Name:_______________________________________________________ Section:
1. Calculate Im to the nearest whole number for the last ten stations in Table 14.2 using equation 1.
2. Locate these same ten stations at “x”s on the maps of ecoregions (Figure 14.2) and soil orders (Figure 14.3). Record the letter codes representing the vegetation and soil at each station (Table 14.1) to complete Table 14.2. For mixed vegetation, use the first type listed in the ecoregions map (Figure 14.2) key.
TABLE 14.1 Vegetation and Soil Codes
|
Use: |
For: |
Use: |
For: |
|
R |
Tropical
Rainforest |
s |
Spodosols ("ash-colored") |
|
B |
Broadleaf
temperate forest |
a |
Alfisols ("aluminum & iron stains") |
|
N |
Needleleaf forest |
m |
Mollisols ("soft & friable") |
|
S |
Savanna |
u |
Ultisols ("old") |
|
G |
Grassland |
o |
Oxisols ("oxidized") |
|
D |
Desert |
v |
Vertisols ("turning over") |
|
T |
Tundra |
h |
Histosols ("tissue-like") |
|
|
|
d |
Aridisols ("dry") |
|
|
|
e |
Entisols ("recent") |
|
|
|
i |
Inceptisols ("beginning") |
|
|
|
v |
Andisols (“volcanic andesite”) |
|
|
|
g |
Gelisols (“gelifluction
& frost heaving”) |
TABLE 14.2 Station Data
|
Station |
Location |
P |
Im |
Vegetation |
Soil |
||
|
1 |
|
35S/059W |
1005 |
759 |
+32 |
G |
m |
|
2 |
|
02N/049W |
2833 |
1537 |
+84 |
R |
i |
|
3 |
|
26N/100W |
606 |
1100 |
-45 |
D |
d |
|
4 |
|
36N/098W |
818 |
776 |
+5 |
G |
m |
|
5 |
|
32N/111W |
295 |
1024 |
-71 |
D |
d |
|
6 |
|
29N/111W |
363 |
1731 |
-79 |
D |
d |
|
7 |
|
40N/116W |
134 |
576 |
-77 |
D |
d |
|
8 |
|
40N/106W |
958 |
285 |
+236 |
T |
i |
|
9 |
|
48N/104W |
352 |
487 |
-28 |
G |
m |
|
10 |
|
44N/093W |
701 |
532 |
+32 |
B |
a |
|
11 |
|
65N/148W |
268 |
357 |
-25 |
N |
g |
|
12 |
Barrow, |
71N/157W |
112 |
222 |
-49 |
T |
g |
|
13 |
|
61N/116W |
326 |
336 |
-3 |
N |
s |
|
14 |
|
54N/057W |
966 |
336 |
+187 |
T |
e |
|
15 |
|
50N/093W |
671 |
424 |
+58 |
B |
s |
|
16 |
|
51N/106W |
368 |
453 |
-19 |
G |
m |
|
17 |
|
54N/114W |
454 |
426 |
+7 |
N |
a |
|
18 |
|
42N/083W |
831 |
549 |
+51 |
B |
a |
|
19 |
|
59N/094W |
402 |
268 |
+50 |
T |
h |
|
20 |
|
64N/016W |
818 |
410 |
+100 |
T |
g |
|
21 |
|
52N/009W |
1081 |
563 |
+92 |
B |
a |
|
22 |
|
61N/022E |
632 |
419 |
+51 |
B |
s |
|
23 |
|
69N/033E |
412 |
321 |
+28 |
N |
s |
|
24 |
|
52N/105E |
418 |
378 |
+11 |
N |
i |
|
25 |
|
44N/881E |
254 |
558 |
-54 |
D |
d |
|
26 |
|
11N/107E |
1934 |
1712 |
+13 |
S |
u |
|
27 |
|
23N/089E |
1633 |
1781 |
-8 |
S |
u |
|
28 |
|
36N/052E |
239 |
848 |
-72 |
D |
d |
|
29 |
|
01N/104E |
2272 |
1687 |
+35 |
R |
o |
|
30 |
|
30N/031E |
28 |
1035 |
-97 |
D |
d |
|
31 |
|
4N/010E |
4000 |
1380 |
+165 |
R |
o |
|
32 |
|
23S/017E |
367 |
865 |
-58 |
D |
d |
|
33 |
|
34S/019E |
611 |
753 |
-19 |
S |
a |
|
34 |
|
04S/040E |
1144 |
1587 |
-28 |
S |
a |
|
35 |
|
00S/033E |
1535 |
971 |
+58 |
S |
u |
|
36 |
|
04N/115E |
2553 |
1610 |
+59 |
R |
o |
|
37 |
|
26S/033E |
767 |
1078 |
-29 |
S |
d |
|
38 |
|
01N/025E |
1858 |
1273 |
+46 |
R |
o |
|
39 |
|
18S/031E |
827 |
813 |
+2 |
S |
a |
|
40 |
|
09S/013E |
369 |
1207 |
-69 |
S |
d |
|
41 |
|
45N/090W |
725 |
504 |
+44 |
B |
a |
|
42 |
|
40N/105W |
327 |
544 |
-40 |
G |
d |
|
43 |
|
39N/090W |
939 |
698 |
35 |
G |
a |
|
44 |
|
39N/077W |
990 |
725 |
37 |
B |
u |
|
45 |
|
34N/084W |
1237 |
783 |
58 |
B |
u |
|
46 |
|
03S/060W |
2081 |
1611 |
29 |
R |
i |
|
47 |
|
04S/073W |
2878 |
1519 |
89 |
R |
o |
|
48 |
|
04S/071W |
2811 |
884 |
218 |
R |
o |
|
49 |
|
20S/070W |
2 |
793 |
-100 |
D |
d |
|
50 |
|
16S/048W |
1555 |
920 |
-13 |
G |
a |
Name:________________________________________________ Section:________________
1. Figures 14.4 (vegetation graph) and 14.5 (soils graph) were created using the data in Table 14.2. Plot the last ten stations on each graph.
