyne method for measuring the complex permittivity of high loss liquids at 3 and 9 GHz is described. The systematic errors are discussed in detail, because the homodyne method seems to be suitable as a simple standard method for precise measurements. The results of measurements on water in the temperature range 6 °C-45 °C are presented. The determination of all five parameters of the Debye function is possible. Finally, accuracy limiting factors for the determination of the relaxation parameters are discussed in detail
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43

Bulmer, C. E., and D. G. Simpson. "Soil compaction and water content as factors affecting the growth of lodgepole pine seedlings on sandy clay loam soil." Canadian Journal of Soil Science 85, no. 5 (2005): 667–79. http://dx.doi.org/10.4141/s04-055.

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The response of lodgepole pine (Pinus contorta Dougl. var. latifolia Engelman.) seedlings to three levels of soil compaction and water content was evaluated in raised beds filled with a sandy clay loam soil. In compacted soils, seedling survival, height, root collar diameter and root growth were reduced. Soil water regime was adjusted with irrigation to levels associated with plant moisture stress (near wilting point) and limiting soil aeration (near 0.10 m3 m-3 air-filled porosity). Soil water regime affected seedling performance, with higher survival, root collar diameter and root growth obs
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44

Asgarzadeh, H., M. R. Mosaddeghi, A. A. Mahboubi, A. Nosrati, and A. R. Dexter. "Integral energy of conventional available water, least limiting water range and integral water capacity for better characterization of water availability and soil physical quality." Geoderma 166, no. 1 (2011): 34–42. http://dx.doi.org/10.1016/j.geoderma.2011.06.009.

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45

ZANGIABADI, Mehdi, Manoochehr GORJI, Mehdi SHORAFA, Saeed KHAVARI KHORASANI, and Saeed SAADAT. "Effect of soil pore size distribution on plant-available water and least limiting water range as soil physical quality indicators." Pedosphere 30, no. 2 (2020): 253–62. http://dx.doi.org/10.1016/s1002-0160(17)60473-9.

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46

Fabricio, Tomaz Ramos, Carlos de Souza Maia Jo atilde o, L. uacute cia dos Santos Weber Oscarlina, and Holanda Campelo J. uacute nior Jos eacute. "Estimate of the least limiting water range based on relative density of an oxisol in Brazil." African Journal of Agricultural Research 11, no. 7 (2016): 516–26. http://dx.doi.org/10.5897/ajar2015.10282.

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47

Fogden, M. P. L. "PREMIGRATORY DEHYDRATION IN THE REED WARBLER ACROCEPHALVS SCIRPACEUS AND WATER AS A FACTOR LIMITING MIGRATORY RANGE." Ibis 114, no. 4 (2008): 548–52. http://dx.doi.org/10.1111/j.1474-919x.1972.tb00858.x.

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48

Soleimani, R., E. Chavoshi, H. Shirani, and I. Esfandiarpour Boroujeni. "Evaluation of Intelligence Models to Estimate the Least Limiting Water Range Using Conveniently Measurable Soil Properties." Eurasian Soil Science 54, no. 3 (2021): 389–98. http://dx.doi.org/10.1134/s1064229321030145.

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49

Pereira, Antonio Higino Frederico, Antonio Carlos Tadeu Vitorino, Eber Augusto Ferreira do Prado, Anderson Cristian Bergamin, Munir Mauad, and Heverton Ponce Arantes. "Least Limiting Water Range and Load Bearing Capacity of Soil under Types of Tractor-Trailers for Mechanical Harvesting of Green Sugarcane." Revista Brasileira de Ciência do Solo 39, no. 6 (2015): 1603–10. http://dx.doi.org/10.1590/01000683rbcs20140561.

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ABSTRACT The expansion of the sugarcane industry in Brazil has intensified the mechanization of agriculture and caused effects on the soil physical quality. The purpose of this study was to evaluate the limiting water range and soil bearing capacity of a Latossolo Vermelho distroférrico típico (Rhodic Hapludox) under the influence of different tractor-trailers used in mechanical sugarcane harvesting. The experiment was arranged in a randomized block design with five replications. The treatments consisted of green sugarcane harvesting with: harvester without trailer (T1); harvester with two tra
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Beutler, Amauri Nelson, José Frederico Centurion, and Alvaro Pires da Silva. "Soil resistance to penetration and least limiting water range for soybean yield in a haplustox from Brazil." Brazilian Archives of Biology and Technology 48, no. 6 (2005): 863–71. http://dx.doi.org/10.1590/s1516-89132005000800002.

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Abstract:
The objective of this study was determine the resistance to penetration (PR), least limiting water range (LLWR) and critical bulk density (Db-crit) for soybean yield in a medium-textured oxisol (Haplustox). The treatments represented the soil compaction by passing a tractor over the site 0, 1, 2, 4, and 6 times, with 4 replications in a randomized experimental design. Samples were collected from 0.02-0.05, 0.07-0.10 and 0.15-0.18 m depths. Soybean (Glycine max cv. Embrapa 48) was sowed in December 2002. Plant height, number of pods, aerial dry matter, weight of 100 seeds, and the yield in 3.6
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