Nitrogen mineralization of vegetable root residues and green manures as related to their (bio)chemical composition

2004 ◽  
Vol 21 (2) ◽  
pp. 161-170 ◽  
Author(s):  
Barbara Chaves ◽  
Stefaan De Neve ◽  
Georges Hofman ◽  
Pascal Boeckx ◽  
Oswald Van Cleemput
2018 ◽  
Vol 13 (1) ◽  
pp. 23
Author(s):  
Rosileyde Golçalves Siqueira Cardoso ◽  
Adriene Woods Pedrosa ◽  
Mateus Cupertino Rodrigues ◽  
Ricardo Henrique Silva Santos ◽  
Paulo Roberto Cecon ◽  
...  

The knowledge about the rate of decomposition and nitrogen mineralization of green manures provides synchronization with the higher absorption stage by the coffee tree. The rate of decomposition and nitrogen mineralization varies according to the species of green manure and with the environmental factors. The aim of the present study was to evaluate the decomposition and nitrogen mineralization of two green manures intercropped with coffee trees for three different periods. The experiment was divided into two designs for statistical analysis, one referring to the characterization of plant material (fresh mass, dry matter, dry matter content, nitrogen concentration and accumulation in the jack bean (Canavalia ensiformis) and hyacinth bean (Dolichos lablab) and another to evaluate the rate of decomposition and N mineralization of these species. The decomposition rate decreased in both species as their growth time increased in the field. The decomposition was influenced by the phenology of green manures. Nitrogen mineralization of the jack bean decreased as the growth period in the field increased and was faster than hyacinth bean only when cut at 60 days. The N mineralization was slower than mass decomposition in both species.


2021 ◽  
Vol 55 (3) ◽  
pp. 233-244
Author(s):  
Kyi Mon Mon KO ◽  
Yasumaru HIRAI ◽  
Takeo YAMAKAWA ◽  
Eiji INOUE ◽  
Takashi OKAYASU ◽  
...  

2009 ◽  
Vol 44 (3) ◽  
pp. 163-172 ◽  
Author(s):  
Mohammad Zarif SHARIFI ◽  
Shoji MATSUMURA ◽  
Tadashi HIRASAWA ◽  
Masakazu KOMATSUZAKI

2010 ◽  
Vol 41 (16) ◽  
pp. 1903-1920 ◽  
Author(s):  
A. R. Mubarak ◽  
E. A. M. Gali ◽  
A. G. Mohamed ◽  
D. Steffens ◽  
A. H. Awadelkarim

1962 ◽  
Vol 14 ◽  
pp. 149-155 ◽  
Author(s):  
E. L. Ruskol

The difference between average densities of the Moon and Earth was interpreted in the preceding report by Professor H. Urey as indicating a difference in their chemical composition. Therefore, Urey assumes the Moon's formation to have taken place far away from the Earth, under conditions differing substantially from the conditions of Earth's formation. In such a case, the Earth should have captured the Moon. As is admitted by Professor Urey himself, such a capture is a very improbable event. In addition, an assumption that the “lunar” dimensions were representative of protoplanetary bodies in the entire solar system encounters great difficulties.


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