Sulfate reducer and sulfur oxidizer respond differentially to the invasion of Spartina alterniflora in estuarine salt marsh of China

2017 ◽  
Vol 99 ◽  
pp. 182-190 ◽  
Author(s):  
Yu Zheng ◽  
Nai-Shun Bu ◽  
Xi-En Long ◽  
Jing Sun ◽  
Chi-Quan He ◽  
...  
Pedosphere ◽  
2018 ◽  
Vol 28 (6) ◽  
pp. 884-894 ◽  
Author(s):  
Lian CHEN ◽  
Jianhua GAO ◽  
Qingguang ZHU ◽  
Yaping WANG ◽  
Yang YANG

2012 ◽  
Vol 34 (3) ◽  
pp. 313-322 ◽  
Author(s):  
JB Adams ◽  
A Grobler ◽  
C Rowe ◽  
T Riddin ◽  
TG Bornman ◽  
...  

1978 ◽  
Vol 112 (985) ◽  
pp. 461-470 ◽  
Author(s):  
Ivan Valiela ◽  
John M. Teal ◽  
Werner G. Deuser

2021 ◽  
Vol 20 (1) ◽  
Author(s):  
Catherine M. Van Dongen ◽  
Logan M. Rakes ◽  
Joseph W. Moriarty ◽  
Sam Mason ◽  
Matthias Leu

1982 ◽  
Vol 60 (9) ◽  
pp. 1618-1624 ◽  
Author(s):  
Andrew C. Marinucci ◽  
R. Bartha

Spartina alterniflora decomposition was monitored in the high and low salt marsh in litter bags (2-mm mesh). The detritus formed in this process was analyzed at various times for ash-free dry weight (AFDW) (combustion at 550 °C), total carbon (wet combustion to CO2), and total nitrogen (Kjeldahl digestion). A mathematical component model predicting the change of these parameters was developed to explain these data.The first-order decay equation Xt = X0 e−kt was used to explain AFDW and carbon changes. The k values ranged from 0.004 to 0.02 per day for data from the high and low marsh, respectively, for New Jersey. Nitrogen fluxes are described by four functions. Three of these are decay functions which theoretically model (1) loss of soluble nitrogen, (2) loss of recalcitrant nitrogenous plant material, and (3) loss of microbial nitrogen. The fourth is a logistic function which describes the microbial incorportaion of nitrogen into the detritus. Nitrogen and C/N ratio values calculated with these equations simulated values obtained from field data.


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