O. Hamel
Directeur du Department des Recherches Forestières et Hydrobiologiques de l'Institute Sénégalais de Recherches Agricoles. Center National de Recherches Forestièeres BE 2312, Dakar, Senegal.
2. On-site behaviour of species
The Senegalese Forestry Research Institute has planted a collection of acacias previously unknown to Africa on a number of stations characteristic of the Sudanian and Sahel area of Senegal. A crop of Australian seeds was used, procured in 1973 by the Centre Technique Forestier Tropical in cooperation with the Australian Forestry Timber Board. Most of the seed introduced came from the Northern and West Australian territories, the climatic conditions with regard to the Australian seeds and the Senegalese sites chosen for introduction are briefly described in Annex I to this paper.
The species introduced were as follows:
a) from Australia: A. bivenosa, A. coriacea, A. dunnii, A. farnesiana, A. holosericea, A. inaequilatera, A. aff. Linarioides, A. monticola, A. mountfordae, A. plectocarna, A. pyrifolia, A. sclerosperma, A. spathulata, A. tenuisissima, A. tetragonophylla, A. tumida;b) from the Maghreb: A. cyanophylla, A. Cyclops, A. salicina.
Raising these Acacia spp. in the nursery poses on particular problems. Direct pot sowing (2 seeds per pot) gives very good results, with an excellent germination rate.
Depending on the site it may be necessary to use shading during the period before the phyllodes appear, i.e. for about a fortnight, but usually the resistance of these species means that this precaution is not necessary. The nursery stage lasts about 3 months. The only precautions necessary are on the health side, against cutworm and nematodes. The latter precaution is important since, like all acacias, these species are sensitive to nematodes, and the risk of infestation on virgin land resulting from the introduction of these species is considerable. Furthermore, nematodes prevent the formulation of rhizobia nodules and thus inhibit their nitrogen-fixative capacity. Nematicide treatment also accelerates the development of the plants in the nursery.
Ongoing research at the ORSTOM Soil Microbiology Laboratory in Dakar in collaboration with the Centre National de Recherches Forestières/ISRA is focusing on the selection of species with good nitrogen-fixative properties, on the selection of successful rhizobia strains and on inoculation in the nursery. Inoculation will enable the nursery stage to be shortened while still providing high quality plants. The behaviour of rhizobia when planted during the dry season is also under study.
Since 1979, direct drilling trials in the natural environment have given highly encouraging results, raising hopes that planting the species will prove to be inexpensive.
Soil: the soil is known locally as "deck dior", consisting of deck soils (vertisols with a temporarily moist soil climate, lithomorphic soils with massive intergrade surface structure consisting of ferruginous soils) but with a much lower clay content in the upper horizons. Plant spacing: 3m × 3m; the plants were holed manually in large seed holes (60 cm × 60 cm × 60 cm).
The plants introduced in 1974 and 1976 (see Annexes 1 and 2 for detailed results) have enabled an initial idea of the behaviour of these species to be gained:
a) A. cynophylla plants died;b) A. farnesiana, spathulata, tenuisissima and tetragonophylla are in the process of dying;
c) A. coriacea, dunnii, inaequlatera, monticola, mountfordea, plectocarpa and pyrifolia are surviving but their performance is mediocre;
d) A. bivenosa, holosericea, linariodes, sclerosperma and tumida are behaving satisfactorily.
Since 1976 a comparative trial on behaviour and production between local and Australian acacias has been launched, giving us a clearer idea of their suitability (see the results recorded in Table 1)
Table 1. Comparative trial on behaviour and production of local and Australian acacias: results of measurements at Bambey site, 1976.
12/1976 |
7/1977 |
12/1977 |
5/1978 |
12/1978 |
6/1979 |
12/1979 | ||||||||
H |
% |
H |
H |
s |
H |
s |
H |
s |
H |
s |
H |
s |
% | |
A. seyal |
108 |
94 |
154 |
168 |
13 |
181 |
9.8 |
239 |
22.3 |
283 |
29.0 |
294 |
30.8 |
93 |
A. senegal |
68 |
98 |
124 |
160 |
10 |
188 |
11.5 |
240 |
26.3 |
272 |
29.6 |
279 |
31.8 |
98 |
A. raddiana |
89 |
100 |
129 |
161 |
9 |
189 |
13.0 |
228 |
24.0 |
278 |
32.4 |
283 |
33.7 |
100 |
A. holosericea |
60 |
97 |
138 |
200 |
13 |
200 |
13.9 |
305 |
33.0 |
332 |
40.0 |
336 |
44.0 |
96 |
A.linarioïles |
88 |
88 |
199 |
229 |
17 |
186 |
21.4 |
251 |
61.3 |
256 |
65.3 |
264 |
67.1 |
81 |
H = height (in cm) s = section (in cm 2)
Variance analysis has demonstrated that since December 1977 the production of Acacia linarioïdes and holosericea has been significantly higher (5% theshold) than local acacias.
In this trial the spacing used was 3m × 3m and it appears that for all species competition become acute in December 1979. The stands were therefore thinned out to 3m × 6m in February 1980, and the data gathered at that time are recorded in Table 2.
Table 2. Comparative trial on behaviour and production of local and Australian acacias: data collected during thinning of stands from 3m × 3m to 3m × 6m at Bambey site, 1976.
Species |
Weight (kg) of dry leaves per tree |
Weight (kg) of dry leaves per hectare |
Weight (kg) of wood per tree |
Production (t) of wood per hectare |
Production (t) of wood per ha/year |
Production in steres per hectare |
Production in stere per ha/year |
A. seyal |
208 |
229 |
4.39 |
4.8 |
1.6 |
18.3 |
6 |
A. senegal |
60 |
66 |
9.92 |
10.9 |
3.6 |
36.5 |
12 |
A. raddiana |
130 |
143 |
5.89 |
6.5 |
2.1 |
24.1 |
8 |
A. holosericea |
2660 |
2926 |
12.03 |
13.2 |
4.4 |
36.5 |
12 |
A. linarioïdes |
1993 |
2192 |
10.65 |
11.7 |
3.9 |
54.7 |
18 |
It should be noted that measurements were carried out in the middle of the dry season, a time at which local acacias have lost a large proportion of their leaves, whereas Australian varieties mostly keep theirs.
It emerges clearly that wood production is higher in Australian varieties and that leaf production at this time of the year could contribute significantly to livestock feeds.
Soil: vertisols and brown eutrophic soils on alluvial clays and zoogenic limestones. The plant spacing used was 4.5 m × 4.5 m, after subsoiling with cross lands to a depth of 50 cm.
The plants introduced in 1977 (see Annex 4 for detailed results) gave results very similar to those at Bambey. Thus:
a) A. cyanophylla, Cyclops and tenuisissima died;b) A. dunnii, monticola, pyrifolia and tumida may or may not survive;
c) the performance of A. plectocarpa and salicina has to be verified;
d) lastly, A. bivenosa, coriacea, holosericea, linarioïles and sclerosperma gave interesting results (A. bivenosa, coriacea and sclerosperma are forming hybrids).
A. farnesiana, mountfordae and inaequilatera were only introduced at Bandia in 1979; their behaviour is therefore not yet significant.
