我市低产的黄泥田,约占全市水田总面积的10％左右。主要分布在山区、丘陵的坑凼田和坡地的梯田上,主要有如下三种。 1.赤浆黄泥田(或叫洪积黄泥田)。它是山洪爆发、崩山的赤泥浆冲下河中,积覆两岸原来肥沃的耕作层而成,其特点是土层较厚、底土软,底层的有机质和养分较丰富。但赤浆的危害很大。 The low-yielding yellow muddy field in our city accounts for about 10% of the total paddy field in the city. Mainly located in the mountains, hills and pits on the slopes of Tajima, there are the following three. 1. Red mud yellow muddy fields (or called flood plot yellow mud fields). It is a flash flood, collapse of the red mud rushed down the river, the accumulation of both sides of the original fertile tillage layer, which is characterized by thick soil, bottom soil soft, the underlying organic matter and nutrient rich. However, the great harm red paste.