Yunzhao Wu

ORCID: 0000-0001-8408-1204
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About
Contact & Profiles
Research Areas
  • Planetary Science and Exploration
  • Astro and Planetary Science
  • Calibration and Measurement Techniques
  • Isotope Analysis in Ecology
  • Geochemistry and Geologic Mapping
  • Space Science and Extraterrestrial Life
  • Space Exploration and Technology
  • Remote Sensing and Land Use
  • Atmospheric Ozone and Climate
  • Geology and Paleoclimatology Research
  • Nuclear Physics and Applications
  • Spacecraft and Cryogenic Technologies
  • Soil Geostatistics and Mapping
  • Geological and Geochemical Analysis
  • Heavy metals in environment
  • Scientific Research and Discoveries
  • Aeolian processes and effects
  • Environmental Quality and Pollution
  • Infrared Target Detection Methodologies
  • Advanced Image Fusion Techniques
  • Atmospheric aerosols and clouds
  • Crystallography and molecular interactions
  • Stellar, planetary, and galactic studies
  • Spaceflight effects on biology
  • Remote-Sensing Image Classification

Purple Mountain Observatory
2017-2025

Center for Excellence in Molecular Cell Science
2019-2024

Macau University of Science and Technology
2009-2024

Chinese Academy of Sciences
2006-2024

Jiangsu Center for Collaborative Innovation in Geographical Information Resource Development and Application
2016-2023

University of Science and Technology of China
2023

Planetary Science Institute
2019

Planet
2019

Nanjing University
2005-2016

State Key Laboratory of Remote Sensing Science
2007-2012

Conventional methods for investigating heavy metal contamination in soil are time consuming and expensive. In this study, we (i) explored reflectance spectroscopy as an alternative method assessing metals, (ii) further the physicochemical mechanism that allows estimation of metals with method. We first investigated spectral response changing concentrations soils. The results indicated only at very high concentration can transition elements exhibit their inherent absorption features. spite...

10.2136/sssaj2006.0285 article EN Soil Science Society of America Journal 2007-05-01

Until recently, global high spatial resolution maps of FeO and TiO 2 the Moon were only derived from Clementine data. In this study, we show using Chang'E‐1 Interference Imaging Spectrometer (IIM) at a 200 m/pixel. With newly developed calibration presented here, spectra obtained by IIM compare well with telescopic spectra. Spectral parameters previously shown to be sensitive iron titanium, calibrated data are highly correlated measured elemental concentration R = 0.96 for 0.95 . The...

10.1029/2011je003879 article EN Journal of Geophysical Research Atmospheres 2011-12-08

Abstract Whether or not background secondary craters dominate populations of small impact on terrestrial bodies is a half‐century controversy. It has been suggested that some planetary are dominated by based partly the steepened slope crater size‐frequency distribution (CSFD) toward diameters, such as less than ~1 km diameter population lunar mare. Here we show topography degradation enlarges and increases CSFD slopes with time. When taken into account, for various‐aged populations, observed...

10.1002/2017gl075298 article EN Geophysical Research Letters 2017-10-06

10.1016/j.epsl.2017.12.003 article EN Earth and Planetary Science Letters 2017-12-20

Abstract How bright the Moon is forms a simple but fundamental and important question. Although numerous efforts have been made to answer this question such as use of sophisticated electro-optical measurements suggestions for calibration sites, still debated. An in situ measurement with panel on surface crucial obtaining accurate absolute reflectance resolving debate. China’s Chang’E-3 (CE-3) “Yutu” rover accomplished type using Visible-Near Infrared Spectrometer (VNIS). The VNIS, which were...

10.3847/1538-3881/aabaf5 article EN The Astronomical Journal 2018-04-27

10.1109/jstars.2025.3549691 article EN cc-by IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing 2025-01-01

Abstract The long-period comets' perihelion places them near the sun so they may exhibit activity. Before 2013 LU28 reached perihelion, we performed a continuous observation to detect possible Using Lijiang 2.4 m telescope with Johnson R filter, measured brightness of from 2024 January 3 April 13. instrumental magnitudes were subsequently transformed into Pan-STARR r system. Due noticeable descending trend in absolute magnitude, verified cometary activity and constrained some photometric...

10.1088/1674-4527/adbea2 article EN Research in Astronomy and Astrophysics 2025-03-10

Abstract Exploring low-velocity collisions is crucial for unraveling intricate processes in planetary formation, particularly the bouncing barrier that impedes aggregation of dust into sizable planetesimals. Observational data on extraterrestrial collision remain limited. Here, we quantify parameters millimeter-sized lunar particles impacting porous surface at speeds ranging from 2.3 to 76.8 cm s −1 under gravity, leveraging Chang’E-4 imagery. This study represents first tangible acquisition...

10.3847/1538-4357/adb4f5 article EN cc-by The Astrophysical Journal 2025-03-17

10.1109/jstars.2025.3554240 article EN cc-by IEEE Journal of Selected Topics in Applied Earth Observations and Remote Sensing 2025-01-01

In this article, we propose that reflectance spectroscopy or remote sensing technology is a rapid and inexpensive tool to monitor heavy-metal contamination in soils. We analyzed three data sets by both chemical methods. Despite the being obtained from different locations at times, all gave similar results; is, those were well correlated with Fe also had higher predictive accuracy: Ni, Cr, Co Baguazhou Island; Cu Jiangning County; Cu, As some areas of Island close correlations Fe, greater R2....

10.1097/ss.0b013e3182114717 article EN Soil Science 2011-03-19

Abstract Submicroscopic metallic iron (SMFe) created by space weathering has strong effects on the optical properties of lunar surface. Spectra measured in situ visible‐near‐infrared spectrometer (VNIS) board Chang'E‐3 Yutu rover were used to investigate maturity differences at CE‐3 landing site caused lander exhaust. SMFe abundances estimated using Hapke's radiative transfer model. Analysis spectrum for a minimally disturbed soil indicates that it contains 0.368 wt % SMFe, corresponding an...

10.1002/2017gl072652 article EN Geophysical Research Letters 2017-04-05

Abstract The last major phases of lunar volcanism occurred mainly in Oceanus Procellarum and Mare Imbrium produced spectrally unique medium‐ high‐titanium basalts. composition distribution these basalts provide a record the late stage thermal evolution Moon. To study spectral mineralogical variations mare basalts, 31 distinct units were mapped employing range remote sensing data. Their inferred characteristics studied by analyzing features small, fresh craters derived from Moon Mineralogy...

10.1002/2016je005051 article EN Journal of Geophysical Research Planets 2016-09-17

Aims . Studies on high-resolution and high-precision laboratory reflectance spectra of the Moon have historically been restricted to analysis old Apollo samples (>3.0 Ga). In contrast, studies young lunar soils exclusively relied remote sensing spectra. this study, we present results a spectral investigation (~2.0 Ga) obtained by Chang’E-5 (CE-5) mission. Methods We analyzed surficial subsurface collected through scooped drilled sampling methods. The CE-5 were compared with those orbital...

10.1051/0004-6361/202347577 article EN cc-by Astronomy and Astrophysics 2023-12-15
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