Comparison of the best Australian varieties with local plants gives the results found in Table 3, but it should be empahsized that here the aim of the trial was to study the behaviour of each species individually and that, as a result, there were no replicates for comparison. Thus, Acacia nilotica and Prosopis juliflora are high as Acacia linarioides, but A. holosericea is the most productive of all.
Table 3. Results of comparison of best Australian with local species.
Species |
12/1977 |
6/1978 |
12/1978 |
6/1979 |
11/1979 | ||||||
H |
% |
H |
H |
s |
% |
H |
s |
H |
s |
% | |
A. bivenosa 1538 |
57 |
95 |
93 |
145 |
10.1 |
93 |
179 |
14.9 |
216 |
28.1 |
93 |
A. coriacea 1460 |
58 |
100 |
105 |
171 |
9.8 |
100 |
219 |
20.8 |
264 |
31.9 |
100 |
A. holosericea 1459 |
43 |
100 |
144 |
278 |
24.4 |
100 |
284 |
19.2 |
382 |
63.7 |
100 |
A. aff. linarioïdes 1466 |
90 |
96 |
120 |
255 |
19.4 |
96 |
265 |
13.9 |
355 |
45.7 |
96 |
A. sclerosperma 1525 |
59 |
97 |
99 |
154 |
9.1 |
97 |
210 |
16.8 |
251 |
27.2 |
97 |
A. nilotica var. adansonii |
65 |
99 |
104 |
195 |
12.2 |
97 |
230 |
14.2 |
305 |
41.5 |
97 |
A. raddiana |
55 |
100 |
53 |
121 |
3.2 |
100 |
174 |
6.1 |
258 |
18.7 |
97 |
A. albida |
30 |
99 |
35 |
70 |
|
98 |
108 |
|
121 |
|
92 |
Prosopis juliflora |
87 |
99 |
125 |
243 |
11.8 |
99 |
307 |
23.7 |
379 |
40.1 |
99 |
Prosopis cineraria |
40 |
99 |
45 |
92 |
|
96 |
124 |
|
200 |
|
92 |
Direct drilling trials gave the results shown in Table 4. These results may be considered highly encouraging.
Table 4. Results of direct drilling trials.
Species |
Treated seeds |
Untreated seeds |
Final site occupied by a plant |
Laboratory Germination |
Acacia linarioïdes |
28% |
21% |
80% |
92% |
Acacia bivenosa |
20% |
9% |
58% |
94% |
Acacia holosericea |
8% |
10% |
52% |
97% |
Acacia tumida |
47% |
32% |
96% |
60% |
Acacia senegal |
1% |
0% |
5% |
50% |
Acacia nilotica |
38% |
25% |
89% |
40% |
Acacia raddiana |
11% |
3% |
63% |
11% |
Acacia seyal |
14% |
12% |
55% |
89% |
Acacia albida |
47% |
33% |
87% |
72% |
Prosopis juliflora |
13% |
5% |
44% |
88% |
Soil: this site, located on the edge of a salt pan, has a large variety of soils with more or less pronounced salinity and hydromorphic features. They are characterised by a gradual transition from bare soil with Salontchaks to a plant cover consisting of Combretum, via a grass cover and an Acacia seyal stand. The original mangrove swamp and its surrounding vegetation probably vanished during the last century. Spacing: the spacing used was 3 m × 3 m; the soil was tilled manually and large seed holes were dug (60 cm × 60 cm × 60 cm).
The 1977 trial (for detailed results see Annex 5) was intended to enable a number of Australian acacia species to be selected for colonizing soils of this kind. To this end six types of soil cover were defined:
a) pure salt pan (Ps);b) salt pan with grass cover (Sg);
c) soil with Acacia seyal (Sa);
d) soil with Combretum (Sc);
e) soil with Parinari (Sp);
f) bottom-land (BI);.
The results recorded were as follows:
a) A. holosericea and linarioïdes behaved quite remarkably throughout the entire range, especially A. holosericea, the performance of which on salt pan is astonishing, to say the least, and may be even suspect; this variety was also the only one to tolerate bottom-land (see Figure 1).
b) A. bivenosa and sclerosperma gave interesting results on soils with A. seyal, while A. plectocarpa did well on Combretum soils.
c) A. tumida, pyrifolia and monticola did not appear to adapt.
The 1978 trial dealt with the forestry methods applicable to these species, from the point of view of both browse and forage production on ferruginous hydromorphic soils with a pre-existing plant cover consisting of Combretum. The first trial tested spacing of 3 m × 3 m, 3 m × 6 m and 6 m × 6 m, using a Latin square layout with Acacia linarioïdes as a control batch.
Spacing |
12/1978 |
6/1979 |
12/1979 | ||||
H |
% |
H |
% |
H |
s |
% | |
3 m ×3 m |
82 |
100 |
177 |
99 |
251 |
45 |
99 |
3 m × 6 m |
81 |
100 |
169 |
99 |
268 |
67 |
93 |
6 m × 6 m |
84 |
100 |
165 |
99 |
268 |
77 |
95 |
Figure 1. Behaviour of A.. holosericea and A. linarioides.
The differences on the section recorded in December 1979 are highly significant. It may be noted that these individuals are already as well developed as the Acacia linarioïdes plants of the 1976 trial at Bambey. We may thus assume that foliage production is also about identical after 18 months.
A second trial launched in 1978 focused on the different possible methods for harvesting the wood and the foliage biomass (felling, cutting back, trimming, stripping, etc). Different forms of utilization were applied for the first time in February 1980 and are to be staggered until July 1980. The first results for trees 18 months old subjected to utilization in February and to a spacing of 3 m × 3 m were as follows:
Weight of leaves per tree |
Weight of leaves per ha (3m × 3m) |
Weight of wood per tree |
Weight of wood per ha (3m × 3m) | |
A.linarioïdes |
1845g |
2029g |
5.25 kg |
5.77t |
Thus it was concluded that the weight of leaves after 18 months was approximately identical to that of the Bambey plantation in 1976 after 36 months.
A third trial launched in 1979 was intended to test direct drilling techniques in the field.
Rates of germination resulting in viable plants.
Soil: edge of salt pans.
Species |
Treated seed |
Untreated seed |
A. holosericea |
51% |
28% |
A. bivenosa |
34% |
14% |
A.linarioides |
45% |
42% |
Prosopis juliflora |
27% |
7% |
A. seyal |
8% |
1% |
Ferruginous soils: soils with Combretum
Species |
Treated seed |
Untreated seed |
A. holosericea |
2% |
1% |
A. albida |
27% |
14% |
It was found that the resistance of young plants is closely linked to the soil type. Other kinds of trial will be launched this year.
Soil: brown-red subarid intergrade soils and ferruginous tropical soils. Plants were introduced in 1974, but unfortunately the low quantity of seed which we had available at the time only enabled us to plant about 10 individuals for each species. In any case the poor planting, maintenance and follow-up conditions have led us to discount these introductions as insignificant.
Soil: brown-red subarid intergrade soils and poorly developed ferruginous tropical soils. The species introduced were A. holosericea, A. linarioïdes, A. bivenosa, A. pyrifolia and A. tumida. All species developed spectacularly during the first year, but unfortunately there were considerable losses during the second year for A. holosericea and tumida. A. linoarioïdes, bivenosa and pyrifolia are surviving at present without showing any noticeable progress. More detailed research will be carried out in this area during this year.
