Modelling water and salt transport in a soil-water-plant system under different groundwater tables

2008 ◽  
Vol 22 (4) ◽  
pp. 265-273 ◽  
Author(s):  
Ligang Xu ◽  
Jingsong Yang ◽  
Qi Zhang ◽  
Hailin Niu
2013 ◽  
Vol 374 (1-2) ◽  
pp. 993-1004 ◽  
Author(s):  
Jinghua Fan ◽  
Zhenli He ◽  
Lena Q. Ma ◽  
Yuangen Yang ◽  
Peter J. Stoffella

2014 ◽  
Vol 22 (6) ◽  
pp. 4513-4526 ◽  
Author(s):  
Stefanie Kloss ◽  
Franz Zehetner ◽  
Jannis Buecker ◽  
Eva Oburger ◽  
Walter W. Wenzel ◽  
...  

2014 ◽  
Vol 497-498 ◽  
pp. 319-331 ◽  
Author(s):  
Rosa Cidu ◽  
Riccardo Biddau ◽  
Elisabetta Dore ◽  
Andrea Vacca ◽  
Luigi Marini

2021 ◽  
Author(s):  
Abdurrahman Lermi ◽  
Emmanuel Daanoba Sunkari

Abstract Globally, potentially toxic elements (PTEs) are regarded as an important group of pollutants for the wider environment because of their intrinsic toxicity and probable accumulation in the soil-water-plant system. In this regard, this study assessed the pollution levels and probable human health risks of PTEs in the soil-water-plant system in the Bolkar mining district of the Niğde Province in south-central Turkey. Pollution assessment using contamination factor, enrichment factor, index of geoaccumulation, and soil pollution index reveals moderate to extremely high pollution of PTEs in the soil, exposing the soils to extreme toxicity levels. The areas that fall under the toxic to extremely toxic categories are in proximity to the ore slags and agricultural lands towards the central and southern domains of the study area. The water hazard index (WHI) values indicate that 100% of the samples collected in both winter and fall seasons are of extreme toxicity (WHI > 15). Arsenic is the dominant contaminant among the PTEs in the soil and water samples. The bioconcentration factor values of the PTEs in most of the fruit plants are > 1, indicating very high levels of element transfer from the soil and water to the plants. The probabilistic human health risk assessment involved exposure to arsenic in groundwater (a major pathway to humans) since it is the only carcinogenic element in this study. The estimated daily intake of arsenic-contaminated water exceeds the safe limit of 5 × 10− 8 mg/kg/day. About 33.3% and 55.6% of the groundwater samples have higher hazard quotient and carcinogenic risk values of arsenic in the winter and fall seasons, respectively. This implies that the people are more exposed to the carcinogenic effects of drinking arsenic-contaminated water.


1990 ◽  
pp. 28-41 ◽  
Author(s):  
Jack Keller ◽  
Ron D. Bliesner
Keyword(s):  

2020 ◽  
pp. 207-210
Author(s):  
M.K. Trivedi ◽  
K.S. Hariprasad ◽  
A. Gairola ◽  
D. Kashyap

2019 ◽  
Vol 28 (3) ◽  
pp. 1637-1650
Author(s):  
Weihong Dong ◽  
Chuanlei Wen ◽  
Pan Zhang ◽  
Xiaosi Su ◽  
Fengtian Yang

1987 ◽  
Vol 35 (3) ◽  
pp. 395-406
Author(s):  
C. Dirksen

With closed, high-frequency irrigation systems, the water supply can be tailored to the instant needs of plants. To be able to do this optimally, it is necessary to understand how plants interact with their environment. To study water uptake under a variety of non-uniform conditions in the root zone, lucerne was grown in laboratory soil columns with automated gamma ray attenuation, tensiometer and salinity sensor equipment to measure soil water contents, pressure potentials and osmotic potentials, respectively. The columns were irrigated with water of different salinity at various frequencies and leaching fractions. This paper presents results obtained in a column irrigated daily with water of conductivity 0.33 S/m (h0 = -13.2 m) at a target leaching fraction of 0.08. This includes the drying and wetting patterns under daily irrigations in deficit and excess of evapotranspiration, respectively. After 230 days the salination of the column had still not reached a steady state. Salinity increased rapidly with depth and root water uptake was shallow for the deep-rooting lucerne. Water and salt transport under daily irrigation cannot be described without taking hysteresis of soil water retention into account. The data presented are suitable for testing various water uptake models, once numerical water and salt transport models of the required complexity are operational. (Abstract retrieved from CAB Abstracts by CABI’s permission)


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