Discussion of “ Soil Surface Evaporation and Water Table Depths ” by Sun F. Shih (December, 1983)

1984 ◽  
Vol 110 (4) ◽  
pp. 415-415
Author(s):  
M. N. Viswanathan
Keyword(s):  
Water Table ◽  
Soil Surface ◽  
Surface Evaporation

Dissolved Phosphorus Losses in Tile Drainage under Subirrigation

2006 ◽  
Vol 41 (1) ◽  
pp. 63-71 ◽  
Author(s):  
Nicolas Stämpfli ◽  
Chandra A. Madramootoo
Keyword(s):  
Water Table ◽  
Residual Effect ◽  
Surface Water Quality ◽  
Soil Surface ◽  
Quality Standard ◽  
Tile Drainage ◽  
Agricultural Field ◽  
Shallow Water Table ◽  
Dissolved Phosphorus ◽  
Water Table Control

Abstract Recent studies have shown subirrigation (SI) to be effective in reducing nitrate losses from agricultural tile drainage systems. A field study was conducted from 2001 to 2002 in southwestern Québec to evaluate the effect of SI on total dissolved phosphorus (TDP) losses in tile drainage. In an agricultural field with drains installed at a 1-m depth, a SI system with a design water table depth (WTD) of 0.6 m below the soil surface was compared with conventional free drainage (FD). Subirrigation increased drainage outflow volumes in the autumn, when drains were opened and water table control was interrupted for the winter in the SI plots. Outflows were otherwise similar for both treatments. Throughout the study, the TDP concentrations in tile drainage were significantly higher with SI than with FD for seven out of 17 of the sampling dates for which data could be analyzed statistically, and they were never found to be lower for plots under SI than for plots under FD. Of the seven dates for which the increase was significant, six fell in the period during which water table control was not implemented (27 September 2001 to 24 June 2002). Hence, it appears that SI tended to increase TDP concentrations compared with FD, and that it also had a residual effect between growing seasons. Almost one-third of all samples from the plots under SI exceeded Québec's surface water quality standard (0.03 mg TDP L-1), whereas concentrations in plots under FD were all below the standard. Possible causes of the increase in TDP concentrations in tile drainage with SI are high TDP concentrations found in the well water used for SI and a higher P solubility caused by the shallow water table.

scholarly journals Mapping the Pollution Plume Using the Self-Potential Geophysical Method: Case of Oum Azza Landfill, Rabat, Morocco

Water ◽  
2021 ◽  
Vol 13 (7) ◽  
pp. 961
Author(s):  
Meryem Touzani ◽  
Ismail Mohsine ◽  
Jamila Ouardi ◽  
Ilias Kacimi ◽  
Moad Morarech ◽  
...  
Keyword(s):  
Electrical Conductivity ◽  
Water Table ◽  
Soil Surface ◽  
The Self ◽  
Drainage Network ◽  
Geophysical Method ◽  
Direct Measurements ◽  
Sandy Material ◽  
The City ◽  
Self Potential

The main landfill in the city of Rabat (Morocco) is based on sandy material containing the shallow Mio-Pliocene aquifer. The presence of a pollution plume is likely, but its extent is not known. Measurements of spontaneous potential (SP) from the soil surface were cross-referenced with direct measurements of the water table and leachates (pH, redox potential, electrical conductivity) according to the available accesses, as well as with an analysis of the landscape and the water table flows. With a few precautions during data acquisition on this resistive terrain, the results made it possible to separate the electrokinetic (~30%) and electrochemical (~70%) components responsible for the range of potentials observed (70 mV). The plume is detected in the hydrogeological downstream of the discharge, but is captured by the natural drainage network and does not extend further under the hills.

Response of winter wheat to prolonged waterlogging under outdoor conditions

1981 ◽  
Vol 97 (3) ◽  
pp. 557-568 ◽  
Author(s):  
R. K. Belford
Keyword(s):  
Winter Wheat ◽  
Water Table ◽  
Stem Elongation ◽  
Soil Surface ◽  
Root Production ◽  
Or Efficiency ◽  
Plant Nitrogen ◽  
Stages Of Growth ◽  
Nodal Root ◽  
Waterlogging Treatment

