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Variation in matric potential at field capacity in stony soils of fluvial and alluvial fans

Geoderma, 2021
Field capacity of soil is fundamental for many agronomic management decisions, as well as for hydrological and environmental models. Around the world, field capacity is assumed to occur at defined matric potentials, −10 kPa and –33 kPa being common ...
Balin B Robertson   +2 more
exaly   +2 more sources

Distance-Aware Precoding for Near-Field Capacity Improvement in XL-MIMO

IEEE Vehicular Technology Conference, 2021
Extremely large-scale MIMO (XL-MIMO) communication is a promising technology to improve the capacity for future 6G networks. With a very large number of antennas, the near-field property of XL-MIMO systems becomes significant.
Zidong Wu   +3 more
semanticscholar   +1 more source

An Integration Approach for Mapping Field Capacity of China Based on Multi-Source Soil Datasets

open access: yesWater (Switzerland), 2018
Field capacity is one of the most important soil hydraulic properties in water cycle, agricultural irrigation, and drought monitoring. It is difficult to obtain the distribution of field capacity on a large scale using manual measurements that are both ...
Guihua Lu, Zhiyong Wu, Hai He
exaly   +2 more sources

Comparative Analysis of MLR, ANN, and ANFIS Models for Prediction of Field Capacity and Permanent Wilting Point for Bafra Plain Soils

Communications in Soil Science and Plant Analysis, 2020
Soil hydraulic parameters like moisture content at field capacity and permanent wilting point constitute significant input parameters of various biophysical models and agricultural practices (irrigation timing and amount of irrigation to be applied).
Sevda Tasan, Yusuf Demir
exaly   +2 more sources

Application of firefly algorithm-based support vector machines for prediction of field capacity and permanent wilting point

Soil and Tillage Research, 2017
Mohammad Ali Ghorbani   +2 more
exaly   +2 more sources

An analytic description of field capacity and its application in crop production

Geoderma, 2018
It has been established for decades that soil water field capacity (FC) includes four main components: drainage rate or flux (q), drainage time from saturation (t), soil water content in the drained zone (θ), and drainage depth (Z).
W Daniel Reynolds
exaly   +2 more sources

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