Zakharovl defined soil structure as the nature of the fragments or clods into which the soil breaks up. The effects of cultural operations such as ploughing, cultivating, harrowing and hoeing on soil structure include the breaking up of soil into such fragments (soil aggregates) thus increasing the volume/weight and porosity. Henin2 affirmed this 'and gave a mathematical expression to such an increase. Nekrassov in 1928, 1929, Ig343-5 and Apsits in 19366 studied the effects of ploughing, cultivating, harrowing, rolling and hoeing on the capillary and noncapillary porosity of the soil (according to whether the pores are of such size that water does or does not drain under gravitational forces). They found that the major influence of tillage was on the non-capillary porosity. Doyarenko and his co-workers (Krause') have investigated the relationship of non-capillary porosity to various soil properties including aeration and nitrate formation. The oxygen content of the soil air, and nitrate formation were closely related to the non-capillary porosity, which in turn was associated with the proportion of larger aggregates in the soil. Other recent experimental results have shown rather definite relationships between non-capillary porosity and soil permeability (permeability to water under gravity), as well as the root development of crops. Saltere has specially stressed the importance of pore space in root-soil relationships. Page, Willard & McCuene studied the non-capillary porosity and compactness of soil resulting from different methods of seed-bed preparation. Ploughed plots were the most porous and mellow. Hoed and disced plots were quite compact and were the most poorly aerated. Chizhersky & Kolobovalo found that plots which had been worked with a cultivator contained 14% of aggregates smaller than 0.25 mm., while ploughed ones contained only 3%. Keen11 compared the aggregation of a soil following cultivation with a ridging plough, an ordinary plough and a rotary cultivator and found the ridging plough to be the best in this respect, a relatively small amount of disintegration of aggregates being caused by the ordinary plough. Dreibelbis & Nairls also found in the 0-4-in. layer greater pore space and better aggregation after discing than after ploughing, but in the 4-7-in. layer the relationship was reversed. Maize plants were better but thinner in the stand on disced than on the ploughed plots, but yields were not affected.Poletaefls studied the effect of tillage on soil fertility. The nitrogen nutrition of crops appeared to be related to the physical conditions of the upper soil layers at sowing time. A cloddy structure in deeper (20)(21)(22) cm.) ploughed plots caused greater leaching of nitrates in winter than did a fine structure in shallow-ploughed (12-14 cm.) plots ; mobilization of nitrates in spring was more active in the former than in the latter. Wheat grown on the shallow-ploughed plots showed signs of lack of nitrogen, but was much better on the deep-ploughed plots ; weight of grain, number of ears a...