Quantitative relationship between soil properties and adsorption of dissolved organic matter onto volcanic ash and non-volcanic ash soils

2000 ◽  
Vol 46 (3) ◽  
pp. 559-569 ◽  
Author(s):  
Kei Nambu ◽  
Koyo Yonebayashi
1973 ◽  
Vol 19 (3) ◽  
pp. 139-146 ◽  
Author(s):  
C. Bernardi ◽  
E. San Martin ◽  
E. Meléndez ◽  
S. Aomine

2021 ◽  
Vol 11 (1) ◽  
Author(s):  
Sae Katayama ◽  
Takayuki Omori ◽  
Masaki Tateno

AbstractPlants have difficulty absorbing phosphorus from volcanic ash soils owing to the adsorption of phosphorus by aluminum and iron in the soils. Thus, on volcanic ash soils, the phosphorus source for natural vegetation is expected to be organic matter, however, there is a lack of experimental evidence regarding this occurrence. Here, we studied the effect of organic matter on plant growth of some species that occur in primary successions of volcanic ash soil ecosystems, based on growth experiments and chemical analyses. We found that a large amount of inorganic phosphorus (but only a limited amount of inorganic nitrogen) is leached from fresh leaf litter of the pioneer spices Fallopia japonica at the initial stage of litter decomposition. Phosphorus from the fresh litter specifically activated the growth of subsequently invading nitrogen-fixing alder when immature volcanic soil was used for cultivation. In contrast, old organic matter in mature soil was merely a minor source of phosphorus. These results suggest that fresh litter of F. japonica is essential for growth of nitrogen-fixing alder because the litter supplies phosphorus. We consider that rapid phosphorus cycles in fresh litter-plant systems underlie the productivity of natural vegetation even in mature ecosystems established on volcanic ash soils.


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