The Korean Journal of Mycology (한국균학회지)

The Korean Society of Mycology (한국균학회)
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Studies on Analyzing Meteorological Elements Related with Yield of Tricholoma matsutake (S. Ito et Imai) Singer.

송이(Tricholoma matsutake)생산(生産)과 관련되는 기후특성분석(氣候特性分析)

  • Kang, An-Seok (Applied mycology and Mushroom Division, Agricultural Sciences Institute R.D.A) ;
  • Cha, Dong-Yeol (Applied mycology and Mushroom Division, Agricultural Sciences Institute R.D.A.) ;
  • Kim, Yang-Sup (Applied mycology and Mushroom Division, Agricultural Sciences Institute R.D.A) ;
  • Park, Yong-Hwan (Applied mycology and Mushroom Division, Agricultural Sciences Institute R.D.A) ;
  • You, Chang-Hyun (Applied mycology and Mushroom Division, Agricultural Sciences Institute R.D.A)
  • 강안석 (농촌진흥청 농업기술연구소 균용과) ;
  • 차동열 (농촌진흥청 농업기술연구소 균용과) ;
  • 김양섭 (농촌진흥청 농업기술연구소 균용과) ;
  • 박용환 (농촌진흥청 농업기술연구소 균용과) ;
  • 유창현 (농촌진흥청 농업기술연구소 균용과)
  • Published : 1989.06.30
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Abstract

This study was carried out to obtain basic information elucidating relationship meteorological elements and yield of Tricholoma matsutake. The yields of pine mushroom in seven areas including Yangyang-gun more than 30,000 kg. Pine mushrooms were generally distributed in the red pine (Pinus densiflora) forests of East-Coast Region, Sobaek and Taebaek-Mountainous Regions, Yeongnam-Central Region and North-Central Region of Korea. Yields of pine mushroom were significant correlation with precipitation during April-October in last years, average minima temperature during July-September, rainy days during Aug. 21-Sep. 10 and precipitation during Sep. 11-30, etc. Air and soil temperature during pine mushroom yield period were 15-25 and $15-20^{\circ}C$, respectively. The first collection date of pine mushroom could be predicted by measuring the soil temperature at 5 cm depth.

송이 인공재배(人工栽培)의 기초자료(基礎資料)로 활용하고자 송이생산과 관련되는 기후특성(氣候特性)을 분석(分析)하여 다음과 같은 결과(結果)를 얻었다. 1. 10년간(年間) 연평균(年平均) 송이 수량(收量)이 30.000 kg을 상회하는 지역은 양양 등 6개 지역이 있었으며 송이생산지역은 동해안지대, 소백산지대, 영남내륙지대, 중부내륙지대의 일부지역(一部地域)에 편중되어 있음. 2. 송이생산지역의 연평균 기온은 $10{\sim}13^{\circ}C$ 범위였고 강수량은 $1000{\sim}1300mm$의 범위였으며 송이 수량(收量)과 연평균(年平均) 강수량, 연평균(年平均) 기온과의 관계(關係)는 일정한 경향이 없었음. 3. 조사지역(調査地域)(표고(標高) 110-130 m)의 송이발생기의 기온은 $15{\sim}25^{\circ}C$, 지온(地溫)은 $15{\sim}20^{\circ}C$ 범위였음. 4. 송이 수량예측 요인은 전년(前年) $4{\sim}10$월 강수량, $7{\sim}9$월 평균(平均) 최저기온(最低氣溫), $8.{\;}21{\sim}9.{\;}10$일 강수일수, $9.{\;}11{\sim}9.{\;}30$일 강수량 등이었음 5. 지온조사(地溫調査)로 송이 첫 발생시기의 예측이 가능(可能)하였음.

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