LBA-ECO ND-11 SOIL WATER PRESSURE AND FLOW MEASUREMENTS UNDER TREE CROPS

2007 ◽  
Author(s):  
J. LEHMANN ◽  
A. RENCK
Keyword(s):  
Soil Water ◽  
Water Pressure ◽  
Flow Measurements ◽  
Tree Crops

Modeling of plant water uptake in two distinct forest stands using whole-plant capacitance approach

2021 ◽  
Author(s):  
Veronika Skalova ◽  
Michal Dohnal ◽  
Jana Votrubova ◽  
Tomas Vogel ◽  
Miroslav Tesar
Keyword(s):  
Soil Water ◽  
Water Uptake ◽  
Sap Flow ◽  
Meteorological Data ◽  
Water Pressure ◽  
Thermal Dissipation ◽  
Richards Equation ◽  
Soil Drought ◽  
Flow Measurements ◽  
Whole Plant

<p>Soil-plant-atmosphere interactions are studied to improve the estimation of actual transpiration – the key part of the catchment water balance. The one-dimensional soil water flow model S1D, involving vertically distributed macroscopic root water uptake and whole-plant hydraulic capacitance, was used. The model is based on the numerical solution of Richards' equation coupled with a transient transpiration stream algorithm.</p><p>The study focuses on the catchment Liz located in the Bohemian Forest, Czech Republic. The catchment is covered with Norway spruce (Picea abies) and European beech (Fagus sylvatica). In 2020, sap flow measurements by thermal dissipation probes were conducted at both forest environments. Soil water pressure head, soil water content, and soil temperature data, as well as complete meteorological data from the nearby meteorological station, were also available for the whole period of interest.</p><p>The registered sap flow and simulated transpiration fluxes are compared with a particular attention to the different behavior of isohydric (spruce) and anisohydric (beech) trees. The model reasonably well reproduces the plant responses caused by both the high midday potential transpiration demand and the occasional soil drought.</p><p>The research is supported by the Czech Science Foundation Project No. 20-00788S.</p>

scholarly journals Analysis of Soil Water Response to Grass Transpiration

2013 ◽  
Vol 1 (No. 3) ◽  
pp. 85-98
Author(s):  
Dohnal Michal ◽  
Dušek Jaromír ◽  
Vogel Tomáš ◽  
Herza Jiří
Keyword(s):  
Soil Water ◽  
Water Uptake ◽  
Preferential Flow ◽  
Water Movement ◽  
Control Volume ◽  
Water Pressure ◽  
Lower Boundary ◽  
Root Water Uptake ◽  
Water Dynamics ◽  
Soil Water Dynamics

This paper focuses on numerical modelling of soil water movement in response to the root water uptake that is driven by transpiration. The flow of water in a lysimeter, installed at a grass covered hillslope site in a small headwater catchment, is analysed by means of numerical simulation. The lysimeter system provides a well defined control volume with boundary fluxes measured and soil water pressure continuously monitored. The evapotranspiration intensity is estimated by the Penman-Monteith method and compared with the measured lysimeter soil water loss and the simulated root water uptake. Variably saturated flow of water in the lysimeter is simulated using one-dimensional dual-permeability model based on the numerical solution of the Richards’ equation. The availability of water for the root water uptake is determined by the evaluation of the plant water stress function, integrated in the soil water flow model. Different lower boundary conditions are tested to compare the soil water dynamics inside and outside the lysimeter. Special attention is paid to the possible influence of the preferential flow effects on the lysimeter soil water balance. The adopted modelling approach provides a useful and flexible framework for numerical analysis of soil water dynamics in response to the plant transpiration.

scholarly journals Yield Component Responses of the Brachiaria brizantha Forage Grass to Soil Water Availability in the Brazilian Cerrado

Agriculture ◽  
2020 ◽  
Vol 10 (1) ◽  
pp. 13
Author(s):  
Camila Thaiana Rueda da Silva ◽  
Edna Maria Bonfim-Silva ◽  
Tonny José de Araújo da Silva ◽  
Everton Alves Rodrigues Pinheiro ◽  
Jefferson Vieira José ◽  
...  
Keyword(s):  
Soil Water ◽  
Water Availability ◽  
Water Pressure ◽  
Soil Water Potential ◽  
Yield Component ◽  
Forage Yield ◽  
Soil Water Availability ◽  
Grass Species ◽  
Forage Production ◽  
Brachiaria Brizantha

