Analysis of Soil Water Matric Potential Requirement for Infection of Turnip with Plasmodiophora brassicae Using Negative Pressure Water Circulation Technique
スポンサーリンク
概要
- 論文の詳細を見る
Critical soil water matric potential for infection of turnip with Plasmodiophora brassicae was examined using the negative pressure water circulation system for the regulation of the soil water matric potential of infested soils. A series of 12 gradients of soil water matric potential ranging from -3.2 kPa to -16.5 kPa was developed and maintained with fluctuations less than a few millibars (hectopascals) for 10 d after seeding. The clubroot symptoms were detected in plants in soil pots controlled at a higher soil water matric potential than -11.2 kPa. The disease was not detected in plants in soil pots controlled at a lower soil matric water potential than -12.2 kPa.
- 社団法人日本土壌肥料学会の論文
著者
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Kubota Toru
National Institute Of Agro-environmental Sciences
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Kubota T
National Inst. Agro‐environment Science Tsukuba Jpn
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Iwama Hidenori
National Institute of Agro-Environmental Sciences
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Ushiroda Tsuneo
Nagasaki Prefectural Fruit Tree Experimental Station
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Osozawa Seiko
National Institute of Agro-Environmental Sciences
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Ushiroda Tuneo
Nagasaki Prefectural Fruit Tree Experimental Station
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Osozawa S
National Inst. Agro‐environmental Sciences Tsukuba Jpn
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Kubota Toru
National Institute Of Agricultural Sciences
関連論文
- SUSCEPTIBILITY OF UNDISTURBED SOILS TO COMPRESSION AS EVALUATED FROM THE CHANGES IN THE SOIL WATER CHARACTERISTIC CURVES
- Control of Soil Water Potential Using Negative Pressure Water Circulation Technique
- Effect of Soil Aeration on the Occurrence of Clubroot Disease of Crucifers
- Analysis of Soil Water Matric Potential Requirement for Infection of Turnip with Plasmodiophora brassicae Using Negative Pressure Water Circulation Technique
- IMPROVED EVAPORIMETER FOR MEASURING POTENTIAL EVAPORATION FROM FIELD SOILS
- MEASUREMENT OF PLANT WATER USE UNDER CONTROLLED SOIL MOISTURE CONDITIONS BY THE NEGATIVE PRESSURE WATER CIRCULATION TECHNIQUE
- Subsurface Drainage in a Soil Overlying an Impermeable Layer
- Measurement of Soil Water Flux in Andisols at a Depth below a Root Zone of about 1 Meter
- ROLE OF HYDROXYALUMINIUM IONS IN THE INTERPARTICLE BONDING OF LAYERALUMINOSILICATE CLAYS