Following these different adaptability tests, which will moreover be continued, the following selection may be put forward:
a) highly interesting species: A. holosericea and A. linarioïdes;
b) interesting species: A. holosericea, A. sclerosperma and coriacea;
c) species which show promise but will have to be confirmed: A. plectocarpa and A. salicina;
d) species for which we do not have enough experience: A. inaequilatera and A. mountfordae;
e) species not selected for the moment: A. dunnii, A. monticola, A. pyrifolia and A. tumida;
f) species which do not adapt: A. farnesiana, A. spathulata, A. tenuisissima, A. tetragonophylla, A. cyanophylla and A. Cyclops.
There is not doubt that the primary suitability of acacias is for browse. The persistence of the leaves throughout the year and the abundant foliage contrast strongly with our traditional acacias.
Feed value analyses have been carried out by the ISRA Laboratoire National de l'Elevage et de Recherches Véterinaires (see results detailed in Table 5).
Table 5. Feed value analyses (in% per kg of dm) of leaves collected on 12 December 1979 at Bandia.
Species |
Dry matter |
Mineral Contents |
Nitrogen extract |
Fat matter |
Cellulose |
Nitrogen free extract |
Insoluble hydrochloric acid |
P |
Ca |
A. holosericea | |||||||||
- dry leaves |
644 |
60 |
78 |
40 |
389 |
433 |
6 |
0.15 |
15.9 |
- green leaves |
477 |
63 |
141 |
87 |
386 |
323 |
4 |
0.85 |
16.1 |
A.linarioïdes |
471 |
72 |
146 |
50 |
326 |
406 |
4 |
1.55 |
17.5 |
A. bivenosa |
322 |
218 |
162 |
30 |
209 |
381 |
12 |
1.03 |
61.8 |
A. sclerosperma |
- |
199 |
140 |
41 |
314 |
306 |
13 |
1.36 |
50.5 |
A. coriacea |
352 |
190 |
126 |
40 |
276 |
368 |
3 |
1.01 |
48.0 |
A. plectocarpa |
419 |
89 |
147 |
75 |
304 |
385 |
31 |
1.51 |
32.2 |
A. salicina |
288 |
147 |
181 |
60 |
238 |
374 |
4 |
1.45 |
37.0 |
A. tumida |
423 |
72 |
157 |
67 |
302 |
402 |
20 |
1.50 |
19.2 |
A. pyrifolia |
391 |
43 |
157 |
53 |
368 |
389 |
2 |
1.01 |
16.8 |
A. monticola |
502 |
64 |
132 |
88 |
275 |
441 |
14 |
0.95 |
10.5 |
A. dunnii |
412 |
92 |
139 |
123 |
346 |
300 |
7 |
0.77 |
21.6 |
A. tenuisissima |
490 |
48 |
120 |
90 |
342 |
400 |
3 |
0.87 |
8.8 |
A. cyanophylla |
346 |
87 |
151 |
71 |
328 |
263 |
3 |
1.33 |
26.4 |
Prosopis juliflora |
352 |
110 |
211 |
67 |
303 |
309 |
10 |
1.86 |
21.0 |
Prosopis cineraria |
419 |
60 |
135 |
45 |
389 |
371 |
5 |
1.69 |
11.8 |
Compare: Acacia albida |
410 |
86 |
171 |
30 |
215 |
498 |
41 |
1.37 |
14.1 |
Obviously there are variable differences between the species in terms of contents of primary elements, but all varieties contain valuable levels of nitrogen, higher than 12% and reaching 18%. Three species have a clearly higher level of minerals, especially calcium, than the others: first Acacia bivenosa, then Acacia sclerosperma and Acacia coriacea.
In addition pod harvests were carried out during February 1980 and are currently being analysed.
Finally, the palatability of all these acacia species was tested during December 1979, under the following conditions: a makeshift enclosure round four trees of the same species in which two head of cattle or three sheep were pastured for one or two days at the most. Thus the spontaneous palatability was tested and the results were as follows:
Cattle |
Sheep | |
A.linarioïdes |
P |
P |
A. bivenosa |
NP |
NP |
A. sclerosperma |
NP |
NP |
A. coriacea |
NP |
NP |
A. plectocarpa |
P |
P |
A. salicina |
PP |
PP |
A. pyrifolia |
P |
P |
A. monticola |
P |
P |
A. tumida |
PP |
PP |
Prosopis juliflora |
PP |
PP |
Prosopis cineraria |
PP |
PP |
The results presented here are the first ones carried out at a time when the animals still have grassland available in satisfactory amounts and are in a generally good state, but probably they would behave differently if all they could obtain was dried grass which was scanty and poor in feed value. Also, two further tests will be carried out in March and June and it should be noted that, as regards Acacia holosericea the palatability test was positive when the leaves were offered to the animals dry.
Pending the results of the various palatability tests as well as of production experiments using harvesting by trimming, pitching and felling, and pending the launching of trials to determine overall feed biomass (grass cover plus browse) as a function of spacing and hence the forestry technique to be used it may be pointed out that some species, especially Acacia linarioïdes offer valuable dry-season browse possibilities which could be utilized either by introducing browse stands on farmland or by organizing forest for pastoral use. In 1980 a pilot scheme will be launched on the Sangalkam experimental farm of the Laboratoire National de l'Elevage et des Recherches Veterinaires (ISRA).
Some Australian acacias have a natural habit and a crown which renders them particularly satisfactory as low-stratum components in a windbreak. Particularly advocated is the combination of Eucalyptus camaldulensis with Acacia holosericea. These two species are often combined in their original habitats in Australia:
a) Eucalyptus camaldulensis would provide the upper stratum of the wind-break; it is a tree over 12 m in height in the Sudano-Sahelian zone, but can reach 20 m or more in more favourable conditions. This tree has a first rate ability to put out new shoot and would thus permit regular utilization, while also providing farmers with firewood or timber in large amounts. When two new shoots are selected the wind-break may be built up very rapidly and is entirely satisfactory.
In order to avoid excessive competition with agricultural crops it is recommended that subsoiling along the windbreak be carried out before the dry season so as to cut outrunning roots.
b) Acacia holosericea (probably A. plectocarpa and A. salicina also) would provide the lower level in the windbreak, thanks to its low height (5 to 6 m in the Sahelo-Sudanian zone), but more especially to its plentiful and dense crown, which often very rapidly reaches 4 to 5 m in diameter at both the base and the summit.
The most satisfactory arrangement of these two species would be the following combination:
+ 0+0+0 +
As regards soil protection and particularly the prevention of runoff erosion, all the species are able to play a valuable part, although probably Acacia bivenosa is the most suitable. This bush covers the soil particularly well and its behaviour on difficult land is good. But we can also draw attention to Acacia coriacea, sclerosperma and linarioïdes.
For stabilizing shifting sand, or more accurately for protecting niayes (bottom-land suitable for marshland cultivation) against sand encroachment, a number of tests have been carried out under a UNDP project at Kebemer, using A. holosericea, tumida, linarioïdes, cyanophylla and Cyclops. The behaviour of A. holosericea and linarioïdes is on the whole satisfactory.