Brazil is one of the world’s largest producers of beef cattle and dairy products, which requires high forage yield to attend grass-fed animals’ demand. Among the grass species adopted in the forage production system in Brazil, the Brachiaria genus stands out. This genus comprises nearly 85% of all planted forage area. In general, forage production systems in Brazil are essentially rainfed, and thus susceptible to seasonal soil water stresses. Selecting the suitable Brachiaria cultivar for lands susceptible to periodic waterlogging and dry spells is crucial to enhance forage yield, and consequently, to reduce the environmental footprint of the livestock sector. In this research, we investigated the performance of three recent commercial Brachiaria brizantha cultivars (Piatã, BRS Paiaguás, and MG13 Braúna) extensively adopted in Brazil’s grazing systems subjected to different ranges of soil water potential. For three cutting periods, yield related-variables (e.g., plant height, leaf area, dry biomass, and water use efficiency) were measured. Our results point to the existence of a low drought-resistant trait among cultivars, indicating the need for releasing better-adapted cultivars to cope with reduced soil water availability. All cultivars achieved higher performance at soil water pressure head between −15 kPa and −25 kPa; and in general, the cultivar. Piatã showed slightly superior results to most of the treatments.

scholarly journals PRODUÇÃO E PÓS-COLHEITA DE DUAS CULTIVARES DE CEBOLA EM FUNÇÃO DA AGUA NO SOLO

Irriga ◽  
2016 ◽  
Vol 21 (4) ◽  
pp. 697-710
Author(s):  
Renato Carvalho Vilas Boas ◽  
Geraldo Magela Pereira ◽  
Joaquim Alves Lima Junior ◽  
Cândido Ferreira Oliveira Neto ◽  
Andre Luiz Pereira Silva
Keyword(s):  
Soil Water ◽  
Allium Cepa ◽  
Water Pressure ◽  
Matter Content ◽  
Dry Matter Content ◽  
Trickle Irrigation ◽  
Average Mass ◽  
Post Harvest ◽  
Soil Water Tension ◽  
Allium Cepa L

 PRODUÇÃO E PÓS-COLHEITA DE DUAS CULTIVARES DE CEBOLA EM FUNÇÃO DA AGUA NO SOLO  RENATO CARVALHO VILAS BOAS1; GERALDO MAGELA PEREIRA2; JOAQUIM ALVES DE LIMA JUNIOR3; CÂNDIDO FERREIRA OLIVEIRA NETO4 E ANDRE LUIZ PEREIRA SILVA5 1Engº Agrícola, Doutor, Departamento de Engenharia Agrícola-DEG/Universidade Federal de Lavras - UFLA/Lavras – MG, Fone: (35) 38291389, [email protected]º Agrícola, Prof. Doutor, Departamento de Engenharia Agrícola-DEG/Universidade Federal de Lavras -UFLA/Lavras – MG, Fone: (35) 38291389, [email protected]º Agrônomo, Prof. Doutor, Universidade Federal Rural da Amazônia - UFRA/Campus Capanema – PA, Fone: (91) 98160-6563, [email protected]º Agrônomo, Prof. Doutor, Universidade Federal Rural da Amazônia - UFRA/Campus Belém – PA, Fone:(91) 99148-7454, [email protected]º Agrônomo, Doutor, Universidade Estadual Paulista –UNESP/Jaboticabal – SP, Fone: (91) 98345-4940, [email protected]  1 RESUMO Objetivou-se, com este trabalho, avaliar o efeito de tensões da água no solo sobre a produção, classificação, teor de matéria seca e perda de massa de bulbos comerciais de duas cultivares de cebola, irrigadas por gotejamento. O experimento foi conduzido na área experimental do Departamento de Agricultura da Universidade Federal de Lavras com delineamento experimental em blocos casualizados, em esquema fatorial 2 x 6, com quatro repetições. Os tratamentos constituíram-se de duas cultivares de cebola, cultivar híbrida Optima F1 e cultivar não  híbrida Alfa Tropical, e seis tensões da água no solo, 15, 25, 35, 45, 60 e 75 kPa. Com os resultados concluiu-se que o híbrido Optima F1 apresentou melhores respostas com relação às seguintes características analisadas: produtividade de bulbos comerciais e massa média de bulbos comerciais. A cultivar Alfa apresentou maior teor de matéria seca e maior perda de massa durante o período de pós-colheita. Considerando o intervalo estudado (15 a 75 kPa), em ambas as cultivares deve-se irrigar no momento em que a tensão da água no solo estiver em torno de 15 kPa, na profundidade de 0,15 m, visando à obtenção de plantas mais produtivas, bulbos maiores e maior massa média de bulbos comerciais. Palavras-chave: Allium cepa L., irrigação localizada, tensão da água no solo  VILAS BOAS,R. C; PEREIRA, G. M.; LIMA JUNIOR, J. A.; OLIVEIRA NETO, C. F. E SILVA, A. L. P. PRODUCTION AND POST- HARVEST OF TWO ONION CULTIVARS IN FUNCTION OF SOIL WATER  2 ABSTRACT This work aimed at assessing the effect of different water tensions in soil on the development and production of two onion cultivars irrigated by drip system. The experiment was carried out in the experimental area of DAG/UFLA, from June to October 2008. The experimental design used was randomized block in factorial scheme 2 x 6, with four repetitions. The treatments comprised two onion cultivars, the hybrid Optima F1 and the non hybrid Alfa Tropical and six water tensions in the soil, i.e., 15, 25, 35, 45, 60 and 75 kPa.      The Optima Hybrid F1 presented the best answers regarding the following characteristics: yield of commercial bulbs and average mass of commercial bulbs . The cultivar Alfa showed higher dry matter content and increased mass loss during the post- harvest period. Considering the range studied ( 15 to 75 kPa) both cultivars should be irrigated when the water pressure in the soil is about 15 kPa at a depth of 0.15 m, in order to obtain more productive plants, larger bulbs and highest average mass of commercial bulbs . Keywords: Allium cepa L., trickle irrigation, soil water tension  

