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据舟山群岛北部丘陵土壤的野外考察及所采14个代表剖面分析资料,多数土壤剖面具有黄红壤亚类的特征,包括土壤颜色、反应、交换性阳离子组成,EGEC及其主导成土作用高蛉化等,但与此相反,大部分剖面的盐基饱和度都很高。因此建议把它们归属于新立的海岛棕红泥土属,而与其他黄红壤相区别,并把它作为黄红壤亚类与黄棕壤土类之间的过渡土壤,另有少数土壤剖面也具有某些黄棕壤的特性,但由于缺乏足够的论据,它们是否归属于黄棕壤土类,有待进一步研究。
According to the field investigation of the hilly soil in the northern Zhoushan Archipelago and analysis of 14 representative sections collected, most of the soil profiles have the characteristics of yellow-red soil sub-classes, including soil color, reaction, exchangeable cation composition, EGEC and its dominant soil-forming action In contrast, most sections have high base saturation. Therefore, it is suggested that they be attributed to the newly established genus of red muddy red soils and to be distinguished from other yellowish red soils as transitional soils between yellow-red soils and yellow-brown soils, with a few other soil profiles Some yellow-brown soil characteristics, but due to the lack of sufficient evidence, whether they belong to yellow brown soil, pending further study.