After 5 years of experiments with these species, it appears that Australian acacias suited to our climate have a browse production which is equal to or higher than local species (see the results at Bambey and Bandia), but our knowledge as to wood quality is largely insufficient and studies on charcoal production and quality have only just begun, using recent utilizations.
Given the growth pattern of the trees it would appear that A. holosericea, plectocarpa and salicina are probably suitable for making good charcoal, since they are trees which have a main trunk, whereas A. linarioïdes, bivenosa, sclerosperma and coriacea are bushes with a large number of fairly thin branches, making them easier to use for firewood than for turning into charcoal.
As regards subsidiary products, studies have not yet begun but they will focus on rubber and honey production, and on any other product which is likely to be valuable to the local population.
The different varieties of Australian acacia provide a variety of phyllodes, habit, behaviour and growth which is truly astonishing. We can exploit this rich variety by adapting their features to our own objectives. Thus, if we have to select only one species for each use, we would identify the following in the light of our present knowledge:
a) Acacia linarioïdes for its feed value;
b) Acacia holosericea for windbreaks;
c) Acacia bivenosa for runoff erosion prevention;
d)Acacia holosericea again for firewood and charcoal.
Given our fairly recent experience of the species we cannot yet with any certainty say that their drought resistance is the same as that of local acacias, but if this is the case these acacias will only complete the range of utilization found in our own traditional varieties without in any way replacing them.
In any case our range of intervention in the Sudanian and Sahelian zones has been enriched by several species which can be used with discernment.
Sites of Australian seeds
Species |
Long. |
Lat. |
Altit. |
Distance from sea |
Nearest met station |
Site where introduced in Senegal |
A. bivenosa | ||||||
1457/CTFT |
121 ° 07' |
19° 33' |
30 m |
1 km |
Anna Plains and Condon |
Bambey Bandia Keur Mactar |
1526/CTFT |
114° 56' |
22° 53' |
10 m |
75 km |
Winning Pool |
Bambey |
1538/CTFT |
113° 57' |
21° 57' |
10 m |
200 km |
Onslow |
Bambey Bandia Linguère Keur Mactar M'Biddi |
A. coriacea | ||||||
1536/CTFT |
114° 05' |
21° 50' |
5 m |
200 km |
Onslow |
Bambey Bandia Linguère Keur Mactar |
A. dunnii | ||||||
1395/CTFT |
126° 37' |
14° 37' |
90 m |
25 km |
Port George IV - Wyndham |
Bambey Bandia |
A. farnesiana | ||||||
1534/CTFT |
114° 19' |
22° 50' |
50 m |
25 km |
Winning Pool and Onslow |
Bambey Bandia Linguère |
A. holosericea | ||||||
1125/CTFT |
131° 07' |
13° 21' |
120 m |
125 km |
Katerine and Darwin |
Bandia |
1459/CTFT |
121° 05' |
19° 37' |
50 m |
2 km |
Anna Plains and Condon |
Bambey Bandia Linguère Keur Mactar M'Biddi Kébémer |
A. inaequilatera | ||||||
1509/CTFT |
118° 51' |
21° 18' |
480 m |
183 km |
Nullagine |
Bambey Bandia Linguère Keur Mactar |
A. off. linarioïdes | ||||||
1466/CTFT |
118° 36' |
20° 22' |
30 m |
10 km |
Port Hedland |
Bambey Bandia Linguère Keur Mactar M'Biddi Kébémer |
A. monticola | ||||||
1460/CTFT |
120° 40' |
19° 49' |
30 m |
5 km |
Anna Plains and Condon |
Bambey Bandia Linguère Keur Mactar |
A. mountfordae | ||||||
1217/CTFT |
133° 04' |
12° 05' |
40 m |
50 km |
Oenpelli and Darwin |
Bambey Bandia |
A. Plectocarpa | ||||||
1261/CTFT |
134° 17' |
12° 53' |
160 m |
90 km |
Oenpelli and Darwin |
Bambey Bandia |
A. pyrifolia | ||||||
1461/CTFT |
119° 26' |
20° 03' |
100 m |
19 km |
Condon and Port Hedland |
Bambey Bandia |
1477/CTFT |
117° 16' |
21° 30' |
230 m |
65 km |
Roebourne and Marble Bar |
Bambey Bandia |
1524/CTFT |
117° 50' |
22° 14' |
560 m |
165 km |
Nullagine and Roy Hill |
Bambey |
1532/CTFT |
114° 19' |
22° 19' |
50 m |
25 km |
Winnima Pool et Onslow |
Bambey Bandia Keur Mactar M'Biddi |
A. sclerosperia | ||||||
1525/CTFT |
117° 09' |
22° 59' |
400 m |
230 km |
Nullagine |
Bambey Bandia Linguère Keur Mactar |
A. spathulata | ||||||
1539/CTFT |
114° 02' |
22° 36' |
50 m |
15 km |
Winning Pool and Onslow |
Bambey Linguère |
A. tenuisissima | ||||||
1485/CTFT |
117° 45' |
21° 41' |
480 m |
113 km |
Roebourne and Marble Bar |
Bambey |
