Arid
DOI10.1007/s12647-019-00337-5
Geochemical, stable isotopic, palynological characterization of surface dry soils and atmospheric particles over Jodhpur city (Thar Desert, Rajasthan) during peak summer of 2013
Agnihotri, Rajesh1,2; Sawlani, Ravi2,3; Azam, M. M.4; Basumatary, S. K.1; Sharma, C.2,3; Mishra, S. K.2,3; Kumar, Rajeev5; Narayanan, T.6; Rathore, J. S.7; Tripathi, Jayant4
通讯作者Agnihotri, Rajesh
来源期刊MAPAN-JOURNAL OF METROLOGY SOCIETY OF INDIA
ISSN0970-3950
EISSN0974-9853
出版年2020
卷号35期号:1页码:53-67
英文摘要Atmospheric dust originating from the Thar Desert (India) acts as the local source of mineral dust in South Asia, spreading over an area of 0.32 x 10(6) km(2). Regional studies conducted during peak boreal summer are required to characterize this mineral dust that blows in form of episodic dust storms towards Indo-Gangetic Plains (IGP), using a multi-tracer approach. To achieve this goal, atmospheric PM10 particles were collected along with surface dry soils between 3 and 11 June, 2013, from in and around the Jodhpur city (26.2389 degrees N, 73.0243 degrees E) to glean elemental composition, stable isotopic and palynological (pollen types) database. Typical crustal elemental ratios, e.g. Si/Al, Ca/Al, Fe/Al, K/Al, Mg/Al, Ti/Al, varied in narrow ranges 8.1 +/- 1.21, 1.02 +/- 1.53, 0.50 +/- 0.14, 0.34 +/- 0.06, 0.19 +/- 0.06 and 0.06 +/- 0.02, respectively. Average Sr/Al, Rb/Al and Zr/Al ratios were found to be 39.70 +/- 12.24, 18.00 +/- 2.0 and 70.83 +/- 13.11 (mu g gm(-1)/wt%), respectively. Average delta C-13, delta N-15, delta S-34 values of surface soils were - 10.5 parts per thousand +/- 4.0, 11.4 parts per thousand +/- 1.6 and 3.6 parts per thousand +/- 2.1, while delta C-13 and delta N-15 of atmospheric PM10 particles varied in ranges - 25.6 parts per thousand +/- 0.67 and 9.9 parts per thousand +/- 1.7, respectively. Observed palynoassemblage indicated the open nature of vegetation that usually grows under warm-humid conditions with traces of few allergens and pathogens. Generated chemical-isotopic-pollen database could be utilized for deciphering origin of dust storms in IGP. Detailed multi-proxy characterization of mineral dust from the Thar Desert can further help to determine its role in influencing air quality and human health.
英文关键词Thar Desert Atmospheric aerosols Surface soils Pollens Carbon isotopes Nitrogen isotopes Sulphur isotopes
类型Article
语种英语
国家India
收录类别SCI-E
WOS记录号WOS:000520484900007
WOS关键词DIESEL EXHAUST PARTICLES ; ARABIAN SEA ; AEROSOL-PARTICLES ; SEDIMENTARY-ROCKS ; POLLEN GRAINS ; DUST ; POLLUTION ; CLIMATE ; NITROGEN ; CARBON
WOS类目Instruments & Instrumentation ; Physics, Applied
WOS研究方向Instruments & Instrumentation ; Physics
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/315154
作者单位1.Birbal Sahni Inst Palaeosci, 53 Univ Rd, Lucknow 226007, Uttar Pradesh, India;
2.CSIR, Natl Phys Lab, Dr KS Krishnan Marg, New Delhi 110012, India;
3.Acad Sci & Innovat Res AcSIR, CSIR, NPL Campus,Dr KS Krishnan Marg, New Delhi 110012, India;
4.Jawaharlal Nehru Univ, Sch Environm Sci, New Delhi 110067, India;
5.CSIR, Adv Mat & Proc Res Inst, Bhopal 462026, India;
6.IIT Hyderabad, Dept Phys, Kandi 502285, Telangana, India;
7.Jay Narayan Vyas Univ, Jodhpur 342001, Rajasthan, India
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Agnihotri, Rajesh,Sawlani, Ravi,Azam, M. M.,et al. Geochemical, stable isotopic, palynological characterization of surface dry soils and atmospheric particles over Jodhpur city (Thar Desert, Rajasthan) during peak summer of 2013[J],2020,35(1):53-67.
APA Agnihotri, Rajesh.,Sawlani, Ravi.,Azam, M. M..,Basumatary, S. K..,Sharma, C..,...&Tripathi, Jayant.(2020).Geochemical, stable isotopic, palynological characterization of surface dry soils and atmospheric particles over Jodhpur city (Thar Desert, Rajasthan) during peak summer of 2013.MAPAN-JOURNAL OF METROLOGY SOCIETY OF INDIA,35(1),53-67.
MLA Agnihotri, Rajesh,et al."Geochemical, stable isotopic, palynological characterization of surface dry soils and atmospheric particles over Jodhpur city (Thar Desert, Rajasthan) during peak summer of 2013".MAPAN-JOURNAL OF METROLOGY SOCIETY OF INDIA 35.1(2020):53-67.
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