SUMMARYThe response of winter wheat cv. Maris Huntsman to waterlogging was studied in two experiments in soil columns outdoors. Winter waterlogging treatments increased nodal root production and the proportion of aerenchyma within roots, but caused chlorosis and premature senescence of leaves, and decreased tillering. For all treatments, grain losses were much less than expected from the extent of tiller loss in winter; losses after single waterlogging events ranged from 2% (after 47 days with the water-table at 5 cm) to 16% (after 80 days with the water-table at the soil surface). Yield losses after three waterloggings at the seedling, tillering and stem elongation stages of growth were additive, and totalled 19%. In many treatments, grain loss was associated with lighter individual grain weights, suggesting that the size of the root system or efficiency of water and nutrient uptake by roots at the later stages of growth may have been less after earlier waterlogging. The importance of nitrogen fertilizer in maintaining a satisfactory plant nitrogen status was shown when nitrogen was with held before a 3-week waterlogging treatment during stem elongation; tiller and floret survival was subsequently greatly restricted and grain yields decreased 22% below those of plants waterlogged at the same stage of growth but supplied with nitrogen.

scholarly journals Influence of Water Table Fluctuation on Natural Source Zone Depletion in Hydrocarbon Contaminated Subsurface Environments

2020 ◽  
Author(s):  
Reem Ismail ◽  
Saeid Shafieiyoun ◽  
Riyadh Al Raoush ◽  
Fereidoun Rezanezhad
Keyword(s):  
Water Table ◽  
Contaminated Soil ◽  
Soil Surface ◽  
Source Zone ◽  
Water Table Fluctuation ◽  
Mass Removal ◽  
Water Table Fluctuations ◽  
Water Conditions ◽  
Static Water ◽  
Influence Of Water

Most of the prediction theories regarding dissolution of organic contaminants in the subsurface systems have been proposed based on the static water conditions; and the influence of water fluctuations on mass removal requires further investigations. In this study, it was intended to investigate the effects of water table fluctuations on biogeochemical properties of the contaminated soil at the smear zone between the vadose zone and the groundwater table. An automated 60 cm soil column system was developed and connected to a hydrostatic equilibrium reservoir to impose the water regime by using a multi-channel pump. Four homogenized hydrocarbon contaminated soil columns were constructed and two of them were fully saturated and remained under static water conditions while another two columns were operated under water table fluctuations between the soil surface and 40 cm below it. The experiments were run for 150 days and relevant geochemical indicators as well as dissolved phase concentrations were analyzed at 30 and 50 cm below the soil surface in all columns. The results indicated significant difference in terms of biodegradation effectiveness between the smear zones exposed to static and water table fluctuation conditions. This presentation will provide an overview of the experimental approach, mass removal efficiency, and key findings.

scholarly journals PRODUÇÃO DE MATÉRIA SECA E EVAPOTRANSPIRAÇÃO REAL DA AVEIA PRETA (Avena strigosa S.) EM SEIS NÍVEIS FREÁTICOS

Irriga ◽  
2001 ◽  
Vol 6 (2) ◽  
pp. 62-68
Author(s):  
Marcos Henrique Sias Silveira ◽  
Antonio Evaldo Klar
Keyword(s):  
Water Level ◽  
Water Table ◽  
Dry Matter ◽  
Soil Surface ◽  
Dry Matter Production ◽  
Progressive Decrease ◽  
Surface Level ◽  
Water Table Level ◽  
Avena Strigosa ◽  
Matter Production