Soil-water characteristics of compacted sandy and cemented soils with and without vegetation

2015 ◽  
Vol 52 (9) ◽  
pp. 1331-1344 ◽  
Author(s):  
W.M. Yan ◽  
Guanghui Zhang
Keyword(s):  
Soil Water ◽  
Pore Water Pressure ◽  
Water Pressure ◽  
Rapid Development ◽  
Characteristic Curve ◽  
Degree Of Saturation ◽  
Material Density ◽  
Water Characteristics ◽  
Field And Laboratory Conditions ◽  
Humidity Monitoring

Experiments were undertaken to study the soil-water characteristics of compacted sandy soil (SS) and cemented soil (CS) in field and laboratory conditions. The influence of vegetation and material density on the development of negative pore-water pressure (PWP) and degree of saturation (Sr) in the studied materials was investigated. The field planting experiments demonstrated a promising survival rate of Schefflera heptaphylla in both types of material, while the (SS) promoted better growth of the seedlings than the cemented one. In the field study, PWP and Sr of the compacted SS responded noticeably and promptly to natural drying–wetting cycles. However, the responses in the CS were relatively mild. When subjected to the same drying–wetting cycles, PWP responded more slowly and to a smaller magnitude compared with that of the uncemented counterpart. In addition, Sr changed little in CS. An increase in the density of the SS promoted rapid development of negative PWP, while an opposite trend was observed for CS. Attempts have been made to explain the observations from the perspectives of material permeability and change in water content during a drying period in both soil types. Furthermore, in SS, the development of PWP (with a measurement limit of −90 kPa) was minimally affected by the presence of vegetation, while vegetation noticeably helped the development of negative PWP in CS. Bounds of the soil-water characteristic curve (SWCCs) of the studied materials were presented based on estimates from the drying and wetting scanning curves derived from the field monitoring. A corresponding laboratory study was carried out in an environmental chamber with controllable temperature and humidity. Monitoring results from the laboratory agreed qualitatively with those obtained from the field.

scholarly journals Glaciohydraulic seismic tremors on an Alpine glacier

2020 ◽  
Vol 14 (1) ◽  
pp. 287-308 ◽  
Author(s):  
Fabian Lindner ◽  
Fabian Walter ◽  
Gabi Laske ◽  
Florent Gimbert
Keyword(s):  
Water Flow ◽  
Lake Level ◽  
Seismic Waves ◽  
Water Pressure ◽  
Drainage System ◽  
Source Tracking ◽  
Lake Basin ◽  
Flow Measurements ◽  
Alpine Glacier ◽  
Subsequent Decrease

