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Relevant bibliographies by topics / Wilting point permanent

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Journal articles

Academic literature on the topic 'Wilting point permanent'

Author: Grafiati

Published: 4 June 2021

Last updated: 1 February 2022

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Journal articles on the topic "Wilting point permanent"

1

Obi, Chinedu Innocent, Jude C. Obi, and Emmanuel U. Onweremadu. "Modeling of Permanent Wilting from Particle Size Fractions of Coastal Plain Sands Soils in Southeastern Nigeria." ISRN Soil Science 2012 (July 31, 2012): 1–5. http://dx.doi.org/10.5402/2012/198303.

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Permanent wilting points in soils have been found to correlate significantly with particle size fractions. This study was conducted to establish functional relationship between soil particle size fractions and permanent wilting point of soils of coastal plain sands in southeastern Nigeria. A total of 102 surface samples were collected from three different dominantly Ultisols toposequences (i.e., 34 samples from each). Permanent wilting point experiment was carried out in pots with the 102 samples in the greenhouse while the particle size analysis was carried out in the laboratory. There was si

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2

Laktionova, T., and S. Nakisko. "Particle Size Distribution as a Basic Characteristic for Pedotransfer Prediction of Permanent Wilting Point." Agricultural Science and Practice 1, no. 1 (2014): 13–19. http://dx.doi.org/10.15407/agrisp1.01.013.

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The permanent wilting point (PWP) belongs to the basic soil hydrological constants and plays the important role in an estimation of the natural or irrigating moisture availability to agricultural plants. Direct measurement of hydrological parameters demands signifi cant amount of time, efforts and equipment. Pedotransfer functions (PTF) can provide an alternative way to an estimation of these parameters indirectly, by calculation, using accessible parameters of the basic soil properties in soil databases. Aim. To work out new PTF for an estimation of permanent wilting point in the chernozem so

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3

Dayana, Ingri, Bandi Hermawan, Yudhi Harini Bertham, and Dwi Wahyuni Ganefianti. "Effects of Arbuscular Mycorrhiza Fungi and Coffee Pulp Compost in Improving Soil Water Uptake by Chilli Around the Permanent Wilting Point Conditions." TERRA : Journal of Land Restoration 3, no. 1 (2020): 23–26. http://dx.doi.org/10.31186/terra.3.1.23-26.

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Soil water availability to the plants is a range of water content between the field capacity and the permanent wilting point (PWP) conditions. The PWP is defined as the lower limit of soil water content that the plant can extract water from the soil as indicated by the symptoms of wilting plants. This is because plant roots are unable to penetrate the soil micropores that contain the water. The study aims to analyze the effects of arbuscular mycorrhizal fungi (AMF) and compost in enhancing soil water absorption by the plant when the water content is close to the permanent wilting point. Four d

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4

Bussiéres, P., J. Hostalery, and A. Battilani. "SIMPLE DEVICE FOR ESTIMATING SOIL WATER CONTENT AT PERMANENT WILTING POINT." Acta Horticulturae, no. 613 (September 2003): 163–68. http://dx.doi.org/10.17660/actahortic.2003.613.21.

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5

Bechtold, Michel, Ullrich Dettmann, Lena Wöhl, Wolfgang Durner, Arndt Piayda, and Bärbel Tiemeyer. "Comparing Methods for Measuring Water Retention of Peat Near Permanent Wilting Point." Soil Science Society of America Journal 82, no. 3 (2018): 601–5. http://dx.doi.org/10.2136/sssaj2017.10.0372.

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6

Filgueiras, Roberto, Vinicius Mendes Rodrigues de Oliveira, Fernando França da Cunha, Everardo Chartuni Mantovani, and Epitácio Jose de Souza. "MODELOS DE CURVA DE RETENÇÃO DE ÁGUA NO SOLO." IRRIGA 1, no. 1 (2018): 115. http://dx.doi.org/10.15809/irriga.2016v1n1p115-120.

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MODELOS DE CURVA DE RETENÇÃO DE ÁGUA NO SOLO ROBERTO FILGUEIRAS¹; VINICIUS MENDES RODRIGUES DE OLIVEIRA²; FERNANDO FRANÇA DA CUNHA³; EVERARDO CHARTUNI MANTOVANI³ E EPITÁCIO JOSE DE SOUZA4 1 Doutorando em Engenharia Agrícola, Universidade Federal de Viçosa. Viçosa, MG. Email: roberto.f.filgueiras@ufv.br² Doutorando em Engenharia Agrícola, Universidade Federal de Viçosa. Viçosa, MG³ Prof. Dr. Departamento de Engenharia Agrícola, Universidade Federal de Viçosa. Viçosa, MG4 Doutorando em Agronomia (Ciência do Solo), UNESP. Ilha Solteira, SP. 1 RESUMO O objetivo deste trabalho foi comparar a umidad

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7

., Bilal Cemek, Ramazan Meral ., Mehmet Apan ., and Hasan Merdun . "Pedotransfer Functions for the Estimation of the Field Capacity and Permanent Wilting Point." Pakistan Journal of Biological Sciences 7, no. 4 (2004): 535–41. http://dx.doi.org/10.3923/pjbs.2004.535.541.

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8

Chen, Chong, Hu Zhou, Jianying Shang, Kelin Hu, and Tusheng Ren. "Estimation of soil water content at permanent wilting point using hygroscopic water content." European Journal of Soil Science 71, no. 3 (2019): 392–98. http://dx.doi.org/10.1111/ejss.12887.

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9

Silva, Bruno Montoani, Érika Andressa da Silva, Geraldo César de Oliveira, Mozart Martins Ferreira, and Milson Evaldo Serafim. "Plant-available soil water capacity: estimation methods and implications." Revista Brasileira de Ciência do Solo 38, no. 2 (2014): 464–75. http://dx.doi.org/10.1590/s0100-06832014000200011.

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The plant-available water capacity of the soil is defined as the water content between field capacity and wilting point, and has wide practical application in planning the land use. In a representative profile of the Cerrado Oxisol, methods for estimating the wilting point were studied and compared, using a WP4-T psychrometer and Richards chamber for undisturbed and disturbed samples. In addition, the field capacity was estimated by the water content at 6, 10, 33 kPa and by the inflection point of the water retention curve, calculated by the van Genuchten and cubic polynomial models. We found

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10

Hohenegger, Cathy, and Bjorn Stevens. "The role of the permanent wilting point in controlling the spatial distribution of precipitation." Proceedings of the National Academy of Sciences 115, no. 22 (2018): 5692–97. http://dx.doi.org/10.1073/pnas.1718842115.

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Convection-permitting simulations on an idealized land planet are performed to understand whether soil moisture acts to support or impede the organization of convection. Initially, shallow circulations driven by differential radiative cooling induce a self-aggregation of the convection into a single band, as has become familiar from simulations over idealized sea surfaces. With time, however, the drying of the nonprecipitating region induces a reversal of the shallow circulation, drawing the flow at low levels from the precipitating to the nonprecipitating region. This causes the precipitating

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