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Dive into the research topics where Michael P. Jimenez-Cruz is active.

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Featured researches published by Michael P. Jimenez-Cruz.


Aerosol Science and Technology | 2004

Analysis of aerosols from the World Trade Center collapse site, New York, October 2 to October 30, 2001

Thomas A. Cahill; Steven S. Cliff; Kevin D. Perry; Michael P. Jimenez-Cruz; Graham Bench; Patrick G. Grant; Dawn Ueda; James F. Shackelford; Michael R. Dunlap; Michael L. Meier; Peter B. Kelly; Sarah G. Riddle; Jodye Selco; Robert Z. Leifer

The collapse of the World Trade Center (WTC) buildings #2 (South Tower), #1 (North Tower), and #7 created an enormous collapse pile which emitted intense plumes of acrid smoke and dust until roughly mid-December, when the last spontaneous surface fire occurred. We collected particles by size (8 modes, ≈12 to 0.09 micrometers diameter) and time (typical resolution of 1 to 3 h) from October 2 until late December at the EML 201 Varick Street site roughly 1.8 km NNE of the collapse site and 50 m above ground level. Here we show some of the 70,000 mass and elemental data from the time period October 2 through October 30. Identification of a WTC collapse pile source for aerosols seen at the receptor site were based upon the simultaneous presence of finely powdered concrete, gypsum, and glass with intense very fine combustion mode mass episodes concurrent with winds from the southwest quadrant. The results, derived from seven independent beam-based analytical techniques, showed that while PM10 and PM2.5 24 h values rarely, if ever, violated federal air quality standards, WTC-derived plumes swept over lower Manhattan Island, resulting in intense aerosol impacts of duration a few hours at any one site. The WTC plume resembled in many ways those seen from municipal waste incinerators and high temperatures processes in coal-fired power plants. The size fractions above 1 micrometer contained finely powdered concrete, gypsum, and glass, with sootlike coatings and anthropogenic metals, but little asbestos. Composition in the very fine size range (0.26 > Dp > 0.09 μm) was dominated by sulfuric acid and organic matter, including polycyclic aromatic hydrocarbons (PAHs) and their derivatives, and glasslike silicon-containing aerosols. Many metals were seen in this mode, most, but not all, at low concentrations. The concentrations of very fine silicon, sulfur, and many metals, as well as coarse anthropogenic metals, decreased markedly during October, probably in association with the cooling of the collapse piles. Values of very fine elements seen in May, 2002 at the WTC site were only a few percent of October values.


Nuclear Instruments & Methods in Physics Research Section B-beam Interactions With Materials and Atoms | 2002

Development of PIXE, PESA and transmission ion microscopy capability to measure aerosols by size and time

V. Shutthanandan; Suntharampillai Thevuthasan; R. Disselkamp; A. Stroud; A. Cavanagh; E.M. Adams; D.R. Baer; L. A. Barrie; Steven S. Cliff; Michael P. Jimenez-Cruz; Thomas A. Cahill

Abstract We describe a new capability that consists of a combination of proton induced X-ray emission (PIXE), proton elastic scattering analysis (PESA) and transmission ion microscopy (all performed at the same location on the sample) techniques to address some of the research needs associated with time series and size-dependent composition of atmospheric aerosols. Simultaneous measurements of PIXE and PESA can be performed on aerosols collected using 3 stage improved rotating DRUM impactor by size (Stage A: 2.5–1.15 μm; Stage B: 0.34–1.15 μm; Stage C: 0.07–0.34 μm) with time resolution set by the rotation rate from 1 mm every 4 h to 1 mm every 6 min on a 16.8 cm long impaction strips that can be coated with Mylar, stretched Teflon, or aluminum, depending on the analysis method chosen. Preliminary measurements carried out using a 1 mm diameter proton beam were made on industrial test samples, yielding promising results at a time resolution of only 6 min.


Journal of Geophysical Research | 2004

Evidence for hygroscopic mineral dust particles from the Intercontinental Transport and Chemical Transformation Experiment

Kevin D. Perry; Steven S. Cliff; Michael P. Jimenez-Cruz


Archive | 1999

Size and time resolved anthropogenic components of aerosols via synchrotron x-ray fluorescence: application to Asian aerosol transport

Thomas A. Cahill; Steven S. Cliff; Kevin D. Perry; Michael P. Jimenez-Cruz; Scott A. McHugo


Journal of Geophysical Research | 2004

Evidence for hygroscopic mineral dust particles from the Intercontinental Transport and Chemical Transformation Experiment: HYGROSCOPIC MINERAL DUST PARTICLES

Kevin D. Perry; Steven S. Cliff; Michael P. Jimenez-Cruz


Archive | 2004

Enhancing spatial and temporal resolution of trace elements in sediment cores

B. L. Johnson; Michael P. Jimenez-Cruz; Steven S. Cliff; James R. Hunt


Archive | 2004

Aerosol Transport to the Greenland Summit Site, June, 2003 to August 2004

Thomas A. Cahill; Steven S. Cliff; Michael P. Jimenez-Cruz; L. Portnoff; Kevin D. Perry; J. R. McConnell; J. F. Burkhart; Roger C. Bales


Journal of Geophysical Research | 2004

Evidence for hygroscopic mineral dust particles from the Intercontinental Transport and Chemical Transformation Experiment : Intercontinental Transport and Chemical Transformation 2002 (ITCT 2K2) and Pacific Exploration of Asian Continental Emissions (PEACE) experiments

Kevin D. Perry; Steven S. Cliff; Michael P. Jimenez-Cruz


Archive | 2003

The Asian continental aerosol plume is the dominant component of the ``background'' tropospheric aerosol over North America

Richard A. VanCuren; Steven S. Cliff; Kevin D. Perry; Michael P. Jimenez-Cruz


Archive | 2002

Aerosol Transport to the U.S. Receptor Sites during ACE-Asia

Michael P. Jimenez-Cruz; Thomas A. Cahill; Kevin D. Perry; Steven S. Cliff; Catherine F. Cahill; Robert Scott Disselkamp

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Peter B. Kelly

University of California

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Richard A. VanCuren

California Air Resources Board

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A. Cavanagh

Pacific Northwest National Laboratory

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A. Stroud

Pacific Northwest National Laboratory

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Catherine F. Cahill

University of Alaska Fairbanks

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D.R. Baer

Pacific Northwest National Laboratory

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