Topography influences primary soil basic properties and bacterial community changes: evidence from volcanic field of 300 years, northeast China

IF 5.4 1区 农林科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Jing Liu , Honghu Liu , Baoyuan Liu , Yunge Zhao
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Abstract

Topographic factor has crucial impacts on the rock weathering and soil development. However, few studies have concerned the influence of topographic features on the spatial distribution of soil properties at the initial soil development stage. To explore this, soil samples were collected from 10 soil profiles on scoria cone, and from 18 quadrats on lava plateau along the NNW-SSE toposequence in Laoheishan volcanic field of 300 years, northeast China. Basic indicators such as soil thickness, mechanical composition, organic carbon and total nitrogen and their mineral-associated fractions were measured, and soil bacterial community were identified by 16S rRNA amplicon sequencing method, and their relationships with topography were determined by Spearman rank correlation and pathway analysis. Compared to lava plateau with weak-weathered binary structure thinner than 13 cm, scoria slopes developed typical soil profiles ranging from 7 to 30 cm, with lower clay and silt fraction (e.g. topsoil: 73.75 % vs. 35.57 %), which positively associated with carbon and nitrogen contents (e.g. topsoil organic carbon: 72.32 vs. 38.59 g kg−1). Northern slope had finer particles, richer carbon and nutrients than southern slope, with organic carbon peaked around middle slope position with 116.76 and 34.70 g kg−1, respectively. Northern lava plateau showed distinctive differences from other topographic sites in bacterial phyla structure and functional groups. The total explanation of carbon and nitrogen contents and their stoichiometric ratio values to bacterial phyla structure accounted for 41 %. In conclusion, topography influenced clay fraction gathering, which in turn affected the accumulation of carbon and nutrients. Ultimately, it regulated shifts in bacterial diversity during the initial soil development process. This study will improve understanding of topographic-driven mechanisms of initial soil development and soil characteristics spatial patterns.
地形对原始土壤基本性质和细菌群落变化的影响——来自东北300年火山场的证据
地形因素对岩石风化和土壤发育具有重要影响。然而,很少有研究关注土壤发育初期地形特征对土壤性质空间分布的影响。为此,在东北老黑山300年火山岩带NNW-SSE地形层序的熔岩高原上采集了10个土壤剖面和18个样方。测定土壤厚度、机械组成、有机碳和全氮及其矿物相关组分等基本指标,采用16S rRNA扩增子测序法鉴定土壤细菌群落,采用Spearman秩相关和通径分析确定其与地形的关系。与薄于13 cm的弱风化二元结构的熔岩高原相比,矿渣坡发育了典型的7 ~ 30 cm的土壤剖面,粘土和粉土含量较低(表层土:73.75%比35.57%),与碳氮含量呈正相关(表层土有机碳:72.32比38.59 g kg−1)。北坡颗粒更细,碳和营养物质更丰富,有机碳在中坡附近达到峰值,分别为116.76和34.70 g kg−1。北部熔岩高原在细菌门结构和功能类群上与其他地形站点有明显差异。碳氮含量及其化学计量比值对细菌门结构的总解释占41%。综上所述,地形影响了粘土组分的聚集,进而影响了碳和养分的积累。最终,它调节了土壤初始发育过程中细菌多样性的变化。该研究将有助于加深对土壤初始发育的地形驱动机制和土壤特征空间格局的认识。
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来源期刊
Catena
Catena 环境科学-地球科学综合
CiteScore
10.50
自引率
9.70%
发文量
816
审稿时长
54 days
期刊介绍: Catena publishes papers describing original field and laboratory investigations and reviews on geoecology and landscape evolution with emphasis on interdisciplinary aspects of soil science, hydrology and geomorphology. It aims to disseminate new knowledge and foster better understanding of the physical environment, of evolutionary sequences that have resulted in past and current landscapes, and of the natural processes that are likely to determine the fate of our terrestrial environment. Papers within any one of the above topics are welcome provided they are of sufficiently wide interest and relevance.
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