
Reviews.
The Correlation of Iron Starvation in Ruminants with the Physical Features of the Country.
R. E. R. Grimmett, M. Sc. (Analyst, Department of Agriculture), in the New Zealand Journal of Agriculture, vol. 34. No. 5, pages 289 to 294, May, 1927), after a year's residence at Rotorua spent in a continuous study of the field conditions in the “bush sick” area, has made a contribution to the knowledge of this remarkable deficiency disease in ruminants, now officially known as “Iron Starvation” (see Transactions New Zealand Institute, vol. 55, 1924, pages 720 to 723).
Grimmett considers that on typical “bush sick” farms, five con-ditions will always be present, viz.:—
| (1) |
The surface soil is sufficiently elevated above the permanent soil water-table to prevent the rise by capillary attraction of ground water from the water-table to the surface soil. |
| (2) |
The surface soil is always of very coarse texture, being coarser than what is known in soil science as a sandy loam; that is, a soil on which the disease occurs always contains less than five per cent. on clay, or does not contain an amount of decayed vegetable matter (“humus”) which would in its action be equivalent to five per cent. of clay. |
| (3) |
The subsoil and substrata are always fairly pervious to water. |
| (4) |
The annual rainfall is fairly heavy. |
| (5) |
The surface topography is that of an approximately horizon-tal, undissected type of country, and, which follows really as a corollary, there is an absence of seepage areas. |
The author explains that the elevated, highly oxygenated porous soil is in an ideal condition for losing by leaching when subjected to a heavy rainfall, the plant foods soluble in water, or for losing by oxidation such compounds as those of ferrous iron, which are taken up by the plant in the reduced state, being unavailable in the more highly oxidised state, e. g., ferric iron.
If five per cent. of clay or an equivalent amount of organic matter be present, the excessive loss of soil water (carrying its load of plant food) by drainage is retarded, and the oxidation is hindered. Also, if near the surface there exists a semipervious substratum such as an alluvial silt layer or a pan, the downward flow of water is checked, encouraging an increase in the run-off and the consequent develop-ment of springs and swamps, conditions favouring the solubility or availability of iron.
With a porous soil, the heavier the rainfall the greater will be the leaching. The disease usually appears to be most prevalent in very

wet seasons. If the topography be one of very sharp ridges and valleys, or of steep slopes, leaching will be modified in two directions: (1) The ratio of soakage to run-off will be lowered, less water sinking into the soil, or sinking through in more restricted areas; (2) The water which does soak through and leach the higher levels will often seep out again, bearing its load of soluble plant food to the plants at lower levels. In such a case where seep-age springs and creeks are bordered by swampy pasture, even in rela-tively small areas, stock having access to the pasture do not develop iron starvation. If the springs are localized, or the streams sharply entrenched so as to leave no room for wet seepage or unaerated soil pasture, the incidence of the disease is but little affected.
Some examples of how the various factors operate together to produce the different degrees of iron starvation actually observed may be given. On portions of the Kapakapa Road, and at Te Pu and Ngawaro (Rotorua County), perhaps the most acute degree of the disease is manifest. All the factors enumerated are present (see N. Z. Journal of Agriculture for January, 1925, p. 2). The situation is relatively high above permanent water, the soil is a fine gravelly sand or a coarse sand, the substrata are pervious, consisting of sands and tuffs, the topography is that of a plateau, or is gently valleyed and hummocky, and the rainfall is heavy, resulting in a leached soil and an absence of springs and seepage areas.
At Mamaku, the chief factor modified is the texture of the soil, which is a sandy silt, rather fine and less pervious than the soils mentioned above. Sickness is less acute, but still severe (see N. Z. Journ. Agr., vol. 29, November, 1924, page 324).
At Oturoa the soil is finer, being a sandy loam, and the altitude less. Springs and creeks occur. Sickness is absent or of a light degree.
Farms at the blind ends of Kapakapa and Kaharoa Roads, and in parts of Ngawaro and on the northern side of Rotoiti Lake, are either free, or exhibit only a mild form of the trouble. The soils and other factors are practically the same here as in other parts of the Kaharoa and Ngawaro districts, with the exception of topography, which is usually found to be well dissected, with springs, swamps and seepage areas, and streams.
At Hamurana, and generally on the low-lying land bordering the lakes, not only is no sickness found, but sick animals from other areas recover quite rapidly. The soils vary from sandy silts to fine gravelly sands, and the only modified factor appears to be the altitude above permanent water, which is often but a few feet, or even inches, and in winter some land may be submerged. Springs, seepage areas, and swamps, occur under the hills and higher terraces to the lake edge.
The higher terrace lands, which are intermediate in altitude and position between the low-lying healthy lakeside soils (as at Rotorua) and the high sick soils (as at Mamaku) are also found to be inter-mediate as regards the incidence of sickness.

