Directory UMM :Data Elmu:jurnal:S:Sensor Review:Vol19.Issue3.1999:
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Residual calculated displacement in the soil pro®le after the single pass of the sugar beet harvester.. The centre line of the track is at the surface (depth 0) and at a
5A clari®es the different backgrounds of the working depth effect: increased covering of garden cress solely occurs in the soil ridges (due to soil level upheaval), whereas
Since analysis of variance was unable to identify signi®cant tillage system by harvest date by sample depth interaction, the data were re-analyzed using the additive main effects
problems with identical period length the difficulty increases in general with the complexity of the alphabetic relations used in the problem.. Here S is less complex than N, N is
With a high degree of profile stability (soil types numbers 1, 2 and 4), the water table depth is linked to drain depth, and the unstable layer occurs below 0.60 m.. At the
To achieve a uniform soil infestation, and higher dis- ease incidence, the inoculum of the following pathogens was incorporated into the soil by rototilling at a depth of 5 } 10
Our study of electromagnetic wave penetration into the seawater was based on wide-band synchronous measurements of ELF r VLF atmospherics on the sea surface and underwater. Two
The irrigation scheduling practices were: tensiometer-based with the tensiometers placed at 50% or 75% of the root-zone depth and irrigations started when tensiometer's readings