Abstract. Hydraulic processes impact viscous and brittle ice deformation. Water-driven fracturing as well as turbulent water flow within and beneath glaciers radiate seismic waves which provide insights into otherwise hard-to-access englacial and subglacial environments. In this study, we analyze glaciohydraulic tremors recorded by four seismic arrays installed in different parts of Glacier de la Plaine Morte, Switzerland. Data were recorded during the 2016 melt season including the sudden subglacial drainage of an ice-marginal lake. Together with our seismic data, discharge, lake level, and ice flow measurements provide constraints on glacier hydraulics. We find that the tremors are generated by subglacial water flow, in moulins, and by icequake bursts. The dominating process can vary on sub-kilometer and sub-daily scales. Consistent with field observations, continuous source tracking via matched-field processing suggests a gradual up-glacier progression of an efficient drainage system as the melt season progresses. The ice-marginal lake likely connects to this drainage system via hydrofracturing, which is indicated by sustained icequake signals emitted from the proximity of the lake basin and starting roughly 24 h prior to the lake drainage. To estimate the hydraulics associated with the drainage, we use tremor–discharge scaling relationships. Our analysis suggests a pressurization of the subglacial environment at the drainage onset, followed by an increase in the hydraulic radii of the conduits and a subsequent decrease in the subglacial water pressure as the capacity of the drainage system increases. The pressurization is in phase with the drop in the lake level, and its retrieved maximum coincides with ice uplift measured via GPS. Our results highlight the use of cryo-seismology for monitoring glacier hydraulics.

Soil-water characteristic curve and consolidation behavior for a compacted silt

2007 ◽  
Vol 44 (3) ◽  
pp. 266-275 ◽  
Author(s):  
Trinh Minh Thu ◽  
Harianto Rahardjo ◽  
Eng-Choon Leong
Keyword(s):  
Soil Water ◽  
Volume Change ◽  
Unsaturated Soils ◽  
Water Pressure ◽  
Characteristic Curve ◽  
Matric Suction ◽  
Confining Stress ◽  
Soil Water Characteristic Curve ◽  
Triaxial Cell ◽  
Isotropic Consolidation

Measurement of the soil-water characteristic curve (SWCC) in the laboratory is commonly conducted under zero confining pressure. However, in the field, the soil is under a confining stress. Therefore, it is important to study the effects of the confining stress on SWCC. In addition, the consolidation curve is normally generated under saturated conditions. However, the soil above the water table is usually unsaturated. Hence, it is also necessary to investigate the effects of matric suction on the characteristics of the consolidation curves. This paper presents the SWCCs under different net confining stresses and the isotropic consolidation curves under different matric suctions that describe the volume change characteristics of unsaturated soils with respect to stress state variables, net normal stress, and matric suction. A series of SWCCs was determined for statically compacted silt specimens in a triaxial cell apparatus under different net confining stresses. Isotropic consolidation tests under different matric suctions were also carried out. The results of the SWCC tests show that the air-entry value increased with increasing net confining stress. The yield points (i.e., yield suction, s0) obtained from the SWCC tests also increased with increasing net confining stress. The results of isotropic consolidation tests indicate the strong influence of matric suction on compressibility and stiffness of the compacted silt specimens.Key words: soil-water characteristic curve, isotropic consolidation, pore-water pressure, volume change, NTU mini suction probe, matric suction.

Dual permeability soil water dynamics and water uptake by roots in irrigated potato fields

Biologia ◽  
2007 ◽  
Vol 62 (5) ◽  
Author(s):  
František Doležal ◽  
David Zumr ◽  
Josef Vacek ◽  
Josef Zavadil ◽  
Adriano Battilani ◽  
...  
Keyword(s):  
Soil Water ◽  
Field Experiments ◽  
Preferential Flow ◽  
Water Movement ◽  
Root Zone ◽  
Water Pressure ◽  
Boundary Curve ◽  
Water Dynamics ◽  
Permeability Model ◽  
Soil Matrix

AbstractWater movement and uptake by roots in a drip-irrigated potato field was studied by combining field experiments, outputs of numerical simulations and summary results of an EU project (www.fertorganic.org). Detailed measurements of soil suction and weather conditions in the Bohemo-Moravian highland made it possible to derive improved estimates of some parameters for the dual permeability model S1D_DUAL. A reasonably good agreement between the measured and the estimated soil hydraulic properties was obtained. The measured root zone depths were near to those obtained by inverse simulation with S1D _DUAL and to a boundary curve approximation. The measured and S1D _DUAL-simulated soil water pressure heads were comparable with those achieved by simulations with the Daisy model. During dry spells, the measured pressure heads tended to be higher than the simulated ones. In general, the former oscillated between the simulated values for soil matrix and those for the preferential flow (PF) domain. Irrigation facilitated deep seepage after rain events. We conclude that several parallel soil moisture sensors are needed for adequate irrigation control. The sensors cannot detect the time when the irrigation should be stopped.

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