2. Encircle clusters of the same letters on Figures 14.4 (vegetation graph) and 14.5 (soils graph) (skip this for entisols and inceptisols), after the grassland and mollisol examples. The enclosure lines may overlap. Then shade the separate clusters in different colors. It would be a good idea to do this in pencil!
3. Compare Figures 14.4 (vegetation graph) and 14.5 (soils graph) with Figure 14.1. While you will have some difference in appearance, there should also be some degree of correspondence between your patterns and those of Figure 14.1.
a. Which of your
vegetation and soils zones seem to fall most consistently into their correct
places according to Figure 14.1? R, D, G for biomes;
o, a, d, m, and s for soils
b. Which of your
vegetation and soils zones seem to fall most inconsistently into their correct places according to Figure 14.1? B, N for vegetation; e, I, a for soils
4. List all vegetation and the soil orders on Figures 14.4 (vegetation graph) and 14.5 (soils graph) that correspond most closely with the following climates:
|
Climate |
Vegetation
Letter Code(s) |
Soil Letter
Code(s) |
|
Tropical (Köppen A) |
R, S |
o, u |
|
Subtropical (Köppen C) |
S, B |
a, u |
|
Continental (Köppen D) |
B, N |
a, s |
|
Frozen (Köppen E) |
T, N |
i, h, s |
|
Arid (Köppen B) |
D, G, S |
a, d, m |
Figure 14.4 Vegetation Graph

Figure 14.5 Soil Orders Graph

Name: Section:
1. What soil(s) and climate(s) best correspond to each vegetation? Use Table 14.2, Figure 14.4 (vegetation graph), and Figure 14.5 (soils graph).
|
Vegetation |
Soil Code |
Climate |
|
Tropical Rainforest (R) |
o, u |
A |
|
Broadleaf Temperate |
a, d |
B, C, D |
|
|
s |
D |
|
Savanna (S) |
a, d, u |
A, B |
|
Grassland (G) |
d, m |
B, C |
|
Desert (D) |
d |
B |
|
Tundra (T) |
e, h, i |
E |
2. Draw a line that separates forest from non-forest vegetation on the vegetation graph (Figure 14.4). This line shows the environmental limits to forest vegetation, something we can actually see on the landscape – the treeline: a boundary beyond which trees do not grow.
3. a. What would be a good approximate cutoff Im value separating savanna from desert?
-50
b. What would be a good approximate cutoff PE value separating tundra from forest?
300 mm
c. Describe the temperature and moisture conditions necessary for forest to exist.
Almost any
temperature (PE), but usually moist (Im>0) unless
alternative sources of water are available (e.g., some climatic dry Broadleaf
are riverbank forests)
Some soil orders (e.g., mollisols) cluster pretty much into their own exclusive areas on Figure 14.5. Others (e.g., oxisols and ultisols) seem to share part of their graph zones. Some orders, inceptisols and entisols, do not seem to cluster very much at all, but appear almost randomly on the graph. Consider the meaning of the axis variables in Figures 14.4 and 14.5 as you try to explain soil occurrence tendencies below.
4. Name another soil order that clusters into its own graph zone. What vegetation (on Figure 14.4) does this soil consistently coincide with, and what climatic conditions evidently exist where this soil and vegetation develops?
Soil Vegetation Climate
|
s |
N |
D
(cold, but humid enough for forest) |
5. a. Name two soil orders that overlap, and thus share a graph zone. a & m, or o & u
b. What climatic conditions (hot/cold, wet, dry) does their overlap represent?
moderate heat
and moisture, or variably humid but warm
c. What non-climatic factors might cause these two different
soils to form under similar climatic conditions?
Soil/bedrock
permeability, sea level changes, bedrock composition, etc.
6. What non-climatic situations could produce entisols and inceptisols across a variety of different climates, as these soil orders appear within Figure 14.5?
geologic
disturbances (volcanoes, isostacy, etc.), hydrologic
alteration
7. Some of the vegetation (Figure 14.4) may overlap or contain outlyers, implying that several types of vegetation coexist together. Give one possible explanation for joint (instead of exclusive) occupation of the same graph zone by unlike vegetation.
8. Using your graphs and comparing the PE and Im values in Table 14.1, what vegetation and soil (use our letter codes) do you predict for the following hypothetical places? Then indicate locations where each of these ecosystems might typically occur.
|
PE |
Im |
Vegetation |
Soil |
Likely |
|
375 |
-5 |
N |
s |
central
|
|
610 |
-31 |
G |
m, a,
d |
western
|
|
733 |
+27 |
B, G,
S |
a, m,
u |
southern
|
|
1225 |
-95 |
B, D |
d |
|
|
1475 |
+105 |
R |
o, u |
|
[NcH1] Computations of potential evapotranspiration (PE) for this exercise follow C. W. Thornthwaite’s method, using PE = 1.6(10(T/I)a
Where T = monthly temperature (°C)
I = annual heat index; sum of 12 monthly heat index
values (i) from i = (t/5)1.514
a = .000000675 I3 - .0000771 I2 + .0179 I + .49
See also Mather, John. Climatology; Fundamentals and Applications. New York: McGraw-Hill, 1974. p. 66-67