CAJ | 학술논문

在分析南亚热带丘陵赤红壤降雨入渗和产流过程基础上，依据田间实测资料，建立了丘陵赤红壤降雨入渗产流数学模型，分析了南亚热带丘陵赤红壤地表径流的动态变化特征及其影响因素。结果表明，丘陵赤红壤区，4～9月每次降雨产生的径流量变化范围为0.2～51.04mm，径流率变化范围为0.56%～47.58%，10月至次年3月一般不产生地表径流；地表径流量与降雨量拟合关系式为R0＝0.0259.Pn1.4034，径流率与土壤表层初始含水量拟合关系式为R′0=9.8788W7.7702，而降雨强度对径流量的影响要比降雨量、土壤表层初始含水量小得多。
재분석남아열대구릉적홍양강우입삼화산류과정기출상，의거전간실측자료，건립료구릉적홍양강우입삼산류수학모형，분석료남아열대구릉적홍양지표경류적동태변화특정급기영향인소。결과표명，구릉적홍양구，4～9월매차강우산생적경류량변화범위위0.2～51.04mm，경류솔변화범위위0.56%～47.58%，10월지차년3월일반불산생지표경류；지표경류량여강우량의합관계식위R0＝0.0259.Pn1.4034，경류솔여토양표층초시함수량의합관계식위R′0=9.8788W7.7702，이강우강도대경류량적영향요비강우량、토양표층초시함수량소득다。
Based on the analyses about the characteristics ofrainfall-infiltrati on-runoff of latored soil in hills of subtropics areas of south China，and on field measurement data，the mathematical model of rainfall-infiltration-runof f of latored soil in hills was made，and the dynamic characteristic of runoff an d its influencing factors of latored soil in hills of subtropics areas of south china. The results showed，in latored soil area in hills，in April to September ，the any runoff amount changed in the range of 0.2～51.04 mm，the any runoff ra te changed in the range of 0.56%～47.58%. There was no runoff amount in Octo be r to Mach of next year. The relationship between the runoff amount and rainfall amount was：R0＝0.0259.Pn1.4034，and the relationship between the runoff rate and initial soil water content in surface layer was：R′0=9.87 88W7.7702.