메뉴 건너뛰기
.. 내서재 .. 알림
소속 기관/학교 인증
인증하면 논문, 학술자료 등을  무료로 열람할 수 있어요.
한국대학교, 누리자동차, 시립도서관 등 나의 기관을 확인해보세요
(국내 대학 90% 이상 구독 중)
로그인 회원가입 고객센터 ENG
주제분류

추천
검색
질문

논문 기본 정보

자료유형
학술저널
저자정보
Mehmet Aydin (Kangwon National University) Yeong-Sang Jung (Kangwon National University) Hyun-Il Lee (Kangwon National University) Kyung-Dae Kim (Kangwon National University) Jae E Yang (Kangwon National University)
저널정보
한국토양비료학회 한국토양비료학회지 한국토양비료학회지 제45권 제1호
발행연도
2012.2
수록면
1 - 8 (8page)

이용수

표지
📌
연구주제
📖
연구배경
🔬
연구방법
🏆
연구결과
AI에게 요청하기
추천
검색
질문

이 논문의 연구 히스토리 (2)

초록· 키워드

오류제보하기
The thermal properties including volumetric heat capacity, thermal conductivity, thermal diffusivity, and diurnal and annual damping depths of 10 representative soil series of Korea were calculated using some measurable soil parameters based on the Taxonomical Classification of Korean Soils. The heat capacity of soils demonstrated a linear function of water content and ranged from 0.2 to 0.8 cal cm<SUP>-3</SUP> ℃<SUB>-1</SUB> for dry and saturated medium-textured soil, respectively. A small increase in water content of the dry soils caused a sharp increase in thermal conductivity. Upon further increases in water content, the conductivity increased ever more gradually and reached to a maximum value at saturation. The transition from low to high thermal conductivity occurred at low water content in the soils with coarse texture, and at high water content in the other textures. Thermal conductivity ranged between 0.37×10<SUP>-3</SUP> cal cm<SUP>-1</SUP> s<SUB>-1</SUB> ℃<SUB>-1</SUB> for dry (medium-textured) soil and 4.01×10<SUP>-3</SUP> cal cm<SUP>-1</SUP> s<SUB>-1</SUB> ℃<SUB>-1</SUB> for saturated (medium/coarse-textured) soil. The thermal diffusivity initially increased rapidly with small increases in water content of the soils, and then decreased upon further increases in the soil-water content. Even in an extreme soil with the highest diffusivity value (1.1×10<SUP>-2</SUP> cm<SUP>2</SUP> s<SUP>-1</SUP>), the daily temperature variation did not penetrate below 70 cm soil depth and the yearly variation not below 13.4 m as four times of damping depths.

목차

Abstract
Introduction
Materials and Methods
Results and Discussion
Conclusions
References

참고문헌 (37)

참고문헌 신청

이 논문의 저자 정보

이 논문과 함께 이용한 논문

최근 본 자료

전체보기

댓글(0)

0

UCI(KEPA) : I410-ECN-0101-2014-521-000792946