2011
DOI: 10.1016/j.apgeochem.2011.05.006
|View full text |Cite
|
Sign up to set email alerts
|

Sources and distribution of aliphatic and polycyclic aromatic hydrocarbons in Yellow River Delta Nature Reserve, China

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
4
1

Citation Types

3
46
1
1

Year Published

2013
2013
2021
2021

Publication Types

Select...
5
3
2

Relationship

1
9

Authors

Journals

citations
Cited by 94 publications
(51 citation statements)
references
References 32 publications
3
46
1
1
Order By: Relevance
“…Ant/(Ant + Phe) ratios of >0.1 are the indicator of pyrogenic origin of PAHs, while <0.1 ratios are petrogenic origin of PAHs [51]. Meanwhile, a Fla/(Fla + Pyr) < 0.4 ratio indicates a petroleum source, a ratio between 0.4 and 0.5 indicates liquid fossil fuel combustion, and a ratio of >0.50 suggests the combustion of biomass and coal [53,54]. In addition, BaA/(BaA + Chr) ratio is considered as a specific marker for coal combustion [55,56].…”
Section: Source Estimates From Diagnostic Ratiosmentioning
confidence: 99%
“…Ant/(Ant + Phe) ratios of >0.1 are the indicator of pyrogenic origin of PAHs, while <0.1 ratios are petrogenic origin of PAHs [51]. Meanwhile, a Fla/(Fla + Pyr) < 0.4 ratio indicates a petroleum source, a ratio between 0.4 and 0.5 indicates liquid fossil fuel combustion, and a ratio of >0.50 suggests the combustion of biomass and coal [53,54]. In addition, BaA/(BaA + Chr) ratio is considered as a specific marker for coal combustion [55,56].…”
Section: Source Estimates From Diagnostic Ratiosmentioning
confidence: 99%
“…9). This compound is a biomarker commonly found in most Chinese crude oil geologically derived from lacustrine sources (Philp and Fan, 1987 Oilfield (Pang et al, 2003) and the surface sediments in the Yellow River Estuary (Bigot et al, 1989;Wang et al, 2011). The steranes were detected in all samples analyzed and comprised mainly the 5a, 14b, 17b and minor 5a, 14a, 17a configurations, both occurring as 20S and 20R epimers (Fig.…”
Section: Introductionmentioning
confidence: 99%
“…One approach to understand sources and fate mechanisms of OM accumulated in sediments and soils is to utilize a molecular organic geochemical method, where n-alkanes, pristane (Pr), phytane (Ph), the unresolved complex mixture (UCM), alkylated polycyclic aromatic hydrocarbons (PAHs), hopane and sterane are used for the source identification of the OM (Yunker et al, 2002b;Kimbrough and Dickhut, 2006;Wang et al, 2006;Hu et al, 2009;Tolosa et al, 2009;Wang et al, 2011). These biomarkers, combined with total organic carbon (TOC), total nitrogen (TN), the soils can provide robust and powerful proxies for the distinguishing of the OM contributions from natural or anthropogenic sources (Wang et al, 2003;Tanner et al, 2010).…”
Section: Introductionmentioning
confidence: 99%