1519/CTFT |
117° 57' |
22° 14' |
560 m |
164 km |
Bullagine and Roy Hill |
Bambey Bandia Keur Mactar |
A. tetragonophylla | ||||||
1548/CTFT |
113° 26' |
24° 15' |
5 m |
3 km |
Carnavon |
Bambey Linguère |
A. tumida | ||||||
1422/CTFT |
122° 56' |
16° 25' |
5 km |
600 km |
Port George IV |
Bambey Bandia Linguère Keur Mactar M'Biddi Kébémer |
1462/CTFT |
119° 23' |
20° 03' |
110 m |
15 km |
Condon and Port Hedland |
Bambey Bandia |
1484/CTFT |
117° 45' |
21° 41' |
480 m |
113 km |
Roebourne and Marble Bar |
Bandia |
A. cyanophylla |
Morocco |
Bambey Bandia Linguère | ||||
A. cyclops |
Morocco |
Bandia Keur Mactar | ||||
A. salicina |
Tunisia |
Bandia Keur Mactar | ||||
Climatological data for Australian sites: Meteorological office, Melbourne ( Pls. make the columns of Annex Ib wide)
Sites |
01 |
02 |
03 |
04 |
05 |
06 |
07 |
08 |
09 |
10 |
11 |
12 |
Year | ||||||
Nullagine 120° 05' 21° 53' 385 m (Western Australia) |
|||||||||||||||||||
Av. max T. |
°C | 39.0 |
38.4 |
36.7 |
32.9 |
28.0 |
24.1 |
24.0 |
26.6 |
31.3 |
35.0 |
28.3 |
39.4 |
32.8 | |||||
Av. min T. |
°C | 24.0 |
23.5 |
21.7 |
16.7 |
11.9 |
8.3 |
7.0 |
8.8 |
12.3 |
17.0 |
21.3 |
23.3 |
16.3 | |||||
Av. T. |
°C | 31.5 |
30.9 |
29.2 |
24.8 |
19.9 |
16.2 |
15.5 |
17.7 |
21.8 |
26.0 |
29.8 |
31.4 |
24.5 | |||||
Av. rel. humid at 9 hour |
% | 40 |
40 |
41 |
40 |
46 |
49 |
49 |
43 |
35 |
31 |
30 |
35 |
39 | |||||
Av. daily rel. humid |
% | 25 |
25 |
26 |
25 |
30 |
33 |
33 |
28 |
22 |
19 |
19 |
22 |
26 | |||||
Rainfall |
mm | 82.8 |
59.4 |
51.1 |
17.3 |
17.5 |
20.1 |
6.1 |
5.1 |
1.5 |
6.6 |
15.5 |
46.7 |
329.7 | |||||
Marble Bar 119° 54' 21° 11' 181 m (Western Australia) | |||||||||||||||||||
Av. max T. |
°C | 41.2 |
40.9 |
30.3 |
36.1 |
31.1 |
27.2 |
27.0 |
29.9 |
34.3 |
37.8 |
41.0 |
41.9 |
35.7 | |||||
Av. min T. |
°C | 26.0 |
25.7 |
24.9 |
20.9 |
16.2 |
12.6 |
11.3 |
13.2 |
16.5 |
20.4 |
24.0 |
25.7 |
19.7 | |||||
Av. T. |
°C | 33.6 |
33.3 |
32.1 |
28.5 |
23.6 |
19.9 |
19.2 |
21.6 |
25.4 |
29.1 |
32.5 |
33.8 |
27.7 | |||||
Av. rel. humid at 9 hour |
% | 42 |
44 |
35 |
38 |
44 |
48 |
42 |
38 |
34 |
31 |
31 |
36 |
39 | |||||
Av. daily rel. humid |
% | 28 |
28 |
32 |
28 |
32 |
34 |
31 |
28 |
24 |
22 |
22 |
24 |
28 | |||||
Rainfall |
mm | 79.5 |
61.0 |
45.0 |
22.1 |
17.0 |
23.1 |
5.1 |
4.1 |
1.3 |
7.8 |
8.1 |
39.1 |
313.2 | |||||
Condon 119° 22' 20° 00' 10 m (Western Australia) | |||||||||||||||||||
Av. max T. |
°C | 34.8 |
34.5 |
34.5 |
32.8 |
28.6 |
25.6 |
24.8 |
27.0 |
29.7 |
32.7 |
34.4 |
34.3 |
31.1 | |||||
Av. min T. |
°C | 25.2 |
25.5 |
23.1 |
19.4 |
15.4 |
12.1 |
10.8 |
11.6 |
13.8 |
17.2 |
21.1 |
23.7 |
18.1 | |||||
Av. T. |
°C | 30.0 |
29.8 |
28.8 |
26.1 |
22.0 |
18.5 |
17.8 |
19.3 |
21.8 |
25.0 |
27.7 |
29.0 |
24.6 | |||||
Av. rel. humid at 9 hour |
% | 62 |
69 |
64 |
58 |
57 |
63 |
63 |
62 |
61 |
60 |
62 |
69 |
63 | |||||
Av. daily rel. humid |
% | |
|
|
|
|
|
|
|
|
|
|
| ||||||
Rainfall |
mm | 56.6 |
64.8 |
77.0 |
23.9 |
18.3 |
27.7 |
9.7 |
4.0 |
0.7 |
1.0 |
1.8 |
16.5 |
302.8 | |||||
Port Hedland 118° 24' 20° 19' 7 m (Western Australia) | |||||||||||||||||||
Av. max T. |
°C | 34.6 |
34.8 |
35.2 |
34.0 |
30.0 |
26.8 |
26.2 |
27.9 |
30.5 |
32.0 |
34.0 |
34.5 |
31.8 | |||||
Av. min T. |
°C | 26.4 |
26.2 |
25.4 |
21.8 |
17.6 |
14.4 |
13.2 |
14.6 |
17.0 |
2.0 |
23.0 |
25.3 |
20.4 | |||||
Av. T. |
°C | 30.5 |
30.5 |
30.3 |
27.9 |
23.8 |
20.6 |
19.7 |
21.2 |
23.7 |
26.0 |
28.5 |
29.9 |
26.1 | |||||
Av. rel. humid at 9 hour |
% | 67 |
63 |
60 |
48 |
50 |
49 |
49 |
50 |
49 |
53 |
56 |
61 |
55 | |||||
Av. daily rel. humid |
% | 63 |
63 |
56 |
49 |
49 |
48 |
47 |
49 |
49 |
52 |
55 |
60 |
53 | |||||
Rainfall |
mm | 42.2 |
52.6 |
78.0 |
24.1 |
24.9 |
24.4 |
6.1 |
9.7 |
1.3 |
2.3 |
0.5 |
8.6 |
279.7 | |||||
Roebourne 177° 09' 20° 46' 12 m (Western Australia) | |||||||||||||||||||
Av. max T. |
°C | 38.2 |
38.2 |
37.0 |
34.4 |
30.1 |
26.3 |
26.1 |
28.3 |
32.0 |
34.6 |
38.0 |
38.8 |
33.5 | |||||
Av. min T. |
°C | 26.2 |
26.2 |
25.2 |
21.4 |
17.8 |
14.5 |
13.0 |
14.2 |
16.4 |
16.2 |
23.0 |
24.8 |
20.1 | |||||
Av. T. |
°C | 32.2 |
32.2 |
31.1 |
27.9 |
23.9 |
20.4 |
19.5 |
21.2 |
24.2 |
26.9 |
30.5 |
31.8 |
26.8 | |||||
Av. rel. humid at 9 hour |
% | 52 |
53 |
55 |
46 |
48 |
51 |
47 |
48 |
41 |
43 |
42 |
47 |
48 | |||||
Av. daily rel. humid |
% | 41 |
42 |
43 |
36 |
38 |
40 |
36 |
36 |
29 |
