The effects of biocrusts on soil parameters in a semi-arid pediment at north-eastern Iran

Q4 Earth and Planetary Sciences
A. Sepehr, Atoosa Gholamhosseinian, I. Emadodin
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引用次数: 2

Abstract

The biocrusts are organized by soil-surface communities of biota that live within or on the very top of soil surface and play an important role in soil conservation. They include lichens, mosses, fungi, cyanobacteria, eukaryotic algae, and other heterotrophic bacteria. The interaction between biocrusts and soil is very important and good awareness from that help to better manage soil specially in arid and semi-arid areas. The linkage between cyanobacteria species and soil physicochemical parameters and mineralogy in two geomorphic zones in the northeastern Iran was studied. Samples were collected in summer along a linear transect by using 50 x 50 cm quadrates for each study zone. Individual mineral soil particles were analyzed by a scanning electron microscopy (SEM). The amounts of Na, K, Ca, and Mg contents as well as EC and SOC altered significantly between two study zones. Biocrusts increased levels of organic carbon, pH, calcium carbonate, exchangeable sodium and potassium percentages. The main soil properties of SOC, CaCO3 and amount of clay changed among biocrust sand bare soils.
生物锈蚀对伊朗东北部半干旱山麓土壤参数的影响
生物结皮是由生活在土壤表层或最表层的生物群落组成的,在土壤保持中起着重要作用。它们包括地衣、苔藓、真菌、蓝藻、真核藻类和其他异养细菌。生物结皮与土壤的相互作用是非常重要的,认识到这一点有助于更好地管理土壤,特别是在干旱和半干旱地区。研究了伊朗东北部两个地貌带蓝藻种类与土壤理化参数和矿物学的联系。夏季沿线性样带收集样本,每个研究区使用50 x 50厘米的方形。用扫描电子显微镜(SEM)对矿质土壤颗粒进行了分析。两个研究区的Na、K、Ca、Mg含量以及EC和SOC变化显著。生物结壳增加了有机碳、pH值、碳酸钙、可交换钠和钾的百分比。生物结砂裸地土壤的主要性质是有机碳、碳酸钙和粘质含量发生了变化。
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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来源期刊
Revista de Geomorfologie
Revista de Geomorfologie Earth and Planetary Sciences-Computers in Earth Sciences
CiteScore
1.20
自引率
0.00%
发文量
0
审稿时长
10 weeks
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