Feng Xian
Biographic Data
| ID | 1243910 |
|---|---|
| NAME | Feng Xian |
| GIVEN NAMES | Feng |
| FAMILY NAME | Xian |
| SIGNATURE | XIAN F |
| AFFILIATIONS | Academy of Arts and Design, Tsinghua University, Beijing, 100084, China. |
| ORCID | 0000-0003-4929-3601 |
| VERIFIED | Yes |
| TOTAL WORKS | 8 |
| TOTAL CITATIONS | 3 |
| WORKS AS AUTHOR | 8 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2004 |
| LATEST PUBLICATION YEAR | 2019 |
| H-INDEX | 1 |
M Under
66m Under is an interactive installation art exhibited in a public space of Beijing 751 Art Zone. A floating balloon sea continues to rise, reflecting the phenomenon of global warming. Visitors can interact with this installation artwork by showing their efforts to delay the rising of the sea in order to save a bird nest 66 meters high above the balloon sea. We created this artwork to encourage people to focus on environmental crisis and arouse p…
Holocene Precipitation Records from Inner Mongolia Derived from Hydrogen Isotope Compositions of Sediment Fatty Acids
The Inner Mongolian Plateau lies along the northern limit reached by the East Asian summer monsoon. This geographic setting makes it especially sensitive to environmental change and an excellent site for understanding Quaternary East Asian monsoon variability. In this study we present new results of hydrogen isotopic compositions of fatty acids extracted from sediments, which were used to construct Holocene paleoprecipitation (or moisture) change…
Asian Monsoon variation over the late Neogene–early Quaternary recorded by Anisotropy of Magnetic Susceptibility (AMS) from Chinese loess
Asynchronous records of Brunhes/Matuyama reversal in marine sediments and Chinese loess
Measurement of 10 Be Concentration of Modern Falling Dust in Northern China
Paleoenvironmental and paleogeomagnetic tracing studies from Chinese loess 10 Be have progressed in recent years (Zhou et al. 2007a,b, 2010). In this approach, 10 Be flux determined from sediment concentration and accumulation rate may be used to recover information about paleomonsoon rainfall rates as well as past variations in the geomagnetic field strength. However, these methods require that a correction be made for residual undecayed 10 Be i…
Measurement of 10Be Concentration of Modern Falling Dust in Northern China
Paleoenvironmental and paleogeomagnetic tracing studies from Chinese loess 10 Be have progressed in recent years (Zhou et al. 2007a,b, 2010). In this approach, 10 Be flux determined from sediment concentration and accumulation rate may be used to recover information about paleomonsoon rainfall rates as well as past variations in the geomagnetic field strength. However, these methods require that a correction be made for residual undecayed 10 Be i…
Reconstruction of 130-kyr Relative Geomagnetic Intensities from 10 Be in Two Chinese Loess Sections
Efforts to extract weak geomagnetic excursion signals from Chinese loess-paleosol 10 Be have generally been unsuccessful due to the complexities of its accumulation, because the geomagnetic and climate (precipitation and dust) signals contained in loess-paleosol sequence are tightly overprinted. Here, we present a reconstruction of geomagnetic relative paleointensities for the past 130 kyr from 10 Be records in 2 Chinese loess-paleosol sections u…
High-resolution evidence from southern China of an early holocene optimum and a mid-Holocene dry event during the Past 18,000 Years
Computer models suggest that the Holocene Optimum for East Asian summer monsoon precipitation occurred at different times in different regions of China. Previous studies indicate that this time-transgressive Holocene Optimum should have been experienced about 3000 yr ago in southern China. In this study we describe a section which allows us to test this timing directly. We have closely examined high-resolution eutrophic peat/mud sequences coverin…
Reconstruction of 130-kyr Relative Geomagnetic Intensities from 10 Be in Two Chinese Loess Sections
Efforts to extract weak geomagnetic excursion signals from Chinese loess-paleosol 10 Be have generally been unsuccessful due to the complexities of its accumulation, because the geomagnetic and climate (precipitation and dust) signals contained in loess-paleosol sequence are tightly overprinted. Here, we present a reconstruction of geomagnetic relative paleointensities for the past 130 kyr from 10 Be records in 2 Chinese loess-paleosol sections u…
High-resolution evidence from southern China of an early holocene optimum and a mid-Holocene dry event during the Past 18,000 Years
Computer models suggest that the Holocene Optimum for East Asian summer monsoon precipitation occurred at different times in different regions of China. Previous studies indicate that this time-transgressive Holocene Optimum should have been experienced about 3000 yr ago in southern China. In this study we describe a section which allows us to test this timing directly. We have closely examined high-resolution eutrophic peat/mud sequences coverin…
Reconstruction of 130-kyr Relative Geomagnetic Intensities from 10 Be in Two Chinese Loess Sections
Efforts to extract weak geomagnetic excursion signals from Chinese loess-paleosol 10 Be have generally been unsuccessful due to the complexities of its accumulation, because the geomagnetic and climate (precipitation and dust) signals contained in loess-paleosol sequence are tightly overprinted. Here, we present a reconstruction of geomagnetic relative paleointensities for the past 130 kyr from 10 Be records in 2 Chinese loess-paleosol sections u…
Measurement of 10 Be Concentration of Modern Falling Dust in Northern China
Paleoenvironmental and paleogeomagnetic tracing studies from Chinese loess 10 Be have progressed in recent years (Zhou et al. 2007a,b, 2010). In this approach, 10 Be flux determined from sediment concentration and accumulation rate may be used to recover information about paleomonsoon rainfall rates as well as past variations in the geomagnetic field strength. However, these methods require that a correction be made for residual undecayed 10 Be i…
Measurement of 10Be Concentration of Modern Falling Dust in Northern China
Paleoenvironmental and paleogeomagnetic tracing studies from Chinese loess 10 Be have progressed in recent years (Zhou et al. 2007a,b, 2010). In this approach, 10 Be flux determined from sediment concentration and accumulation rate may be used to recover information about paleomonsoon rainfall rates as well as past variations in the geomagnetic field strength. However, these methods require that a correction be made for residual undecayed 10 Be i…
Asynchronous records of Brunhes/Matuyama reversal in marine sediments and Chinese loess
Asian Monsoon variation over the late Neogene–early Quaternary recorded by Anisotropy of Magnetic Susceptibility (AMS) from Chinese loess
M Under
66m Under is an interactive installation art exhibited in a public space of Beijing 751 Art Zone. A floating balloon sea continues to rise, reflecting the phenomenon of global warming. Visitors can interact with this installation artwork by showing their efforts to delay the rising of the sea in order to save a bird nest 66 meters high above the balloon sea. We created this artwork to encourage people to focus on environmental crisis and arouse p…
Holocene Precipitation Records from Inner Mongolia Derived from Hydrogen Isotope Compositions of Sediment Fatty Acids
The Inner Mongolian Plateau lies along the northern limit reached by the East Asian summer monsoon. This geographic setting makes it especially sensitive to environmental change and an excellent site for understanding Quaternary East Asian monsoon variability. In this study we present new results of hydrogen isotopic compositions of fatty acids extracted from sediments, which were used to construct Holocene paleoprecipitation (or moisture) change…
Geology (7 works) · Geology and Paleoclimatology Research (7 works) · Geography (5 works) · Geomagnetism and Paleomagnetism Studies (5 works) · Loess (5 works) · Paleontology (4 works) · Physical geography (4 works) · Precipitation (4 works) · Quaternary (4 works) · Archaeology (3 works)