33 |
33 |
37 |
37 | |||||
Rainfall |
mm | 42.2 |
47.0 |
85.9 |
24.6 |
27.7 |
21.8 |
5.6 |
5.1 |
2.0 |
1.6 |
1.6 |
14.0 |
278.9 | |||||
Darwin 130° 51' 12° 28' 29 m (Northern Territory) | |||||||||||||||||||
Av. max T. |
°C | 32.1 |
32.0 |
32.3 |
33.2 |
32.2 |
30.9 |
30.3 |
31.4 |
32.8 |
33.7 |
34.0 |
33.3 |
32.3 | |||||
Av. min T. |
°C | 25.1 |
25.0 |
25.1 |
24.4 |
22.5 |
20.9 |
19.9 |
20.9 |
23.2 |
25.1 |
25.7 |
25.6 |
23.6 | |||||
Av. T. |
°C | 28.6 |
28.5 |
28.7 |
28.8 |
27.4 |
25.9 |
25.1 |
26.2 |
28.0 |
29.4 |
29.8 |
29.4 |
28.0 | |||||
Av. rel. humid at 9 hour |
% | 80 |
80 |
79 |
68 |
60 |
55 |
55 |
61 |
65 |
69 |
70 |
73 |
68 | |||||
Av. daily rel. humid |
% | 71 |
72 |
68 |
54 |
47 |
47 |
44 |
45 |
49 |
52 |
58 |
68 |
56 | |||||
Rainfall |
mm | 411.0 |
314.2 |
284.0 |
78.2 |
8.4 |
2.3 |
0.2 |
0.5 |
15.2 |
49.0 |
109.8 |
217.7 |
490.5 | |||||
Wyndham 128° 07' 15° 27' 7 m (Western Australia) | |||||||||||||||||||
Av. max T. |
°C | 35.6 |
35.3 |
35.1 |
34.9 |
32.3 |
29.9 |
29.4 |
31.4 |
34.2 |
36.0 |
37.0 |
36.4 |
34.0 | |||||
Av. min T. |
°C | 26.8 |
26.6 |
26.4 |
25.1 |
22.4 |
20.0 |
19.0 |
20.9 |
23.8 |
26.6 |
27.4 |
27.4 |
24.3 | |||||
Av. T. |
°C | 31.2 |
30.8 |
30.8 |
30.0 |
27.3 |
25.0 |
24.2 |
26.1 |
29.0 |
31.3 |
32.2 |
31.9 |
29.1 | |||||
Av. rel. humid at 9 hour |
% | 66 |
67 |
63 |
46 |
41 |
40 |
38 |
40 |
44 |
52 |
55 |
60 |
51 | |||||
Av. daily rel. humid |
% | 54 |
54 |
49 |
38 |
37 |
37 |
35 |
39 |
33 |
47 |
50 |
52 |
45 | |||||
Rainfall |
mm | 172.4 |
160.0 |
132.6 |
12.7 |
3.3 |
5.1 |
2.0 |
0.5 |
1.3 |
9.6 |
39.4 |
99.6 |
638.8 | |||||
Port George IV 124° 43' 15° 25' 594 m (Western Australia) | |||||||||||||||||||
Av. max T. |
°C | 32.6 |
32.4 |
32.9 |
33.9 |
32.3 |
30.4 |
30.0 |
31.8 |
33.9 |
34.5 |
35.1 |
34.1 |
32.5 | |||||
Av. min T. |
°C | 24.6 |
24.4 |
23.9 |
20.3 |
16.5 |
13.9 |
11.9 |
13.8 |
17.3 |
21.5 |
24.1 |
25.1 |
19.7 | |||||
Av. T. |
°C | 28.6 |
28.4 |
28.4 |
27.1 |
24.4 |
22.2 |
20.9 |
22.8 |
25.6 |
28.0 |
29.6 |
29.6 |
26.3 | |||||
Av. rel. humid at 9 hour |
% | 76 |
77 |
76 |
67 |
62 |
60 |
60 |
62 |
61 |
61 |
64 |
69 |
67 | |||||
Av. daily rel. humid |
% | |
|
|
|
|
|
|
|
|
|
|
|
| |||||
Rainfall |
mm | 284.0 |
282.7 |
254.3 |
54.4 |
24.4 |
19.1 |
7.6 |
1.0 |
1.5 |
9.9 |
46.7 |
194.3 |
1279.9 | |||||
Katherine 132° 42' 14° 06' | |||||||||||||||||||
Hottest month: av. max 38.1 - av. min: 24.7 | |||||||||||||||||||
Coldest month: av. max 30.2 - av. min: 13.2 | |||||||||||||||||||
Rainfall |
mm | 232.2 |
201.4 |
156.2 |
34.0 |
5.6 |
2.0 |
0.8 |
0.5 |
5.8 |
29.7 |
83.8 |
199.4 |
951.4 | |||||
Royhill 119° 54' 22° 36' | |||||||||||||||||||
Rainfall |
mm | 41.9 |
53.3 |
47.0 |
22.3 |
19.0 |
16.8 |
11.7 |
6.1 |
1.8 |
4.3 |
7.4 |
24.9 |
256.5 | |||||
Location of Senegalese research sites
S i t e s |
Long. |
Lat. |
Alt. |
Distance from sea |
Av. rainfall 1930/1961 |
Short-fall for 1970 |
Official met. station |
Bambey |
16° 28' |
14° 42' |
20m |
70 km |
665.8 |
30% |
Diourbel |
Bandia |
17° 02' |
14° 35' |
12m |
10 km |
(730.0) |
( 43%) |
Thiès |
linguere |
15° 07' |
15° 23' |
20m |
170 km |
525.2 |
35% |
Linguère |
Keur Mactar |
16° 11' |
14° 02' |
6m |
70 km |
788.7 |
29% |
Kaolack |
M'biddi |
14° 57' |
16° 08' |
170 km |
(400.0) |
Podor |
Climatological data for Senegalese sites (Asecna)
S i t e s |
01 |
02 |
03 |
04 |
05 |
06 |
07 |
08 |
09 |
10 |
11 |
12 |
Year | |
Podor 14° 56'W 16° 33' N | ||||||||||||||
Av. max T. |
°C |
31.5 |
32.7 |
37.4 |
39.4 |
41.3 |
40.2 |
36.8 |
34.7 |
34.6 |
35.0 |
34.1 |
30.1 |
35.7 |
Av. min T. |
°C |
15.2 |
16.1 |
18.2 |
20.5 |
22.5 |
23.9 |
24.4 |
24.4 |
24.9 |
24.9 |
21.8 |
16.5 |
21.1 |
Av. T. |
°C |
23.2 |
24.8 |
27.5 |
26.9 |
32.1 |
32.2 |
30.8 |
29.8 |
29.8 |
30.0 |
28.0 |
23.1 |
28.1 |
Av. daily rel. humid |
% |
30 |
28 |
24 |
22 |
26 |
37 |
54 |
63 |
65 |
53 |
43 |
34 |
40 |
Rainfall |
mm |
0.6 |
1.6 |
0.0 |
0.1 |
3.2 |
16.2 |
67.7 |
133.3 |
83.8 |
23.2 |
3.0 |
2.0 |
334.7 |
Linguere 150° 07' 15° 23 N | ||||||||||||||
Av. max T. |
°C |
33.2 |
34.1 |
38.2 |
40.0 |
40.5 |
38.0 |
34.5 |
32.7 |
33.2 |
35.8 |
36.6 |
32.4 |
35.8 |
Av. min T. |
°C |
15.1 |
16.5 |
18.1 |
19.9 |
21.7 |
23.4 |
23.6 |
23.4 |
23.1 |
21.8 |
19.0 |
16.4 |
20.2 |
Av. T. |
°C |
24.0 |
25.6 |
27.9 |
29.8 |
31.2 |
30.9 |
29.1 |
27.9 |
28.6 |
27.4 |
23.9 |
27.8 |
|
Av. daily rel. humid |
% |
24 |