At Te Ngae, Okareka, and other places where sufficient thickness of the 1886 Rotomahana eruption mud remains to form a new surface soil, no sickness either in cattle or sheep occurs, even on the high flattish land with a coarse pumice subsoil. Apparently the fact that the soil is a sandy loam with over five per cent. of clay is largely responsible for this immunity. In addition, little time has elapsed for leaching to occur; iron is present in considerable quantity, and, judging by the colour (bluish grey), is not greatly oxidized.
The road from Rotorua to Atiamuri passes through a large area of country the surface soil of which, generally of coarse texture,* is derived from subaerially deposited pumice, as in the remainder of the district. This deposit varies in depth from 1ft. to 4ft., the substrata consisting of alluvial deposits varying from coarse water-worn gravel to well-sorted sands, silts, and clays of a compact and fairly imper-vious nature. Excessive leaching of the top-soil seems thereby to have been prevented, and the run-off of rain-water and the formation of springs, streams, swamps, and seepage areas greatly increased. Thus, despite the presence of other factors favouring iron starvation, this does not appear to have been experienced where farming on this area has been carried out.
Remedial Treatment for Iron-Starvation.
Remedial treatment may be sought in three different directions:
(1) By supplying iron to the animal direct; (2) by supplying iron to the pasture direct, either through the leaves or through the roots; (3) by sufficiently modifying any of the factors contributing to the resent unavailability of the iron in the soil.
1. Feeding of iron salts to the animal, particularly iron ammonium citrate as originally introduced by Mr. Aston, is meeting with very general success, but obviously has limitations. Its greatest usefulness is found in the case of dairy cows, where the supplying of a regular ration is a fairly simple operation.
2. The supplying of iron to the pasture is being experimented with, serrous sulphate being used both as a soil top-dressing and as a weak spray applied to the green growth. So long as the conditions which contribute to the unavailability of the natural iron in the soil remain unaltered, it seems unlikely that the application of soluble iron salts to the soil will be of more than temporary benefit, the application needing to be renewed at fairly frequent intervals.
3. Modification of contributory factors:—
(a) The attitude of the surface soil above the permanent water-table can scarcely be modified by human agency.
[Footnote] * Since the above was written, some of these topsoils have been found by analysis in this Laboratory to be much finer (belonging to the type called silts) than most pumice soils, a fact which may somewhat modify the opinions in this paragraph.

(b) Texture of the soil: Of the two possible ways in which this could be amended—namely, by increasing either the clay or the humus —the latter is alone likely to be practicable. As recommended by Aston (N. Z. Jour. Agr. for August, 1912, p. 122, May, 1912, p. 377, and August, 1924, p. 90) of all avenues open to the farmer, green manuring appears to be the most immediately promising for diminish-ing the trouble. By this means a closer and less pervious structure is given to the soil, the store of material capable of reducing the insoluble ferric to the more soluble ferrous form of iron salts is added to, and the general fertility of the soil increased. Somewhat the same end is attained by the establishment of a close and well-compacted turf of approved pasture plants; and it is probably for this reason that with ageing of the pasture iron starvation generally diminishes, while reploughing and resowing is said frequently to produce a tem-porary return to a more acute stage. Rolling, trampling by stock, or other means of consolidation also should be beneficial, both by decreasing the air space in the soil and by tending to restrict soakage and leaching.
(c) Neither the nature of the substrata nor (d) the amount of rainfall, nor (e) the general nature of the topography are factors amenable to practical control.
(f) Building up of the store of iron in the soil should be aimed at, even though much of it may be rendered for the time being practically unavailable. Especially is the use of basic slag (or, better still, of a slag super mixture), or a mixture of iron sulphate with superphosphate likely to be beneficial, as the phosphate encourages root growth, and by bringing the roots into close association with the iron, may tend towards a greater degree of absorption. Mr. Aston has recently recommended the trial of “ferrous superphosphate,” a mixture of superphosphate, sulphate of iron (hydrated ferrous sul-phate), and hydrated sulphate of lime (gypsum). This mixture contains 12 per cent. of iron sulphate (see Griffiths's Treatise on Manures, 1892, p. 283, Whittaker, London).
(g) The utilization of any areas of seepage, swamp, or river flat existing on “bush-sick” farms should be zealously aimed at, pasture grown under such conditions being usually rich in iron and an anti-dote to the sickness.
To make his paper complete, the reviewer here summarizes some of the remedial treatment recommended or adopted at the Government Farm, Mamaku, as the result of many years' experience of officers who have assisted in this investigation, together with some recommenda-tions of his own. This may be compared with the last authoritative advice published by the Department (see N. Z. Journ. Agr., vol. 33, p. 98):—
“(1) Farm more highly; get the plough in; compact the soil; grow plenty of winter feed, and save plenty of hay; subdivide into smaller paddocks, and keep the pasture eaten short. Topdress with phosphate—preferably containing iron, or in conjunction with iron sulphate—as frequently as is the practice to topdress in the Waikato. Treat the stock well, especially in the matter of water-supply.

“(2) Use molasses freely in the feeding, especially in the rearing of young stock. Regard molasses as a preventive, but not as a cure.
“(3) When an animal shows signs of going back in condition owing to iron hunger, give iron ammonium citrate as supplied by the Mamaku Demonstration Farm, and by the Stock Inspectors at Roto-rua and Tauranga, at a cost price to bonafide farmers.
“(4) Buy any stock required from districts remote from the affected pumice land, and under conditions which ensure that the animals are free from disease or parasitic infection. Lack of the mineral elements is known to predispose an animal to other diseases and ailments, which, when introduced on to a farm on sick country, run a rapid course in the stock.”
The use of molasses (first introduced to the Department by Mr. Norman Callister, farmer, Te Puke), is still advocated by the Depart-ment as in the use of winter feed (hay, roots, etc.). Also new stock brought on to the farm should comply with condition No. 4.
The value of Grimmett's contribution lies in his production of further evidence towards the theory that “bush sickness” is iron starvation; his testimony to the value of green manuring, or of rein-forcing the organic matter (humus) of the soil; his support to the explanation previously advanced (N. Z. Journ. Agri., December, 1924, p. 370) by which it is sought to explain why the disease occurs on some lands and not on others nearby of similar mechanical composition. But he does more than endorse theories long held, for he has by the careful examination of the physiography of many examples of sick and healthy lands occurring in close proximity, been able to distin-guish the surface features which characterize a typical “bush-sick” farm, from those features which characterize healthy country in such a way that typically bad country may be recognized from typically good country.
B. C. Aston.
