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Homework 1 - Myweb @ CW Post

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---! Next, list bonds e-k, in order from most covalent to most ionic. Notice that these<br />

are the major elements bonding with oxygen as in silicate minerals.<br />

coordination polyhedra & ionic substitution<br />

6)! Using Figures 2.7-2.8 and Table 2.5 in the textbook, determine the coordination<br />

number and type for the following ions.<br />

! Note: the values listed in Figs 2.7 & 2.8 are for general use but not necessarily the<br />

specific radius in a given compound. The radius listed for Si +4 in b) below is specific<br />

for its bonding with oxygen and differs from the general radius given in Fig 2.7.<br />

! a) Na + relative to Cl - in halite (Cl- ionic radius: 1.72 Å)<br />

! b) Si +4 relative to O -2 in silicates (Si +4 ionic radius here is ~0.34 Å; Faure, 1998)<br />

! c) Al +3 relative to O -2 in silicates<br />

! d) Na + relative to O -2 in silicates<br />

! e) Fe +2 relative to O -2 in silicates<br />

7)! Atomic and ionic radii vary with valence state but also with the type and number of<br />

surrounding ions (for example, see Table 2.6). Determine the coordination number<br />

and type for carbon in carbon dioxide and in carbonate ions:<br />

! a) C +4 relative to O -2 in CO2 (radius of C +4 in CO2: 0.16 Å)<br />

! b) C +4 relative to O -2 in CO3 -2 (radius of C +4 in CO3 -2 : 0.29 Å)<br />

!<br />

8)! Determine whether the following substitutions will occur. Show why or why not, and<br />

if coupled substitution is required. Use Figure 2.7 and Table 2.6 for cation radii (note<br />

correct coordination in Table 2.6).<br />

a) will Mg +2 substitute for Fe +2 bonded to O -2 in silicates<br />

! b) will Ca +2 substitute for Na + bonded to O -2 in silicates<br />

! c) will K + substitute for Na + bonded to O -2 in silicates

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