δ15N natural abundance may directly disclose perturbed soil when related to C:N ratio

2013 ◽  
Vol 27 (10) ◽  
pp. 1101-1104 ◽  
Author(s):  
Franz Conen ◽  
Mikhail V. Yakutin ◽  
Nina Carle ◽  
Christine Alewell
2012 ◽  
Vol 31 (3) ◽  
pp. 1003-1015 ◽  
Author(s):  
Marc Peipoch ◽  
Eugènia Martí ◽  
Esperança Gacia

Geoderma ◽  
2018 ◽  
Vol 313 ◽  
pp. 126-134 ◽  
Author(s):  
Kathryn A. Conrad ◽  
Ram C. Dalal ◽  
Scott A. Dalzell ◽  
Diane E. Allen ◽  
Ryosuke Fujinuma ◽  
...  

2009 ◽  
Vol 325 (1-2) ◽  
pp. 157-169 ◽  
Author(s):  
Melanie Kriszan ◽  
Wulf Amelung ◽  
Jürgen Schellberg ◽  
Thomas Gebbing ◽  
Walter Kühbauch

2008 ◽  
Vol 53 (No. 8) ◽  
pp. 329-339 ◽  
Author(s):  
S.P. Sah ◽  
H. Ilvesniemi

The primary objective of this paper is to study the interspecific variation of <sup>15</sup>N natural abundance in two dominant conifer tree species, Scot pine (<i>Pinus sylvestris</i> L.) and Norway spruce (<i>Picea abies</i> L. Karst) in a N-limited mixed boreal coniferous forest in southern Finland. Both a mature tree stand (a natural forest stand) and a stand of seedlings in a clear-cut area were considered. We analyzed %N and δ15N natural abundance in needles, branches, litter and soil of the both above-mentioned stands. Pine needles had higher N concentrations than spruce needles, both in mature forest (pine = 1.09%, SE ± 0.02 and spruce = 0.79%, SE ± 0.02) and in the clear-cut area (pine = 1.01%, SE ± 0.07 and spruce = 0.74%, SE ± 0.04). Furthermore, pine needles were significantly more depleted in δ15N natural abundance than the spruce needles, both in the mature forest (pine = –5.6‰, SE ± 0.1‰ and spruce = –4.0‰, SE ± 0.2‰) and in the clear-cut sites (pine = –2.8‰, SE ± 0.2‰ and spruce = –2.1‰, SE ± 0.3‰). The more pronounced depletion of <sup>15</sup>N in the pine foliage might be connected to its different fungal associates in the roots compared to spruce roots. We assume that the mycorrhizal N-uptake is very prominent at the N-limited site. After clear-cutting, needles of the seedlings and the uppermost part of soil organic layer were found to be more 15N-enriched than at the natural forest site. This was attributed to an increased level of nitrification in the clear-cut site soil.


Author(s):  
V. T. Sinegovskaya ◽  
E. T. Naumchenko

The article presents the results of comparative evaluation of the efficiency of the long-term application of mineral and organic fertilizers in the crop rotation system. It was found that the application of the mineral fertilizer system increased the value of hydrolytic acidity of the soil from 4,30 to 5,29 mg-eq per 100 g of soil, the indicator of metabolic acidity decreased from 5,2 to 4,9 pH units. By the end of the 11th rotation for both fertilizer systems, the content of mobile phosphorus increased by more than 4 times relative to the initial value, its mobility indicator – by 2,2-3,2 times compared with the control. The use of the organo-mineral system was accompanied by an increase in the content of humus by 0,35 % and a decrease in the C:N ratio from 11,2 to 8,9. The increased productivity of wheat was revealed when applying nitrogen and nitrogen-phosphorus fertilizers against the background of prolonged use of the mineral and organo-mineral fertilizer system. The change in wheat productivity by 56 % depended on the content of mineral nitrogen, mobile phosphorus, humus in the topsoil, and on the phosphate ion mobility. Soybean productivity depended on soil fertility indicators only by 24 %: the relationship between soybean productivity and the mineral forms of nitrogen and phosphorus is weak and direct, between productivity and P2O5 mobility - weak and inverse, with humus - moderate and direct.


Author(s):  
Alla Varenik ◽  
Alla Varenik ◽  
Sergey Konovalov ◽  
Sergey Konovalov

Atmospheric precipitations can be an important source of nutrients to open and coastal zones of marine ecosystem. Jickells [1] has published that atmospheric depositions can sup-port 5-25% of nitrogen required to primary production. Bulk atmospheric precipitations have been collected in a rural location at the Black Sea Crimean coast – Katsiveli settlement, and an urban location – Sevastopol city. Samples have been analyzed for inorganic fixed nitrogen (IFN) – nitrate, nitrite, and ammonium. Deposi-tions have been calculated at various space and time scales. The monthly volume weighted mean concentration of IFN increases from summer to winter in both locations. A significant local source of IFN has been revealed for the urban location and this source and its spatial influence have been quantified. IFN deposition with atmospheric precipitations is up to 5% of its background content in the upper 10 m layer of water at the north-western shelf of the Black Sea. Considering Redfield C:N ratio (106:16) and the rate of primary production (PP) in coastal areas of the Black Sea of about 100-130 g C m-2 year-1 we have assessed that average atmospheric IFN depositions may intensify primary production by 4.5% for rural locations, but this value is increased many-fold in urban locations due to local IFN sources.


1981 ◽  
Vol 45 (2) ◽  
pp. 450-451 ◽  
Author(s):  
Daniel H. Kohl ◽  
Barbara A. Bryan ◽  
Georgia Shearer ◽  
Ross A. Virginia

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