PRODUÇÃO DE MATÉRIA SECA E EVAPOTRANSPIRAÇÃO REAL DA AVEIA PRETA (Avena strigosa S.) EM SEIS NÍVEIS FREÁTICOS  Marcos Henrique Dias SilveiraAntonio Evaldo KlarDepartamento de Engenharia Rural –  Faculdade de Ciências Agronômicas – UnespBotucatu – SP  Cep: 18603-970Fone: (0xx14) 6802-7165 – [email protected]  1  RESUMO Para avaliar os efeitos de seis diferentes níveis freáticos na produção de matéria seca e na evapotranspiração real ou de cultura da aveia preta (Avena strigosa S.) foi conduzido um experimento em casa de vegetação, no Departamento de Engenharia Rural da FCA - Campus de Botucatu - UNESP.  Foram semeadas 21 sementes de aveia por vaso, construído de anéis de PVC, com diâmetro nominal de 0,15m x 0,07m de comprimento e alturas totais variando entre 0,21m e 0,91m, de modo a simular os efeitos de níveis freáticos de 0,17m, 0,31m, 0,45m, 0,59m, 0,73m e 0,87m de profundidade.  Após a emergência das plântulas procedeu-se ao desbaste,  deixando-se 8 plantas por vaso, com 06 repetições (seis vasos) para cada nível freático, totalizando 36 vasos em delineamento inteiramente casualizado.  Dados de evapotranspiração real foram coletados diariamente e computados semanalmente.  As plantas foram cortadas rente ao solo ao final da 12.ª semana após a semeadura.  Foram avaliadas as produções de matéria seca da parte aérea e do sistema radicular em cada nível freático.  Os resultados mostraram maior produção de matéria seca para o nível freático mais superficial (0,17m), com queda gradativa à medida que o nível freático se aprofundava. A evapotranspiração da cultura  mostrou a mesma tendência, variando entre 591,6 mm  no tratamento com nível freático a 0,17m de profundidade e 215,4 mm para o de 0,87m de profundidade. UNITERMOS: evapotranspiração, níveis freáticos, aveia preta.  SILVEIRA, M. H. D., KLAR, A. E.  DRY MATTER PRODUCTION AND EVAPOTRANSPIRATION OF OAT         ( Avena strigosa S.) UNDER  SEVERAL TABLE LEVELS.  2  ABSTRACT The aim of this study was to evaluate the influence of six different water table levels on yield and evapotranspiration of oat (Avena strigosa S.) .  21 seeds were sowed  per  pot, which was built with PVC rings (0.15m nominal diameter x 0.07m lenght).  6 water table levels were used: 0.17; 0.31; 0.45; 0.59; 0.73; and 0.87 m measured from the soil surface replicated  6  times.  The completely randomised design was used.  After seedling emergency, 8 plants were maintained  per  pot.  The evapotranspiration were daily measured from reservoirs connected to the pots.  The plants were cut at the soil surface level after 12 weeks from the sowing.The results showed greater dry matter production at the most superficial water table level with progressive decrease with water level distance from the soil surface.  The  evapotranspiration  showed  the  same tendency: the higher values occurred on the 0.17m water table (591.6 mm) until 0.87m water table (215.4 mm). KEYWORDS:  water table, evapotranspiration, Avena strigosa S.

scholarly journals Evaporation and Soil Surface Resistance of the Water Storage Pit Irrigation Trees in the Loess Plateau

Water ◽  
2019 ◽  
Vol 11 (4) ◽  
pp. 648 ◽  
Author(s):  
Wei Meng ◽  
Xihuan Sun ◽  
Juanjuan Ma ◽  
Xianghong Guo ◽  
Lijian Zheng
Keyword(s):  
Surface Resistance ◽  
Water Storage ◽  
Growth Period ◽  
Soil Surface ◽  
Soil Evaporation ◽  
Utilization Efficiency ◽  
The Loess Plateau ◽  
Surface Evaporation ◽  
Orchard Soil ◽  
Quantitative Calculations

As an important step for formulating a water-saving agricultural strategy, it is essential to make quantitative calculations for orchard soil evaporation and confirm its inner mechanism, so as to reduce ineffective water consumption and improve the utilization efficiency of water resources. To reveal the effect of water storage pits under water storage pit irrigation conditions in orchard soil evaporation, micro-lysimeters were used to measure the soil evaporation in two different forms (soil surface evaporation and pit wall evaporation) under diverse irrigation systems using water storage pit irrigation in the apple growth period of 2018. To calculate the orchard soil evaporation of water storage pit irrigation, the pit irrigation coefficient was introduced and a model was constructed. To illustrate the inner mechanism of orchard soil evaporation, the soil surface resistance under water storage pit irrigation conditions was analyzed and calculated quantitatively. The results show that: (1) introducing the pit irrigation coefficient can boost the calculation precision of the orchard soil evaporation under water storage pit irrigation conditions; (2) when applying the soil evaporation of the water storage pit irrigation model for calculation of the orchard soil evaporation, R 2 can reach 0.92; and (3) the mechanisms of the two orchard soil evaporation forms under water storage pit irrigation are very different. When soil surface evaporation and pit wall evaporation were calculated by the soil surface resistance of water storage pit irrigation model, R 2 values were 0.95 and 0.96, respectively.

Dynamics of Soil Surface Bulk Density: Role of Water Table Elevation and Rainfall Duration

2008 ◽  
Vol 72 (2) ◽  
pp. 412-423 ◽  
Author(s):  
B. Augeard ◽  
L. M. Bresson ◽  
S. Assouline ◽  
C. Kao ◽  
M. Vauclin
Keyword(s):  
Bulk Density ◽  
Water Table ◽  
Soil Surface ◽  
Rainfall Duration

Effect of Soil Surface Submergence and a Water Table on Vegetative Growth and Nutrient Uptake of Corn

1992 ◽  
Vol 35 (4) ◽  
pp. 1173-1177 ◽  
Author(s):  
N. Ahmad ◽  
R. S. Kanwar ◽  
T. C. Kaspar ◽  
T. B. Bailey
Keyword(s):  
Nutrient Uptake ◽  
Water Table ◽  
Vegetative Growth ◽  
Soil Surface
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