Method for homogenizing soil moisture of test fields in hilly areas of middle and lower reaches of the Yangtze River
A technology of soil moisture and test fields, applied in the hilly agricultural field in the middle and lower reaches of the Yangtze River, can solve the problems of large soil moisture differences, repeated parallel differences, etc., and achieve the effect of uniform groundwater level and lower groundwater level
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[0035] 1) Investigate the movement characteristics of groundwater around the experimental field A:
[0036] From April to July, the period from April to July is when the middle and lower reaches of the Yangtze River are relatively rich in rainfall. Use soil drilling to determine the buried depth of groundwater around the test field, such as figure 1 As shown, the northern part (upper part) of the experimental field 1 is bordered by the plot A2. In this embodiment, the plot A is a mountain pond for long-term livestock and water. The plot B3 bordering the east and west sides of the test field is the plot C4. In this embodiment, the plot B and the plot C are both slope lands, which are used for long-term dry farming. Bordering on the southern part (lower part) of the test field is plot D5, and in this embodiment, plot D is a paddy field. The results are as follows: the buried depth of groundwater table at the junction of test field 1 and plot A2 is 20 cm, the buried depth of gro...
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