Phosphorus Speciation in Manure-Amended Alkaline Soils

2004 ◽  
Vol 33 (4) ◽  
pp. 1521 ◽  
Author(s):  
Jeremy C. Hansen ◽  
Barbara J. Cade-Menun ◽  
Daniel G. Strawn
2015 ◽  
Vol 2015 (19) ◽  
pp. 2178-2188
Author(s):  
C. Felipe Gutierrez ◽  
Kerry Kinney ◽  
Lynn Katz

2021 ◽  
Vol 593 ◽  
pp. 125822
Author(s):  
Cheng Xu ◽  
Solomon Felix Dan ◽  
Bin Yang ◽  
Dongliang Lu ◽  
Zhenjun Kang ◽  
...  

2021 ◽  
Vol 97 (4) ◽  
Author(s):  
Lucas Dantas Lopes ◽  
Jingjie Hao ◽  
Daniel P Schachtman

ABSTRACT Soil pH is a major factor shaping bulk soil microbial communities. However, it is unclear whether the belowground microbial habitats shaped by plants (e.g. rhizosphere and root endosphere) are also affected by soil pH. We investigated this question by comparing the microbial communities associated with plants growing in neutral and strongly alkaline soils in the Sandhills, which is the largest sand dune complex in the northern hemisphere. Bulk soil, rhizosphere and root endosphere DNA were extracted from multiple plant species and analyzed using 16S rRNA amplicon sequencing. Results showed that rhizosphere, root endosphere and bulk soil microbiomes were different in the contrasting soil pH ranges. The strongest impact of plant species on the belowground microbiomes was in alkaline soils, suggesting a greater selective effect under alkali stress. Evaluation of soil chemical components showed that in addition to soil pH, cation exchange capacity also had a strong impact on shaping bulk soil microbial communities. This study extends our knowledge regarding the importance of pH to microbial ecology showing that root endosphere and rhizosphere microbial communities were also influenced by this soil component, and highlights the important role that plants play particularly in shaping the belowground microbiomes in alkaline soils.


2015 ◽  
Vol 81 ◽  
pp. 186-194 ◽  
Author(s):  
Youzhi Feng ◽  
Ruirui Chen ◽  
Junli Hu ◽  
Fei Zhao ◽  
Junhua Wang ◽  
...  

2004 ◽  
Vol 50 (7) ◽  
pp. 1159-1165 ◽  
Author(s):  
Hiroyuki Oki ◽  
Suyeon Kim ◽  
Hiromi Nakanishi ◽  
Michiko Takahashi ◽  
Hirotaka Yamaguchi ◽  
...  

1925 ◽  
Vol 15 (2) ◽  
pp. 201-221 ◽  
Author(s):  
Edward M. Crowther

A hydrogen electrode apparatus for soils is described. Similar or adjacent soils may show considerable differences inpH value, with no changes in their degrees of buffer action, as shown in titration curves with lime water. In such cases the conventional “lime requirements” are correlated with thepH values, but no such relation holds in dissimilar soils. ThepH value of a soil suspension is intimately connected with the nature and amount of the cations present. Neutral salts markedly increase the hydrogen ion concentration of both acid and slightly alkaline soils. Sodium salts, including the hydroxide, give lower hydrogenion concentrations than the corresponding potassium or calcium salts, and chlorides give lowerpH values than sulphates. The degree of buffer action (slope of titration curve) is unaffected by the addition of a neutral salt. Previous extraction of a soil with water causes a considerable increase i n thepH value of its suspensions. A number of soils showed a regular increase of about 0·1 inpH. value for twofold dilution. The “salt effect” and “dilution” effect appear to be of the same type. It is recommended that the soil-water ratio of 1:5 be generally adopted. The indicator methyl red gives erroneouspH values in turbid soil suspensions owing to the absorption of the red form, which is apparently a cation capable of undergoing “base exchange” with the soil.


Soil Research ◽  
2021 ◽  
Author(s):  
Sepideh Bagheri Novair ◽  
Hossein Mirseyed Hosseini ◽  
Hassan Etesami ◽  
Teimour Razavipour

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