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Facskó Ferenc (szerk.) (2012): Kutatások a Nyugat-magyarországi

Facskó Ferenc (szerk.) (2012): Kutatások a Nyugat-magyarországi

Facskó Ferenc (szerk.) (2012): Kutatások a Nyugat-magyarországi

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<strong>Kutatások</strong> a <strong>Nyugat</strong>-<strong>magyarországi</strong> Egyetemen<br />

data can be mapped by GIS methods to ensure visualization of within fi eld diff erences. Soil<br />

moisture and soil electrical conductivity measurements are two relatively easy methods to<br />

determine variability of soil characteristics within fi eld.<br />

In our examination we carried out fi eld measurements with the purpose of determining soil<br />

characteristics on the investigated research fi eld where site-specifi c crop production was<br />

applied since 2001. The instruments applied were:<br />

1. A hand-held Spectrum Field Scout TDR-300 type soil moisture probe further equipped<br />

with a data logger and GPS receiver. Data transfer was via RS-232 port, the rods were 20 cm.<br />

Due to the additional equipments we could automatically collect volumetric soil moisture<br />

data with additional coordinates.<br />

2. The other instrument was a vehicle-pulled specifi c Veris 3100 Electrical Conductivity<br />

meter. This instrument was equipped with GPS-connection too. This tool underway<br />

permit of continuous measurement and with this it assures the necessary number and<br />

density of data.<br />

In the research we looked for an instrument which provides enough data for precise mapping<br />

of soil characteristics and helps to decide the boundaries of various management<br />

zones within fi eld. In the investigated fi eld we have found that soil electrical conductivity<br />

measurement provides enough data for soil characteristics measurements, furthermore<br />

correlation between soil electrical conductivity and soil moisture content was R2=0.79 in<br />

the best case (R2=0.74 in the worst), therefore in the investigated area soil moisture mapping<br />

can be carried out by means of indirect, semi-online data collection.<br />

I. VIRÁG – M. CSIBA – G. MILICS – N. SMUK – M. NEMÉNYI (2011): Evaluation of Variable Rate<br />

Fertilization Technology with the help of geospatial processing programs. 8 th European<br />

Conference on Precision Agriculture, július 11-14., pp. 352-357.<br />

Abstract – In this study a modern, nutrient replenishment plan-based Variable Rate<br />

Fertilization system (spinner disc applicator) was tested with respect to accuracy and<br />

traceability. The as-applied rates were compared to the prescribed rates. The correlation<br />

between the data set of prescription map to the data set of as-applied map was determined.<br />

In areas of the management zones, the correlation coeffi cient between the as-applied and<br />

prescribed rates was 0.87. This result was attributed to scattering that was attributed to a<br />

sluggish system response (when changing from low to high application rates). When the<br />

tramlines of the tractor were close to the neighbouring management zones, the distribution<br />

was done beyond the border of the actual management zone. This is another important fact<br />

that aff ects the accuracy of the distribution work.<br />

G. MILICS – N. SMUK – V. NAGY – J. DEÁKVÁRI – M. NEMÉNYI (<strong>2012</strong>): The role of microrelief<br />

measurements in precision agriculture. In: HARCSA Marietta (<strong>szerk</strong>.): Proceedings of<br />

the 11 th Alps Adria Scientifi c Workshop. Budapest: Akadémiai Kiadó, pp. 403-406.<br />

Abstract – Micro relief measurements are providing information on the small scale diff erences<br />

concerning relief within fi eld. Precision agriculture measurements nowadays can be<br />

carried out by sub-inch accuracy, therefore micro relief measurements have provided accurate<br />

information on the surface of our experimental research fi eld near Mosonmagyaróvár,<br />

Hungary. Within fi eld diff erences on yield permanently appears in the experimental fi eld.<br />

Yield is determined by various factors, such as nutrient replenishment, soil chemical and<br />

physical properties etc. Subsurface water resources such as soil moisture and groundwater or<br />

in other words inorganic green water and its regime have also signifi cant role on yield. Available<br />

water for the vegetation – being “blue” or “green” – therefore determines the success of<br />

plant production. Surface of the cultivated fi eld in every case has diff erences in height above<br />

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