Search Results - "Feng, Z. D."

Stratigraphies and chronologies of late Quaternary loess–paleosol sequences in the core area of the central Asian arid zone by Feng, Z.-D., Ran, M., Yang, Q.L., Zhai, X.W., Wang, W., Zhang, X.S., Huang, C.Q.

“…The sporadic distribution of the Quaternary loess in Central Asia makes it hard to establish a regional pedostratigraphy through visual tracing of marker…”
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Holocene climatic and environmental changes in the arid and semi-arid areas of China: a review by Feng, Z.-D., An, C. B., Wang, H. B.

“…This paper reviews recently published literature, most of which was published in Chinese, and searches for regional patterns of Holocene changes useful in…”
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Climate changes and hydrological responses in the Tianshan Mountains and the northern Basins by Feng, Z.-D.

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Bioclimatic change of the past 2500 years within the Balkhash Basin, eastern Kazakhstan, Central Asia by Feng, Z.-D., Wu, H.N., Zhang, C.J., Ran, M., Sun, A.Z.

“…On the bases of analytical data of an 850-cm-long sediment core collected from Balkhash Lake with a chronological control of seventeen AMS dates, this research…”
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Geomorphological and sedimentological precautions in radiocarbon dating of eolian and lacustrine sequences in arid Asia by Feng, Z.-D., Ran, Min, Yang, Qili

“…Lacustrine sediments in deep lakes are suitable for establishing radiocarbon chronology. Lacustrine sediments in shallow lakes are not suitable for…”
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Effect of liquid-phase-deposited parameters on the photogenerated cathodic protection properties of TiO2 films by Lei, C.X., Zhou, H., Feng, Z.D.

“…► The TiO2 films were prepared at different deposition parameters by LPD method. ► The deposition parameters could affect the photocathodic protection of TiO2…”
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Holocene climate variations retrieved from Gun Nuur lake-sediment core in the northern Mongolian Plateau by Feng, Z-D, Ma, YZ, Zhang, HC, Narantsetsega, Ts, Zhang, XS

“…Our pollen-based climate reconstruction shows that both temperature and moisture were low during the early Holocene from ~10,000 to ~8000 cal. a BP and…”
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Late Quaternary palaeolake levels in Tengger Desert, NW China by Zhang, H.C, Peng, J.L, Ma, Y.Z, Chen, G.J, Feng, Z.-D, Li, B, Fan, H.F, Chang, F.Q, Lei, G.L, Wünnemann, B

“…Comprehensive field investigations and laboratory analyses show that palaeolakes, including the Megalake Tengger, and other semi-connected and isolated water…”
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Holocene vegetation variations and the associated environmental changes in the western part of the Chinese Loess Plateau by Feng, Z.-D., Tang, L.Y., Wang, H.B., Ma, Y.Z., Liu, K.-b.

“…The western part of the Chinese Loess Plateau has experienced a series of environmental changes during the Holocene. A desert-steppe of late glacial was…”
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Vegetation variations and associated environmental changes during marine isotope stage 3 in the western part of the Chinese Loess Plateau by Feng, Z.-D., Tang, L.Y., Ma, Y.Z., Zhai, Z.X., Wu, H.N., Li, F., Zou, S.B., Yang, Q.L., Wang, W.G., Derbyshire, E., Liu, K.-B.

“…This study further investigates the reported “uniqueness” of MIS 3 climatic changes in northwestern China by focusing on the MIS 3 lacustrine-wetland sequences…”
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Simulating evapotranspiration of Qinghai spruce ( Picea crassifolia) forest in the Qilian Mountains, northwestern China by Tian, F.X., Zhao, C.Y., Feng, Z.-D.

“…Qinghai spruce ( Picea crassifolia) forests play an important role in regulating the regional water balance of the Qilian Mountains in northwestern China. The…”
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Stratigraphic evidence of a Megahumid climate between 10,000 and 4000 years B.P. in the western part of the Chinese Loess Plateau by Feng, Z.-D., An, C.B., Tang, L.Y., Jull, A.J.T.

“…Our field surveys show that a wetland/swamp layer is widely distributed in the western part of the Chinese Loess Plateau. The grayish-blue and aquatic…”
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Eolian environmental changes in the Northern Mongolian Plateau during the past ∼ 35,000 yr by Feng, Z.-D., Zhai, X.W., Ma, Y.Z., Huang, C.Q., Wang, W.G., Zhang, H.C., Khosbayar, P., Narantsetseg, T., Liu, K.-B., Rutter, N.W.

“…This study focuses on an eolian section (Shaamar section) in the Northern Mongolian Plateau and compares the eolian sequences in the Northern Mongolian Plateau…”
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Neural network learning algorithms for tracking minor subspace in high-dimensional data stream by FENG, Da-Zheng, ZHENG, Wei-Xing, YING JIA

“…A novel random-gradient-based algorithm is developed for online tracking the minor component (MC) associated with the smallest eigenvalue of the…”
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Lacustrine and eolian records of Holocene climate changes in the Mongolian Plateau: preliminary results by Feng, Z.-D., Wang, W.G., Guo, L.L., Khosbayar, P., Narantsetseg, T., Jull, A.J.T., An, C.B., Li, X.Q., Zhang, H.C., Ma, Y.Z.

“…This study compares two pairs of adjacent lacustrine and eolian sections at sites in the southern and northern Mongolian Plateaus in order to test spatial…”
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The effect of high-temperature annealing on tensile strength and its mechanism of Hi-Nicalon SiC fibres under inert atmosphere by YAO, R. Q., WANG, Y. Y., FENG, Z. D.

“…ABSTRACT Hi‐Nicalon SiC (silicon carbide) fibres were annealed in an argon flow for 10 h at 1400 °C, 1600 °C and 1800 °C. The strength of the fibres was…”
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Pedogenic factors affecting magnetic susceptibility of the last interglacial palaeosol S1 in the Chinese Loess Plateau by Feng, Z.D, Wang, H.B, Olson, C.G

“…The magnetic susceptibility has been used as a quantitative or semi-quantitative proxy for reconstructing the summer monsoon intensity in the Chinese Loess…”
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A high resolution record of vegetation and environmental variation through the last ∼ 25,000 years in the western part of the Chinese Loess Plateau by Wu, H.N., Ma, Y.Z., Feng, Z.-D., Sun, A.Z., Zhang, C.J., Li, F., Kuang, J.

“…We present a high-resolution reconstruction of vegetation and environmental changes from a 40-m thick section in the western part of the Chinese Loess Plateau…”
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Pedostratigraphy and carbonate accumulation in the last interglacial pedocomplex of the Chinese Loess Plateau by Feng, Z.D, Wang, H.B

“…This paper examines the geographic variations of carbonate concentrations in last interglacial pedocomplex (S1) profiles along a northwest (NW)-southeast (SE)…”
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Geographic variations in particle size distribution of the last interglacial pedocomplex S1 across the Chinese Loess Plateau: Their chronological and pedogenic implications by Feng, Z.-D., Wang, H.B.

“…Due to northwestward attenuation of the summer monsoon and northwestward intensification of loess deposition during the last interglacial, the last…”
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