CAJ | 학술논문

于2012年5月中旬至10月初，在大兴安岭干旱阳坡的蒙古栎林内，选择不同的坡向和坡位设置观测样地定点测定土壤温度、空气温湿度和土壤含水量。分析结果表明：不同坡向土壤温度由大到小为南坡、西南坡、东南坡，气温由大到小为西南坡、南坡、东南坡，空气湿度和土壤含水量由大到小均为东南坡、西南坡、南坡；南坡空气和土壤温度由大到小为坡上、坡下，土壤含水量坡下大于坡上含水量，空气湿度坡上大于坡下湿度；空气和土壤温湿度受空间位置和季节分布影响差异较大，不同坡向和坡位土壤温湿度差异明显，不同季节空气温湿度波动较大。
우2012년5월중순지10월초，재대흥안령간한양파적몽고력림내，선택불동적파향화파위설치관측양지정점측정토양온도、공기온습도화토양함수량。분석결과표명：불동파향토양온도유대도소위남파、서남파、동남파，기온유대도소위서남파、남파、동남파，공기습도화토양함수량유대도소균위동남파、서남파、남파；남파공기화토양온도유대도소위파상、파하，토양함수량파하대우파상함수량，공기습도파상대우파하습도；공기화토양온습도수공간위치화계절분포영향차이교대，불동파향화파위토양온습도차이명현，불동계절공기온습도파동교대。
For the characteristic of the arid sunny-slope Mongolian oak forests temperature and humidity in Daxing ’ an Mountains, we selected different slope aspect and slope position set observation sample plots and fixed point to measure soil temperature, air temperature, humidity and soil moisture from mid May to early October in 2012.The soil temperature of different slope aspect was in the descending order of southern slope, southwest slope and southeast slope, air temperature was in the descending order of southwest slope, south slope, and southeast slope, and air humidity and soil moisture con-tent was in the descending order of southeast slope, southwest slope and south slope.The southern slope air and soil tem-perature were in the descending order of upper slope, lower slope, soil moisture was in the descending order of lower slope and upper slope, air humidity was in the descending order of upper slope and lower slope.Air and soil temperature and hu-midity were affected significantly by spatial distribution and seasonal differences, and soil temperature and humidity were with a clear difference in different slope direction and slope position with large fluctuation in different seasons.