scholarly journals Implications of a zinc uptake and transport model

2013 ◽  
Vol 8 (5) ◽  
pp. e24167 ◽  
Author(s):  
Juliane Claus ◽  
Andrés Chavarría-Krauser
Keyword(s):  
Transport Model ◽  
Zinc Uptake ◽  
Uptake And Transport

Differential zinc uptake and transport in sorghum varieties suited for different moisture regimes

1981 ◽  
Vol 4 (4) ◽  
pp. 337-351 ◽  
Author(s):  
Saradha Ramani ◽  
Seshadri Kannan ◽  
Arvind S. Nirale
Keyword(s):  
Zinc Uptake ◽  
Moisture Regimes ◽  
Uptake And Transport

scholarly journals Zinc uptake and distribution in ivy (Hedera helix L.) leaves

2021 ◽  
Vol 9 (1) ◽  
pp. 73-82
Author(s):  
Jana Marešová ◽  
Miroslav Horník ◽  
Martin Pipíška ◽  
Jozef Augustín
Keyword(s):  
Leaf Area ◽  
Vascular Plants ◽  
Zinc Uptake ◽  
Mineral Nutrient ◽  
Inhibitory Effects ◽  
Hedera Helix ◽  
Nutrient Media ◽  
Detached Leaves ◽  
Leaf Tissues ◽  
Uptake And Transport

Detached leaves of ivy (Hedera helix L.) were used as a model for the study of zinc uptake and transport in vascular plants. By the uptake via the surface of fully immersed leaves in 25 % Hoagland nutrient media (HM) spiked with 65ZnCl2 (50 μmol/dm3 ZnCl2), concentration in leaves 4.98 μg Zn/g (dry wt.), i. e. 2.6 μg Zn/dm2 leaf area after 7d exposition were obtained. By the uptake via immersed stalks of not immersed (transpiring) leaves concentrations up to 370 μg Zn/g (dry wt.) were obtained. When Zn enters into detached leaves via the surface of immersed leaf blades, zinc is uniformly distributed in leaf blades and leaf stalks. When zinc enters detached leaves via immersed stalks of non-immersed transpiring leaves, only small part of zinc is transported to leaf blades and the prevailing part remains in leaf stalks. Stalks act as a trap, able to prevent other leaf tissues against inhibitory effects of high Zn concentrations. Mineral nutrient salts in solutions mobilize Zn trapped in leaf stalks and facilitate Zn transport by transpiration stream to leaf blades, what means that Zn in stalks is bound in ion-exchageable forms.

Use of SEM, X-ray analysis and TEM to localize Fe3+ reduction in roots

1988 ◽  
Vol 46 ◽  
pp. 392-393 ◽  
Author(s):  
William P. Wergin ◽  
P. F. Bell ◽  
Rufus L. Chaney
Keyword(s):  
Electron Microscopy ◽  
Root Hairs ◽  
Rapid Reduction ◽  
X Ray ◽  
Physical Evidence ◽  
Transmission Electron ◽  
Young Root ◽  
Insoluble Precipitate ◽  
Uptake And Transport ◽  
Scanning Electron

In dicotyledons, Fe3+ must be reduced to Fe2+ before uptake and transport of this essential macronutrient can occur. Ambler et al demonstrated that reduction along the root could be observed by the formation of a stain, Prussian blue (PB), Fe4 [Fe(CN)6]3 n H2O (where n = 14-16). This stain, which is an insoluble precipitate, forms at the reduction site when the nutrient solution contains Fe3+ and ferricyanide. In 1972, Chaney et al proposed a model which suggested that the Fe3+ reduction site occurred outside the cell membrane; however, no physical evidence to support the model was presented at that time. A more recent study using the PB stain indicates that rapid reduction of Fe3+ occurs in a region of the root containing young root hairs. Furthermore the most pronounced activity occurs in plants that are deficient in Fe. To more precisely localize the site of Fe3+ reduction, scanning electron microscopy (SEM), x-ray analysis, and transmission electron microscopy (TEM) were utilized to examine the distribution of the PB precipitate that was induced to form in roots.

A detailed contaminant transport model for facility hazard assessment in urban areas

1999 ◽  
Author(s):  
Bohdan Cybyk ◽  
Jay Boris ◽  
Theodore Young, Jr. ◽  
Charles Lind ◽  
Alexandra Landsberg
Keyword(s):  
Contaminant Transport ◽  
Hazard Assessment ◽  
Urban Areas ◽  
Transport Model

The Carbon:²³⁴Thorium ratios of sinking particles in the California Current Ecosystem 2: Examination of a thorium sorption, desorption, and particle transport model

2019 ◽  
Author(s):  
Michael Stukel ◽  
Thomas Kelly
Keyword(s):  
Organic Carbon ◽  
Water Column ◽  
Particulate Organic Carbon ◽  
Transport Model ◽  
California Current ◽  
In Situ Measurements ◽  
Power Law Distribution ◽  
Sinking Particles ◽  
Organic Carbon Concentration

Thorium-234 (234Th) is a powerful tracer of particle dynamics and the biological pump in the surface ocean; however, variability in carbon:thorium ratios of sinking particles adds substantial uncertainty to estimates of organic carbon export. We coupled a mechanistic thorium sorption and desorption model to a one-dimensional particle sinking model that uses realistic particle settling velocity spectra. The model generates estimates of 238U-234Th disequilibrium, particulate organic carbon concentration, and the C:234Th ratio of sinking particles, which are then compared to in situ measurements from quasi-Lagrangian studies conducted on six cruises in the California Current Ecosystem. Broad patterns observed in in situ measurements, including decreasing C:234Th ratios with depth and a strong correlation between sinking C:234Th and the ratio of vertically-integrated particulate organic carbon (POC) to vertically-integrated total water column 234Th, were accurately recovered by models assuming either a power law distribution of sinking speeds or a double log normal distribution of sinking speeds. Simulations suggested that the observed decrease in C:234Th with depth may be driven by preferential remineralization of carbon by particle-attached microbes. However, an alternate model structure featuring complete consumption and/or disaggregation of particles by mesozooplankton (e.g. no preferential remineralization of carbon) was also able to simulate decreasing C:234Th with depth (although the decrease was weaker), driven by 234Th adsorption onto slowly sinking particles. Model results also suggest that during bloom decays C:234Th ratios of sinking particles should be higher than expected (based on contemporaneous water column POC), because high settling velocities minimize carbon remineralization during sinking.

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