27 |
27 |
29 |
34 |
47 |
64 |
74 |
76 |
56 |
41 |
31 |
44 |
Rainfall |
mm |
0.1 |
1.5 |
1.6 |
0.0 |
3.6 |
31.4 |
100.7 |
209.0 |
135.5 |
45.0 |
4.3 |
2.0 |
534.7 |
Diourbel 16° 14' 14° 39 N | ||||||||||||||
Av. max T. |
°C |
33.7 |
34.5 |
38.4 |
39.7 |
39.9 |
37.4 |
33.8 |
31.9 |
32.9 |
35.2 |
36.1 |
32.7 |
35.5 |
Av. min T. |
°C |
14.2 |
15.4 |
16.7 |
17.9 |
20.1 |
22.6 |
23.1 |
22.9 |
22.6 |
21.7 |
18.6 |
15.5 |
19.3 |
Av. T. |
°C |
23.7 |
25.2 |
27.2 |
28.6 |
29.8 |
30.1 |
28.6 |
27.7 |
27.7 |
28.4 |
27.0 |
23.7 |
27.3 |
Av. daily rel. humid |
% |
37 |
39 |
39 |
40 |
48 |
59 |
72 |
77 |
80 |
71 |
55 |
41 |
55 |
Rainfall |
mm |
0.1 |
1.3 |
0.1 |
0.2 |
6.3 |
40.2 |
139.5 |
259.8 |
189.1 |
55.0 |
4.5 |
4.2 |
700.3 |
Kaolack 16° 04'W 13° 46 N | ||||||||||||||
Av. man T. |
°C |
33.9 |
34.9 |
38.7 |
39.7 |
38.4 |
35.7 |
32.5 |
31.2 |
32.5 |
34.3 |
35.7 |
33.1 |
35.1 |
Av. min T. |
°C |
15.6 |
16.8 |
18.0 |
19.6 |
21.4 |
23.6 |
23.8 |
23.2 |
23.2 |
23.1 |
20.4 |
16.9 |
20.5 |
Av. T. |
°C |
24.8 |
26.5 |
28.5 |
29.6 |
30.3 |
30.0 |
28.7 |
27.6 |
28.1 |
28.8 |
27.8 |
25.2 |
27.9 |
Av. daily rel. humid |
% |
32 |
36 |
35 |
38 |
48 |
63 |
75 |
82 |
83 |
75 |
57 |
41 |
55 |
Rainfall |
mm |
0.5 |
0.9 |
0.0 |
0.1 |
78 |
61.1 |
160.2 |
295.1 |
200.7 |
63.8 |
4.0 |
2.6 |
796.8 |
Thies 14° 48'w 16° 57 n | ||||||||||||||
Av man T. |
°C |
31.6 |
31.6 |
33.6 |
33.4 |
33.1 |
33.3 |
31.7 |
30.6 |
31.4 |
32.6 |
33.4 |
30.9 |
32.3 |
Av. min T. |
°C |
15.0 |
15.9 |
16.8 |
17.1 |
19.6 |
21.9 |
22.8 |
22.7 |
22.5 |
21.7 |
18.9 |
16.1 |
19.3 |
Av. T. |
°C |
23.3 |
23.8 |
25.2 |
25.3 |
26.4 |
27.6 |
27.3 |
26.7 |
27.0 |
27.2 |
26.2 |
23.5 |
25.8 |
Av. daily rel. humid |
% |
|||||||||||||
Rainfall |
mm |
0.2 |
1.8 |
0.1 |
0.1 |
1.6 |
24.2 |
121.9 |
273.0 |
206.3 |
57.1 |
3.4 |
5.1 |
694.8 |
Bambey site: 1974 introductions measured in Nov. 1979
Species |
Provenance |
Height (cm) |
Section at base |
A. bivenosa |
1538 |
258 |
74 |
1457 |
258 |
48 | |
1426 |
256 |
63 | |
A. coriacea |
1536 |
235 |
22 |
A. dunii |
1395 |
415 |
24 |
A.farnesiana |
1534 |
190 |
32 |
A. holosericea |
1459 |
416 |
107 |
A. inaequilatera |
1509 |
360 |
92 |
A. aff. linarioïdes |
1466 |
280 |
99 |
A. monticola |
1460 |
287 |
39 |
A. pyrifolia |
1477 |
370 |
108 |
1532 |
344 |
44 | |
A. sclerosperma |
1525 |
295 |
49 |
1549 |
207 |
35 | |
1543 |
207 |
38 | |
A. spathulata |
1539 |
120 |
12 |
A. tenuisissima |
1519 |
156 |
26 |
1485 |
184 |
28 | |
A. tetragonophyla |
1548 |
85 |
4 |
A. tumida |
1462 |
425 |
170 |
A. cyanophylla |
Morocco |
|
|
Bambey site
1974 introductions measured in Nov. 1979
A. bivenosa |
1538 |
265 |
62 |
94 |
1457 |
210 |
25 |
82 | |
1526 By |
207 |
30 |
79 | |
270 |
52 |
91 | ||
A. dunii |
1395 |
415 |
66 |
73 |
A. holosericea |
1459 |
380 |
68 |
91 |
1459 By |
346 |
52 |
79 | |
A. aff. linarioïdes |
1466 By |
259 |
53 |
82 |
A. monticola |
1460 |
226 |
18 |
|
A. mountfordae |
1217 |
256 |
46 |
|
A. plectocarpa |
1261 |
248 |
28 |
|
1477 |
236 |
17 |
82 | |
1461 |
245 |
22 |
58 | |
A. pyrifolia |
1532 |
270 |
30 |
64 |
1524 By |
309 |
22 |
||
282 |
28 |
70 | ||
A. tenuisissima |
1485 |
212 |
49 |
|
1519 |
160 |
15 |
| |
A. tumida |
1442 |
384 |
127 |
73 |
Bandia site
1977 introductions
12/1977 |
6/1978 |
12/1978 |
6/1979 |
11/1979 | ||||||||
Species |
H |
% |
H |
H |
S |
% |
H |
S |
H |
S |
% | |
A. bivenosa |
1538 |
47 |
93 |
84 |
146 |
10.9 |
90 |
170 |
13.3 |
221 |
30.6 |
90 |
1457 |
51 |
92 |
65 |
148 |
6.3 |
90 |
168 |
15.4 |
227 |
22.5 |
90 | |
By 1538 |
67 |
98 |
108 |
144 |
9.4 |
97 |
188 |
16.5 |
211 |
25.7 |
97 | |
A. coriacea |
By 1460 |
58 |
100 |
105 |
171 |
9.8 |
100 |
219 |
20.8 |
264 |
31.9 |
100 |
A. dunii |
1395 |
|
|
131 |
315 |
19.5 |
50 |
|
|
400 |
34.0 |
50 |
By 1395 |
32 |
75 |
146 |
303 |
17.3 |
67 |
321 |
24.2 |
366 |
31.7 |
67 | |
1459 |
40 |
100 |
157 |
293 |
30.6 |
100 |
301 |
19.5 |
400 |
74.6 |
100 | |
A. holosericea |
1125 |
84 |
90 |
159 |
239 |
19.7 |
66 |
263 |
14.9 |
325 |
56.6 |
64 |
By 1459 |
46 |
100 |
131 |
264 |
18.3 |
100 |
268 |
19.0 |
365 |
52.8 |
100 | |
A. aff. linarioïdes |
By 1468 |
90 |
96 |
126 |
255 |
19.4 |
96 |
265 |
13.9 |
355 |
45.7 |
96 |
A. monticola |
1460 |
37 |
62 |
117 |
206 |
12.2 |
50 |
222 |
15.4 |
298 |
32.9 |
48 |
By 1460 |
40 |
94 |
116 |
229 |
10.1 |
92 |
218 |
15.2 |
218 |
23.1 |
92 | |
A. plectocarpa |
