Physicochemical properties of three typical purple soils with different parent materials and land uses in Sichuan Basin, China

Yi Xiao, Jia-liang Tang, Ming Kuang Wang
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引用次数: 13

Abstract

Abstract Mainly located in the Sichuan Basin, known as the ‘Land of Plenty’, purple soils (developed from purple sandstone and shale) have been long noted as highly productive in spite of their rocky texture. However, information on the physicochemical properties (including mineral properties) of purple soils remained obscure for the scientific community. For example, it is not clear what causes the purple color of the soils. In this study, eight soil profiles of the Jiufeng (JF, acidic), Shibao (SB, neutral), and Yanting (YT, calcareous) areas, representing the three most widely distributed purple soils in Sichuan Basin, were individually sampled under both cropland and forestland, and then analyzed using common chemical analysis and conventional X-ray diffraction to clarify the effects of clay mineral and anthropogenic influences on the typical soils. The results show that considerable variability of soil pH and cation-exchange capacity (CEC) exists between soil types (p < 0.05). Organic matter, total nitrogen, and CEC of forestland are higher than those of farmland, while farmland has a higher content of Olsen-P, indicating significant farming effects on nutrient status. Acidic and neutral purple soils had higher total P contents than calcareous soils while calcareous soils had higher TN, clay, and CaCO3 contents. OM, TN, TP, and Olsen-P decreased with soil depth both in farmland and forestland soil profiles. Vertical distribution of organic-bound Fe-oxides (Fep) and clay particles also shows the anthropogenic interference on farmland. Illite, chlorite, kaolinite, goethite, and trace amounts of an illite–chlorite mixing layer in clay fractions were identified for typical purple soils. Hematite was observed in the coarser fractions of the calcareous pedons, confirming that the purple soil color was mainly derived from the parent rocks. Understanding of the physicochemical properties and mineral species of soil profiles can shed light on the sustainable uses of typical purple soils in subtropical area.
四川盆地3种典型紫色土不同母质和土地利用方式的理化性质
紫色土壤主要位于四川盆地,被称为“天府之国”,紫色土壤(由紫色砂岩和页岩发展而来)长期以来一直被认为是高产的,尽管它们的岩石质地。然而,关于紫色土壤的物理化学性质(包括矿物性质)的信息对科学界来说仍然是模糊的。例如,土壤呈紫色的原因尚不清楚。本文选取四川盆地紫色土壤分布最广的九峰(酸性)、石堡(中性)和盐亭(钙质)3个地区的8个土壤剖面,分别在农田和林地条件下进行取样,利用常规化学分析和x射线衍射分析,阐明粘土矿物和人为影响对典型土壤的影响。结果表明:土壤pH值和阳离子交换容量(CEC)在不同土壤类型间存在较大差异(p < 0.05)。林地的有机质、全氮和CEC均高于农田,农田的Olsen-P含量较高,说明耕作对土壤养分状况有显著影响。酸性和中性紫色土壤总磷含量高于钙质土壤,全氮、粘粒和CaCO3含量高于钙质土壤。农田和林地土壤剖面的OM、TN、TP和Olsen-P均随土壤深度的增加而降低。有机结合的铁氧化物(Fep)和粘土颗粒的垂直分布也表现出对农田的人为干扰。在典型的紫色土壤中,鉴定出粘土组分中含有伊利石、绿泥石、高岭石、针铁矿和微量伊利石-绿泥石混合层。粗粒钙质土墩中可见赤铁矿,紫色土壤主要来源于母岩。了解土壤剖面的理化性质和矿质种类,有助于研究亚热带典型紫色土壤的可持续利用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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