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野果林土是在我国珍存的野苹果、野胡桃和野杏等温带半干旱地区落叶阔叶林下发育的森林土壤类型。呈岛状或小块状分布在伊犁谷地两侧的深沟峡谷海拔１０００～１７００ｍ一带。野果林上有其自身的发生发展规律和时空位置。腐殖化过程较强，钙积化过程明显，粘化过程微弱，剖面分异显著。野果林土表疏松含水较多，养分表聚性强，盐基饱和度＞８１％，ＳｕＯ２、Ａｌ２Ｏ３含量较高，并略有移动。
The forest soil is the type of forest soil developed under the deciduous broad-leaved forest in temperate semi-arid areas such as wild apple, wild walnut and wild apricot stored in our country. The island-shaped or small-shaped distribution in the Ili Valley on both sides of the deep gully valley at an elevation of 1000 ~ 1700m area. Wild fruit forest has its own rules of occurrence and development and space-time position. The humification process is strong, the process of calcium accretion is obvious, the sticking process is weak, and the profile is distinctly different. Wild forest soil loose loose more water, nutrients table poly, base saturation> 81%, SuO2, Al2O3 content is higher, and a slight movement.