Hydrogeochemical characterization of oilfield waters from southeast Maracaibo Basin (Venezuela): Diagenetic effects on chemical and isotopic composition

2016 ◽  
Vol 73 ◽  
pp. 228-248 ◽  
Author(s):  
Tiziano Boschetti ◽  
Beatriz Angulo ◽  
Frank Cabrera ◽  
Jhaisson Vásquez ◽  
Ramón Luis Montero
Ecohydrology ◽  
2011 ◽  
Vol 4 (4) ◽  
pp. 597-607 ◽  
Author(s):  
V. Marconi ◽  
M. Antonellini ◽  
E. Balugani ◽  
E. Dinelli

2003 ◽  
Vol 19 (2) ◽  
pp. 209-214 ◽  
Author(s):  
Jean-François Mauffrey ◽  
François Catzeflis

Stable isotopes are commonly used in ecological studies to infer food resources (Ambrose & DeNiro 1986, Bocherens et al. 1990,1991,1994;Yoshinaga et al. 1991) since isotopic composition is conserved during the feeding process. Moreover,for herbivorous (sensu lato) species, it is often possible to identify the main resource because different photosynthetic pathways generate different values of carbon isotope ratios (Park & Epstein 1961, Sternberg et al. 1984). This allows the characterization of broad biota such as savannas or forest and discrimination of grazers from sympatric folivorous species (DeNiro & Epstein 1978).


2013 ◽  
Author(s):  
T. Mikunthan ◽  
M. Vithanage ◽  
S. Pathmarajah ◽  
S. Arasalingam ◽  
R. Ariyaratne ◽  
...  

2019 ◽  
Vol 31 (4) ◽  
pp. 1245-1253 ◽  
Author(s):  
Lakhvinder Kaur ◽  
Madhuri S. Rishi ◽  
Sakshi Sharma ◽  
Bhavika Sharma ◽  
Renu Lata ◽  
...  

2019 ◽  
Vol 98 ◽  
pp. 12016 ◽  
Author(s):  
Neus Otero ◽  
Alba Llovet ◽  
Raúl Carrey ◽  
Angela Ribas ◽  
Xavier Domene ◽  
...  

Increase of soil fertilization produces an increase of N exported to the hydrosphere. The amount of nitrate that reaches the aquifers is controlled by processes affecting N-species within the soils. The most relevant processes are nitrification, denitrification, assimilation, mineralization, and immobilization. This work studies the fate of N compounds in soil after manure application in a lysimeter study. To this end the isotopic composition of N and O of dissolved nitrate (δ15N-NO3- and δ18O-NO3-) was studied coupled with the evolution of N-compounds retained and leached from the soil. Results showed an increase in the δ15N-NO3- of the leached nitrate towards values similar to the δ15N-NH4+ from the applied manure. The highest δ15N-NO3- values were measured after 100 days of manure application, and thereafter, values decreased progressively towards the initial δ15N-NO3- of the soil before manure application.


Sign in / Sign up

Export Citation Format

Share Document