Method for improving soil fertility of mountain tea garden
A tea garden and soil fertility technology, applied in the field of tea planting, can solve the problems of soil porosity reduction, waste of resources, premature decline of tree vigor and other problems, and achieve the effect of promoting the increase of organic matter, improving supply capacity, and improving soil moisture
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Embodiment 1
[0019] In Peiyuan Village, Xiuning County, Huangshan City, the main green tea producing area in Anhui Province, the soil of the tea garden is yellow-red soil developed from phyllite and sand shale, with a pH value of about 4.51. The tea garden for testing was built in the spring of 1984. The variety is the Xiuning local group species (commonly known as the cowhide species), and the tea trees are planted in three densely planted ways. Before the test, the tea tree growth, landscape and management level of the tea garden were average, the level of fertilization was low (approximately 20 kg of pure nitrogen per mu), and the yield was low (the annual output of dry tea per mu was about 50 kg).
[0020] Set up a test area (area of 2 mu) and a control area (area of 2 mu) in the tea garden.
[0021] Perform the following operations in the test area:
[0022] According to the actual planting and arrangement of mountain tea gardens, the tea garden is cultivated every other year wit...
Embodiment 2
[0027] This test is located in the tea garden of Hongtong tea factory test base in Huizhou District, Huangshan City, Anhui Province, and the test setting process is the same as in Example 1
[0028] Result of the test: the soil organic matter, total nitrogen, available potassium, and available phosphorus contents of the tea garden soil treated according to the present invention were 22.4g / kg, 1.15g / kg, 63.6mg / kg, and 41.2mg / kg, which were higher than those in the control area tea garden respectively. The soil has increased by 22.9%, 34.5%, 31.8%, and 52.5%; compared with the tea garden soil in the control area: compared with the soil capillary water holding capacity, the soil capillary water holding capacity has increased by 3.7% to 6.2%, and the soil bulk density has decreased by an average of 0.05g / cm 3 ~0.11g / cm 3 , soil porosity increased by 2.0% to 2.5%, surface runoff decreased by 4.9% to 8.6%, and annual dry tea production increased by 15.4%.
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