It is generally accepted that the population of subterranean micro-organisms having a direct concern with the nitrogen metabolism of plants grown in the sand is rather scarce as compared with those in ordinary farm soil, and the ammonification as well as the nitrification processes in sand, in consequence, has been considered to be generally small. For raising of plants in sand, therefore, it is quite necessary to make clear the nitrification processes which take place in the sand, and also to get more advanced knowledge concerning the fertilizing method of nitrogen in the Suna Saibai (a type of sand culture). In this connection, the author carried out studies on the nitrogen metabolism in the Suna Saibai, e.g., the influence of water content in the sand, of the concentration of nitrogen in the sand, and the effect of applying clay (bentonite) to the sand under 30°C constant temperature condition.1. The ammonification and the nitrification in the sand took place quite sufficieutly. The nitrification of urea was detected 4 days after application.2. The effect of the water content of the sand upon the ammonification was relatively small, and when the concentration of applied nitrogen was 125 or 333ppm, the ammonification at the 4th day attained ca. 65 to 85% of total nitrogen.3. When the concentration of applied nitrogen was 125ppm, the nitrification was not influenced at all by the water content of the medium. The rate of nitrification per the total nitrogen attained ca. 95 to 100% at the 20th day. When it was 333 ppm the effect of the water content became detectable only after 12 days. The nitrification occurred earliest in the plot with a water content of 30ml per 150g of the sand, next in the plot of 20ml, and finally those of both 10 and 40ml. Namely, in the plots of 10, 20, 30 and 40ml water content, the nitrification attained to 35, 60, 70 or 40% on the 12th day and 60, 90, 95 or 60% of total nitrogen, respectively on the 20th day.4. When the water content was the most favorable (30ml of water per 150g of sand, i.e., ca. 60% of the maximum water holding capacity), the ammonification and the nitrification were remarkably influenced by the concentration of applied nitrogen, and the higher the concentration, the later these occurred. The rates of ammonification at each level of nitrogen concentration (125, 250, 500 and 1, 000ppm) were 80, 65, 50 and 35% on the 4th day, and the nitrification on the 16th day was 100, 95, 70 and 50% respectively.5. The added bentonite was refinitely effective in each of three different kinds of nitrogen levels, (250, 500 and 1, 000ppm), inducing good effect on the ammonification and the nitrification. In the case of 250ppm of nitrogen and 30ml water per 150g of sand, the effect of supplying bentonite at four different levels (0, 0.5, 1.5 and 4.5g) could be noticed on the 12th day after application when the population of soil organisms was considered to become sufficiently large. The nitrification rates on the 16th day were 45, 80 and 100%, respective to the increased application of bentonite upon pH was as follows: When 4.5g was added, pH was 7.2 at about 60% nitrification (on the 16th day). On the other hand, when the bentonite was not added at all, the pH value remained very low, being 4.6 at about 45% nitrification (on the 16th day). Thus the effect upon the ammonification, the nitrification and upon pH caused by the addition of bentonite was quite evident.
Read full abstract