YUAN Shu-jie, HE Xing-tong, HE Yuan, GU Xiao-ping, PAN Ti, YU Fei
Water Saving Irrigation. 2018, (10):
83-90.
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From 2011 to 2015 in Guizhou karst region 53 daily observation of soil moisture and soil humidity automatic observatory meteorological stations observation data, applying EOF analyses the aim of 0 ~ 100 cm soil moisture spatial distribution characteristics, and relationship with possible evapotranspiration and precipitation, the results showed that: (1) 10~20cm, 30~50cm, 60~100cm spatial distribution is similar, Weining, Yanhe, Zhengan, Yinjiang and Sinan which soil moisture are smaller, Tongren, Anshun, Duyun area are larger. (2) The soil moisture in 10~50cm soil layers was relatively low in middle of July and September, middle of mid-March and mid-May, and high in mid-November and mid-January. The soil moisture in 60~100cm soil layers were not very different, and the soil moisture were 70~89% in mid-January, mid-March, mid-May, mid-July, mid-September and mid-November. (3) The first principal component and the second principal component of soil moisture field converge rapidly in 10~100cm soil layers ,and the cumulative contribution rate of variance is over 98%, the maximum value of the first main component was in northwest and southeast of Guizhou , and the minimum value was mainly in west of Guizhou. (4) The effect of potential evapotranspiration on soil moisture maybe less affected in spring. In summer, the lag time of the effect of evapotranspiration are 10 days on 10~50cm, 60~100cm are low correlation. In autumn, the lag time of the evapotranspiration in the soil moisture of 10~50cm are 10 or 20 days, with a low correlation between 60~100cm. In winter, the potential evapotranspiration may have less effect on 10~50cm soil moisture. (5) In spring, Zhenyuan’s precipitation affect the time lag for two ten-day for 10~60 cm soil humidity, Nayong’s precipitation is not obvious effect on soil moisture, Fenggang’s spring precipitation affect the lag time is when the ten-day or a meadow in 10~30 cm soil moisture; In summer, the precipitation affects the soil humidity of 10~30cm in the Zhenyuan, Nayong and Fenggang; In autumn, the effects of the precipitation on the soil moisture are not obvious. In winter, the precipitation influence lag time are10 days of 10, 20cm soil moisture in Zhenyuan and Fenggang.