On examining this table it may be observed that, notwithstanding the very great variety in the proportion of ash in different plants, some general relations may be traced. A certain similarity may be observed between those belonging to the same natural family, the seeds of all the cereal grains, for instance, containing in round numbers two per cent of inorganic matters. Leguminous seeds (peas and beans) contain about three per cent, while in rape-seed, linseed, and the other oily seeds, it reaches four per cent. In the stems and straws less uniformity exists, but with the exception of a few extreme cases, the quantity of ash in general approaches pretty closely to five per cent. Still more diversified results are obtained from the entire plants; but this diversity is probably much more apparent than real, and must be, in part at least, dependent on the proportion existing between the stem and leaves, for the leaves are peculiarly rich in ash, and a leafy plant must necessarily yield a higher total percentage of ash, although, if stems and leaves were separately examined, they might not show so conspicuous a difference.
The leaves surpass all other parts of plants, in the proportion of inorganic constituents they contain, the table showing that in some instances, as in the maple and Jerusalem artichoke, they exceed one-fourth of the whole weight of the dry matter. In other leaves, and more especially in those of the coniferæ, the proportion is much smaller. Taking the average of all the analyses hitherto made, it appears that leaves contain about thirteen per cent of ash, but the variations on either side are so large that little value is to be attached to it except as an indication of the general abundance of mineral matters.
In roots and tubers the variations are less, and all, except the potato and the turnip, contain about seven per cent of ash.
The smallest proportion of mineral matter is found in wood. In one case only does the proportion reach five per cent, while the average scarcely exceeds one, and in the fir the quantity amounts to no more than one six-hundredth of the dry matter. In the bark the quantity is much larger, and may be stated at seven per cent.
The general proportion of ash found in different parts of plants is given in round numbers in the subjoined table:—
| Wood | 1 |
| Seeds | 3 |
| Stems and straws | 5 |
| Roots and tubers | 7 |
| Bark | 7 |
| Leaves | 13 |
The differences in the quantity of ash contained in different parts of plants are obviously intended to serve a useful purpose, and it is interesting to observe that the wood which is destined to remain for a long period, sometimes for several centuries, a part of the plant, contains the smallest proportion, and it is not improbable that what it does contain is really due, not to the actual woody matter itself, but to the sap which permeates its vessels. By this arrangement but a small proportion of these important mineral matters, which the soil supplies in very limited quantity, is locked up within the plant, and those which are absorbed, after circulating through it, and fulfilling their allotted functions, are accumulated in the leaves, and annually returned to the soil.
The different proportions of mineral matters contained in the individual organs of plants is most strikingly illustrated when parallel experiments are made on the same species; but the number of instances in which a sufficiently extensive series of analyses has been made to show this, is comparatively limited, and is confined to the oat, the orange-tree, and the horse chesnut—each of which has formed the subject of a very elaborate investigation. The following table gives the results obtained on the oat:—
| Hopetoun Oats, Northumberland. | Hopetoun Oats, Fifeshire. | Potato Oats, Northumberland. | Black Oats, Edinburgh. | Sandy Oats, Fifeshire. | Mean. | |
| Grain | 2·14 | 1·81 | 2·22 | 2·11 | 1·76 | 2·00 |
| Husk | 6·47 | 6·03 | 6·99 | 8·24 | 6·03 | 6·75 |
| Chaff | 16·53 | 17·23 | 15·59 | 19·19 | 18·97 | 16·06 |
| Leaves | 8·44 | 7·19 | 14·59 | 10·29 | 15·92 | 10·88 |
| Upper part of straw | 4·95 | 5·44 | 9·22 | 8·25 | 11·0 | 7·77 |
| Middle part of straw | 6·11 | 5·23 | 7·41 | 6·53 | 9·01 | 6·66 |
| Lower part of straw | 5·33 | 5·18 | 9·76 | 7·11 | 7·30 | 6·93 |