Total contents and mobile fractions of chemical elements within a soil toposequence in the south-east of the Valdai Hills, Russia
收藏Mendeley Data2021-04-26 更新2026-04-09 收录
下载链接:
https://data.mendeley.com/datasets/j6kwvh9x43
下载链接
链接失效反馈官方服务:
资源简介:
Samples were taken from September 2016 to May 2018 in the southern part of the Central Forest Reserve (Russia) within a catena with c Retisols under coniferous-deciduous forest (Tília cordáta, Pícea ábies, Ácer platanoídes) on loess-like loams underlain by carbonate moraine deposits. Soil properties were analysed at the MSU (Lomonosov Moscow State University) Faculty of Geography: - pH value was measured in suspension (static conditions) using a pH-meter "Expert-рН" (Russia); - total organic carbon (TOC) content was determined in 120 samples using titrimetric method with phenylanthranilic acid (Reeuwijk, 2002); - the particle-size distribution was analyzed using laser diffraction technique and an ‘Analizeter 22’ equipment (Germany). Particle-size classes (Russian system): G1 – clay (<1 μm), G2 – very fine silt (5–1), G3 – medium silt (10–5), G4 – сoarse silt (50–10), G5 –fine sand (250–50), G6 – medium sand (500–250). Total content of chemical elements (ChEs) and mobile fractions was measured at the VIMS (N. M. Fedorovskii All-Russia Institute of Mineral Raw Materials) using an Elan-6100 ICP-MS System and an Optima-4300 DV ICP-AES System. The studied fractions of the ChEs: - F1 (exchangeable) was extracted with NH4Ac (ammonium acetate buffer) - F2 (bound within organo-mineral complexes) was extracted with with 1% EDTA (ethylenediaminetetraacetic acid) - F3 (bound with Fe and Mn hydroxides) was extracted with 1M HNO3 - F4 (residual fraction) - the difference between the total content of elements and the content of mobile forms.
本数据集的样本采集于2016年9月至2018年5月,采自俄罗斯中部森林保护区南部的一段土链(catena),该土链上发育针阔混交林(心叶椴*Tília cordáta*、云杉*Pícea ábies*、挪威槭*Ácer platanoídes*),林下为黄土状壤土,下伏碳酸盐冰碛沉积物,且以粘磐土(Retisols)为主要土壤类型。土壤属性分析在莫斯科国立罗蒙诺索夫大学(Lomonosov Moscow State University, MSU)地理学院完成,具体测定项目与方法如下:
1. pH值采用静态悬液法,使用俄罗斯产"Expert-pH"pH计进行测定;
2. 总有机碳(total organic carbon, TOC)含量采用苯基邻氨基苯甲酸滴定法(Reeuwijk, 2002)对120份样本进行测定;
3. 粒度分布采用激光衍射技术,搭配德国产"Analizeter 22"仪器开展分析。
本次研究采用俄罗斯标准土壤粒度分级体系,具体分级标准如下:
G1 – 黏粒(<1 μm),G2 – 极细粉粒(5–1 μm),G3 – 中粉粒(10–5 μm),G4 – 粗粉粒(50–10 μm),G5 – 细砂粒(250–50 μm),G6 – 中砂粒(500–250 μm)。
化学元素(chemical elements, ChEs)总量及有效态组分的测定工作在全俄N. M. 费多罗夫斯基矿物原料研究所(N. M. Fedorovskii All-Russia Institute of Mineral Raw Materials, VIMS)完成,所用仪器为Elan-6100型电感耦合等离子体质谱(ICP-MS)系统与Optima-4300 DV型电感耦合等离子体原子发射光谱(ICP-AES)系统。
本次研究针对以下化学元素组分开展分析:
- F1(可交换态):采用醋酸铵缓冲液(ammonium acetate buffer, NH₄Ac)进行提取;
- F2(有机-矿质复合体结合态):采用1%乙二胺四乙酸(ethylenediaminetetraacetic acid, EDTA)溶液进行提取;
- F3(铁锰氢氧化物结合态):采用1mol/L硝酸(HNO₃)溶液进行提取;
- F4(残渣态):为化学元素总量与有效态组分含量的差值。
创建时间:
2021-04-26



