Clarification of the characteristics of soil aeration at upland field is very important for the evaluation of tillage effect. The dry density method is often applied as the index of soil aeration. However, it is very difficult to take soil samples without disturbance at field. For above reason, we made the portable apparatus for evaluation of soil aeration.
The air permeability experiments were conducted in upland field to monitor the changes of soil aeration after tillage by using portable apparatus as explained above. The experimental results show that the changes of dry density, one of the fundamental properties of soil, can be estimated and the effect of tillage can be estimated.
The results presented in this paper are summarised as follows:
(1) The changes of the dry density of soil after tillage can be estimated by using portable air permeability apparatus.
(2) If the dry density of soils is constant, the variations of soil aeration show the changes of soil moisture content and then the changes of soil moisture content can be estimated.
(3) Because of ununiform distribution of the clod size of soils tilled by a tractor, it is difficult to carry out measuring soil aeration by a direct sampling method.
(4) There is a near connection between the value of Q/(HR) and soil texture.
(5) When we obtain the both values of Q/H and soil moisture content using this apparatus at upland field, it will be possible to estimate the dry density of soils presented tillage effect at upland field.
Note Q: the discharge of air., H: aeration pressure. R: (volume fraction of gas)
3/(volume fraction of solid)
2
抄録全体を表示