scholarly journals Soil nitrogen supply and nitrogen uptake for local rice grown in unfertilized acid sulfate soil in South Kalimantan

Tropics ◽  
2006 ◽  
Vol 15 (4) ◽  
pp. 349-354
Author(s):  
Erry PURNOMO ◽  
Toshihiro HASEGAWA ◽  
Yasuyuki HASHIDOKO ◽  
Mitsuru OSAKI
Ecology ◽  
2004 ◽  
Vol 85 (4) ◽  
pp. 955-962 ◽  
Author(s):  
Annika Nordin ◽  
Inger K. Schmidt ◽  
Gaius R. Shaver

2010 ◽  
Vol 18 (6) ◽  
pp. 1157-1162
Author(s):  
Shu-Jun ZHAO ◽  
Jia-Fu YUAN ◽  
Xin-Ran ZHANG ◽  
Xiang-Yu XU ◽  
You-Sheng XIONG ◽  
...  

2020 ◽  
Vol 117 (3) ◽  
pp. 351-365
Author(s):  
J. Pijlman ◽  
G. Holshof ◽  
W. van den Berg ◽  
G. H. Ros ◽  
J. W. Erisman ◽  
...  

1996 ◽  
Vol 46 (2) ◽  
pp. 103-109 ◽  
Author(s):  
A. Jugsujinda ◽  
J. Prasittikhet ◽  
R. D. DeLaune ◽  
C. W. Lindau ◽  
R. P. Gambrell

Ecology ◽  
1982 ◽  
Vol 63 (5) ◽  
pp. 1277-1284 ◽  
Author(s):  
Edward K. Christie ◽  
James K. Delting

2020 ◽  
Author(s):  
Joann Whalen ◽  
Hicham Benslim

<p>Earthworms create hotspots that support microbial diversity and activity in soil. These hotspots may be internal to the earthworm, such as in their intestinal tract, or external to the earthworm in the biopores, casts and middens they create on the soil surface and within the soil profile. This presentation summarizes some of the key hotspots associated with earthworms, and how the biostimulated microbial community in these areas contributes to soil nitrogen cycling. We will present observations about the diversity and activity of nitrogen-cycling microorganisms that live within the earthworm and in its built environments, as well as the population- and community-level contributions of earthworms to denitrification, nitrogen mineralization, and the soil nitrogen supply in temperate agroecosystems.</p>


Soil Research ◽  
2017 ◽  
Vol 55 (1) ◽  
pp. 47 ◽  
Author(s):  
Duy Minh Dang ◽  
Ben Macdonald ◽  
Sören Warneke ◽  
Ian White

Sea-level rise and saline water intrusion have caused a shortage of fresh water and affected agricultural areas globally. Besides inundation, the salinity could alter soil nitrogen and carbon cycling in coastal soils. To examine the effect of salinity, an incubation experiment was used to investigate soil nitrogen and carbon cycling from an acid sulfate soil and an alluvial soil with and without additional nitrogen and carbon sources. Four levels of saline solution of 0.03, 10, 16 and 21dSm–1 were used to submerge acid sulfate and alluvial soil samples in a 125-mL jar. The experimental jars were incubated in the dark at 25°C. Gas samples were collected over 4 weeks and analysed for nitrous oxide (N2O), carbon dioxide (CO2) and methane (CH4). The results showed that salinity significantly decreased N2O emissions from the acid sulfate soil but did not affect emissions from the alluvial soil. Addition of glucose and nitrate enhanced N2O production in both salt-affected soils. Emissions of CO2 were not different among the salinity treatments, whereas available carbon and nitrate promoted soil respiration. Changes in CH4 fluxes over the 4-week incubation were the same for both soils, and substrate addition did not affect emissions in either soil. The findings indicate that salinity has altered carbon and nitrogen cycles in the acid sulfate soil, and future fertiliser and crop management will need to account for the changed nutrient cycling caused by saline water intrusion and climate change.


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