r2018a programming language Search Results


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Output of GA method for optimization of independent variables in As(V) adsorption process on amino-MIL-68(Al). MATLAB <t>R2013a</t> software was used to create this figure ( https://www.mathworks.com/products/matlab.html ).
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An Advective impact along the NEMC path of nutrients rich and cold waters from the Madagascar northern tip to the Tanzanian coast during Sep02 and the climatology (1997–2015). A cross-section (T0) from 39 to 65°E of modelled temperature in °C ( a , d ), Chl-a in mg/m 3 ( b , e ) and DIN in mmol/m 3 ( c,f ) is displayed along the latitude line 10° S as indicated with the black line on panel ( g ). The MLD in m of Sep02 and the climatology are represented by the black solid and dashed lines respectively on panel ( b ). The 2 mmol/m 3 isopleth is highlighted with a thick black line on panels ( c ) and ( f ). ( g ) Trajectories of virtual particles backtracked from the East African coastal zones (marked with light yellow dots) in Sep02 and Sep11, back to their upstream sources in the surface Indian Ocean up to 100 days prior. Colours denote the ‘connectivity timescale’—i.e. the minimum amount of time, in days, required for waters from a given area to reach any of the end points on the East African coast. Note that reds/oranges paths are plotted on top of blues/purples to highlight the most rapid advective pathways in both cases. Maps on panel (g) was created by the authors using MATLAB software <t>vR2013a</t> (see <t>https://uk.mathworks.com/videos/r2013a-release-highlights-75269.html</t> and https://uk.mathworks.com/products/matlab.html ).
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MathWorks Inc software version r2017a
An Advective impact along the NEMC path of nutrients rich and cold waters from the Madagascar northern tip to the Tanzanian coast during Sep02 and the climatology (1997–2015). A cross-section (T0) from 39 to 65°E of modelled temperature in °C ( a , d ), Chl-a in mg/m 3 ( b , e ) and DIN in mmol/m 3 ( c,f ) is displayed along the latitude line 10° S as indicated with the black line on panel ( g ). The MLD in m of Sep02 and the climatology are represented by the black solid and dashed lines respectively on panel ( b ). The 2 mmol/m 3 isopleth is highlighted with a thick black line on panels ( c ) and ( f ). ( g ) Trajectories of virtual particles backtracked from the East African coastal zones (marked with light yellow dots) in Sep02 and Sep11, back to their upstream sources in the surface Indian Ocean up to 100 days prior. Colours denote the ‘connectivity timescale’—i.e. the minimum amount of time, in days, required for waters from a given area to reach any of the end points on the East African coast. Note that reds/oranges paths are plotted on top of blues/purples to highlight the most rapid advective pathways in both cases. Maps on panel (g) was created by the authors using MATLAB software <t>vR2013a</t> (see <t>https://uk.mathworks.com/videos/r2013a-release-highlights-75269.html</t> and https://uk.mathworks.com/products/matlab.html ).
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Image Search Results


Output of GA method for optimization of independent variables in As(V) adsorption process on amino-MIL-68(Al). MATLAB R2013a software was used to create this figure ( https://www.mathworks.com/products/matlab.html ).

Journal: Scientific Reports

Article Title: Facile fabrication of amino-functionalized MIL-68(Al) metal–organic framework for effective adsorption of arsenate (As(V))

doi: 10.1038/s41598-022-16038-0

Figure Lengend Snippet: Output of GA method for optimization of independent variables in As(V) adsorption process on amino-MIL-68(Al). MATLAB R2013a software was used to create this figure ( https://www.mathworks.com/products/matlab.html ).

Article Snippet: Design-Expert v13 ( https://www.statease.com/docs/v13/ ) and MATLAB R2013a ( https://www.mathworks.com/products/matlab.html ) software were used to perform CCD and GA in this study, respectively.

Techniques: Adsorption, Software

An Advective impact along the NEMC path of nutrients rich and cold waters from the Madagascar northern tip to the Tanzanian coast during Sep02 and the climatology (1997–2015). A cross-section (T0) from 39 to 65°E of modelled temperature in °C ( a , d ), Chl-a in mg/m 3 ( b , e ) and DIN in mmol/m 3 ( c,f ) is displayed along the latitude line 10° S as indicated with the black line on panel ( g ). The MLD in m of Sep02 and the climatology are represented by the black solid and dashed lines respectively on panel ( b ). The 2 mmol/m 3 isopleth is highlighted with a thick black line on panels ( c ) and ( f ). ( g ) Trajectories of virtual particles backtracked from the East African coastal zones (marked with light yellow dots) in Sep02 and Sep11, back to their upstream sources in the surface Indian Ocean up to 100 days prior. Colours denote the ‘connectivity timescale’—i.e. the minimum amount of time, in days, required for waters from a given area to reach any of the end points on the East African coast. Note that reds/oranges paths are plotted on top of blues/purples to highlight the most rapid advective pathways in both cases. Maps on panel (g) was created by the authors using MATLAB software vR2013a (see https://uk.mathworks.com/videos/r2013a-release-highlights-75269.html and https://uk.mathworks.com/products/matlab.html ).

Journal: Scientific Reports

Article Title: Interannual monsoon wind variability as a key driver of East African small pelagic fisheries

doi: 10.1038/s41598-020-70275-9

Figure Lengend Snippet: An Advective impact along the NEMC path of nutrients rich and cold waters from the Madagascar northern tip to the Tanzanian coast during Sep02 and the climatology (1997–2015). A cross-section (T0) from 39 to 65°E of modelled temperature in °C ( a , d ), Chl-a in mg/m 3 ( b , e ) and DIN in mmol/m 3 ( c,f ) is displayed along the latitude line 10° S as indicated with the black line on panel ( g ). The MLD in m of Sep02 and the climatology are represented by the black solid and dashed lines respectively on panel ( b ). The 2 mmol/m 3 isopleth is highlighted with a thick black line on panels ( c ) and ( f ). ( g ) Trajectories of virtual particles backtracked from the East African coastal zones (marked with light yellow dots) in Sep02 and Sep11, back to their upstream sources in the surface Indian Ocean up to 100 days prior. Colours denote the ‘connectivity timescale’—i.e. the minimum amount of time, in days, required for waters from a given area to reach any of the end points on the East African coast. Note that reds/oranges paths are plotted on top of blues/purples to highlight the most rapid advective pathways in both cases. Maps on panel (g) was created by the authors using MATLAB software vR2013a (see https://uk.mathworks.com/videos/r2013a-release-highlights-75269.html and https://uk.mathworks.com/products/matlab.html ).

Article Snippet: Maps on panel (g) was created by the authors using MATLAB software vR2013a (see https://uk.mathworks.com/videos/r2013a-release-highlights-75269.html and https://uk.mathworks.com/products/matlab.html ).

Techniques: Northern Blot, Software