1261 |
35 |
72 |
91 |
195 |
15.2 |
72 |
263 |
17.1 |
364 |
46.3 |
68 |
1532 |
42 |
94 |
91 |
189 |
14.8 |
92 |
249 |
12.0 |
282 |
16.6 |
92 | |
1461 |
49 |
78 |
100 |
206 |
11.2 |
78 |
182 |
13.8 |
275 |
20.3 |
78 | |
A. pyrifolia |
1477 |
45 |
50 |
84 |
183 |
11.7 |
90 |
240 |
12.8 |
242 |
17.8 |
90 |
By 1477 |
39 |
88 |
91 |
240 |
10.4 |
88 |
225 |
12.4 |
271 |
20.7 |
84 | |
By 1532 |
57 |
100 |
96 |
270 |
17.1 |
100 |
252 |
17.2 |
279 |
21.1 |
76 | |
A. sclerosperma |
By 1525 |
59 |
97 |
99 |
154 |
9.1 |
97 |
210 |
16.8 |
251 |
27.2 |
97 |
A. tenuisissima |
1519 |
9 |
69 |
47 |
121 |
|
63 |
133 |
|
174 |
|
56 |
1442 |
26 |
100 |
95 |
304 |
26.4 |
72 |
262 |
20.4 |
370 |
48.3 |
85 | |
A.tumida |
1484 |
42 |
100 |
112 |
255 |
15.9 |
90 |
251 |
18.2 |
382 |
28.0 |
83 |
By 1462 |
67 |
98 |
142 |
274 |
15.1 |
93 |
287 |
|||||
A. cyanophylla |
Maroc |
51 |
94 |
140 |
223 |
24.4 |
80 |
153 |
15.0 |
277 |
35.7 |
40 |
A. cyclops |
Maroc |
29 |
91 |
54 |
80 |
|
44 |
88 |
|
120 |
| 7 |
12/1978 |
6/1979 |
11/1979 |
||||||||||
Species |
H |
% |
H |
H |
S |
% |
H Height in cm | |||||
A. salicina |
91 |
100 |
221 |
266 |
99 |
S Section in cm2 | ||||||
Keur-Mactar site 1977 trials
Soil beneath Acacia seyal
Species |
12/1977 |
6/1978 |
12/1978 |
6/1979 |
12/1979 | |||||||
H |
% |
H |
% |
H |
% |
H |
S |
% |
H |
S |
% | |
A. holosericea |
49 |
100 |
105 |
100 |
193 |
100 |
242 |
23 |
100 |
250 |
45 |
100 |
A.linarioïdes |
78 |
96 |
96 |
96 |
131 |
96 |
159 |
18 |
96 |
237 |
42 |
96 |
A. bivenosa |
56 |
100 |
48 |
100 |
73 |
96 |
136 |
9 |
96 |
170 |
|
96 |
A. tumida |
60 |
76 |
100 |
68 |
156 |
68 |
220 |
23 |
68 |
226 |
29 |
56 |
A. sclerosperma |
65 |
96 |
73 |
97 |
119 |
96 |
168 |
11 |
96 |
203 |
|
96 |
A. pyrifolia |
45 |
60 |
64 |
56 |
101 |
52 |
140 |
11 |
52 |
234 |
|
52 |
A. plectocarpa |
32 |
24 |
48 |
20 |
68 |
16 |
120 |
7 |
12 |
157 |
18 |
12 |
Soil beneath Combretum
A, holoserica |
47 |
92 |
87 |
92 |
201 |
92 |
224 |
24 |
92 |
354 |
45 |
88 |
A. linarioides |
98 |
96 |
104 |
96 |
178 |
96 |
213 |
25 |
96 |
276 |
53 |
96 |
A. bivenosa |
52 |
88 |
49 |
88 |
91 |
88 |
138 |
11 |
88 |
193 |
|
88 |
A.tumida |
59 |
88 |
101 |
88 |
161 |
84 |
217 |
17 |
84 |
342 |
41 |
72 |
A. sclerosperma |
63 |
96 |
73 |
96 |
120 |
96 |
188 |
17 |
96 |
220 |
|
96 |
A. plectocarpa |
53 |
80 |
79 |
80 |
173 |
80 |
228 |
29 |
80 |
319 |
60 |
80 |
Soil beneath Parinari
A. holosericea |
48 |
100 |
100 |
100 |
186 |
100 |
268 |
24 |
96 |
383 |
44 |
96 |
A.linarioides |
88 |
100 |
132 |
100 |
162 |
100 |
197 |
25 |
100 |
282 |
66 |
100 |
A. bivenosa |
57 |
96 |
58 |
88 |
83 |
28 |
137 |
8 |
92 |
177 |
|
92 |
A.tumtda |
76 |
100 |
189 |
96 |
175 |
76 |
256 |
29 |
76 |
400 |
66 |
72 |
A. sclerospenna |
65 |
100 |
76 |
96 |
97 |
92 |
95 |
3 |
24 |
133 |
|
24 |
A. monticola |
58 |
60 |
115 |
60 |
151 |
32 |
211 |
19 |
32 |
259 |
38 |
32 |
A. coriacea |
56 |
96 |
79 |
96 |
119 |
88 |
161 |
8 |
84 |
417 |
22 |
76 |
H = height in cm; S = Section in cm2
Bottom land
Species |
12/1977 |
6/1978 |
12/1978 |
6/1979 |
12/1979 | |||||||
H |
% |
H |
% |
H |
% |
H |
S |
% |
H |
S |
% | |
A. holosericea |
50 |
100 |
145 |
100 |
254 |
100 |
302 |
32 |
100 |
436 |
71 |
100 |
A.linarioides |
92 |
92 |
140 |
92 |
114 |
36 |
187 |
19 |
56 |
270 |
44 |
32 |
A. bivenosa |
56 |
92 |
62 |
92 |
45 |
8 |
120 |
28 |
8 |
180 |
|
8 |
A.tumida |
67 |
92 |
150 |
84 |
134 |
56 |
260 |
32 |
52 |
392 |
77 |
52 |
A.sclerosperma |
74 |
88 |
67 |
88 |
59 |
44 |
166 |
14 |
44 |
183 |
|
40 |
A. monticola |
56 |
92 |
111 |
92 |
180 |
4 |
210 |
10 |
4 |
280 |
72 |
4 |
Pure salt-pans
A. holosericea |
48 |
96 |
103 |
92 |
175 |
82 |
231 |
29 |
82 |
344 |
54 |
82 |
A.linarioides |
72 |
100 |
65 |
100 |
93 |
92 |
133 |
13 |
92 |
187 |
27 |
92 |
A. bivenosa |
49 |
92 |
38 |
52 |
51 |
40 |
62 |
|
24 |
66 |
|
20 |
Grassy salt-pans
A. holosericea |
34 |
96 |
70 |
96 |
136 |
88 |
155 |
15 |
88 |
229 |
39 |
88 |
A.linarioides |
75 |
88 |
86 |
88 |
114 |
88 |
185 |
19 |
88 |
250 |
41 |
88 |
A. bivenosa |
55 |
100 |
51 |
92 |
67 |
76 |
111 |
13 |
72 |
136 |
|
72 |
A. tumida |
69 |
68 |
89 |
68 |
155 |
56 |
207 |
17 |
56 |
293 |
44 |
56 |
A.sclerosperma |
48 |
80 |
52 |
76 |
78 |
76 |
138 |
15 |
76 |
139 |
|
76 |
A. pyrifolia |
44 |
52 |
40 |
52 |
72 |
52 |
117 |
7 |
52 |
148 |
|
52 |
H = height in cm; S = Section in cm2