Technical Note: The Vertical Distribution of Beryllium-7 Activity in Soil Profiles Determined by a Designed Device

2012 ◽  
Vol 55 (6) ◽  
pp. 2229-2236
Author(s):  
Y. Liu ◽  
B. Liu ◽  
X. Wei
2012 ◽  
Vol 610-613 ◽  
pp. 1718-1721 ◽  
Author(s):  
Hao Hu ◽  
Yu Zhao Feng ◽  
Yi Yang ◽  
Shu Guang Wang ◽  
Can Liang Li

Selected six soil profiles in a relocation paint factory, respectively sampling at 20cm, 50cm, 100cm of each profile and detecting the Pb、Zn、Cd、Ni content to research the vertical distribution and pollution characteristics. The results showed that: part of the sample profiles were in different degrees of pollution by Pb and Zn. When the heavy metals were not accumulated in the soil upper layers, the content of the heavy metals fluctuated around the background value, when the heavy metals were accumulated in the soil upper layers, the heavy metals contents down a decreasing trend from upper layers to lower layers.


2014 ◽  
Vol 65 (1) ◽  
pp. 2-9 ◽  
Author(s):  
Gábor Sándor ◽  
György Szabó

Abstract Soil profiles of the city centre of Debrecen were investigated in order to examine their properties and investigate the vertical distribution of heavy metals as a measure the anthropogenic activity. During the laboratory work the basic soil features were identified (texture, artefact content, pH, CaCO3, and amounts of organic matter). Furthermore, contents of Pb, Zn, Cu and Co in the soils were measured. Most of the metals showed a strong positive correlation with the humus content and the silt fraction. The soils of the city centre are exposed to a significant anthropogenic effect, therefore the original soil morphologies are usually difficult to identify. The soil profiles are greatly disturbed, which is traceable in the vertical distribution of certain soil features and metal contents.


2014 ◽  
Vol 962-965 ◽  
pp. 1386-1391
Author(s):  
Li Li Huo ◽  
Xian Guo Lv ◽  
Da Song Lin

To investigate how reclamation of wetlands in three different soil types impacts the vertical distribution of soil organic carbon (SOC) content in soil profiles, contents and density of soil organic carbon (SOC) in soil profiles of three types of wetland soils in wetland, soybean and paddy field in Sanjiang Plain were determined. Both soybean and paddy field were reclaimed from wetland. We observed that reclamation significantly reduced SOC content in 0-10,10-20 and 20-30 cm soil layers in meadow albic soil and meadow marsh soil, and 0-10,10-20,20-30 and 30-40 cm soil layers in peat bog soil, there were no significant difference in SOC contents in soil layers under 0-30 or 0-40 cm before and after reclamation. After reclamation, SOC density in three types of wetland soils decreased, and SOC density in soybean field were higher than that in paddy field. Either in wetlands or farm lands in the three types of wetland soils, most of the SOC storage in 0-100 cm soil layer was stored in 0-50 cm soil layer. Though wetland reclamation reduced the SOC content, it hasn’t changed the regularity of SOC vertical distribution. The relationships between SOC content and soil depth in wetlands and farm lands all could be described by exponential functions in three types of soils. The specific functions are useful to estimate and predict the regional SOC pool by models.


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