基于碎屑锆石年代学对黄土高原物源及其时空差异的理解与展望

doi:10.12118/j.issn.1000–6060.2021.06.11

Abstract

Abstract:

The Loess Plateau of China preserves the most widely distributed, thickest, and continuous aeolian dust deposits in the world. It is a valuable geological archive of continental paleoclimate and paleoenvironment in the Quaternary. For more than half a century, several studies have been conducted on the climate records of aeolian dust deposition and the genesis of the Loess Plateau. However, studies have yet to determine the exact source of loess dust and verify whether a temporal-spatial change occurred in the provenance history. In this study, existing zircon age spectral data are statistically analyzed to explore the genetic relationship of loess and the surrounding desert with orbital and tectonic age scales. Results reveal the following: (1) the application of zircon U-Pb age spectral method based on the obtained exact chronological information of deserts in northern arid regions may clarify the provenance relationship between loess and aeolian sand. (2) available data indicate that the provenance of L1 loess may be spatially different. (3) confirmation that the provenance of loess in the glacial-interglacial period has not changed significantly. (4) On the tectonic timescale, the age spectra of different regions indicate that the periods of possible provenance transfer have an obvious overlap. (5) The limited age spectral data of red clays suggest that spatial differences in provenance probably existed before the Quaternary. However, current data are limited; thus, further related studies should be conducted. Using this method, the history of changes in loess provenance may be explored on a continuous long-term scale, and data sets may be obtained and used for future provenance comparisons of multiple locations and profiles in the Loess Plateau.

Key words: detrital zircon U-Pb dating, source tracing, time and space differences, Loess Plateau

NIU Yanning,QI Lin,QIAO Yansong. Understanding and prospects of provenance and time-spatial differences in the Loess Plateau based on detrital zircon chronology[J].Arid Land Geography, 2021, 44(6): 1623-1634.

Figures/Tables 6

Fig. 1

Fig. 2

Fig. 3

Fig. 4

Fig. 5

Fig. 6

References 71

[1]	An Z S, Kukla G J, Porter S C, et al. Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of central China during the last 130000 years[J]. Quaternary Research, 1991, 36(1):29-36. doi: 10.1016/0033-5894(91)90015-W
[2]	An Z S, Kutzbach J E, Prell W L, et al. Evolution of Asian monsoons and phased uplift of the Himalaya-Tibetan Plateau since Late Miocene times[J]. Nature, 2001, 411(6833):62-66. doi: 10.1038/35075035
[3]	Ding Z L, Yu Z Y, Rutter N W, et al. Towards an orbital time scale for Chinese loess deposits[J]. Quaternary Science Reviews, 1994, 13(1):39-70. doi: 10.1016/0277-3791(94)90124-4
[4]	Ding Z L, Rutter N W, Sun J M, et al. Re-arrangement of atmospheric circulation at about 2.6 Ma over northern China: Evidence from grain size records of loess-palaeosol and red clay sequences[J]. Quaternary Science Reviews, 2000, 19(6):547-558. doi: 10.1016/S0277-3791(99)00017-7
[5]	Lu H Y, Sun D H. Pathways of dust input to the Chinese Loess Plateau during the last glacial and interglacial periods[J]. Catena, 2000, 40(3):251-261. doi: 10.1016/S0341-8162(00)00090-4
[6]	刘东生. 黄土与环境[M]. 北京: 海洋出版社, 1985: 31-48.
	[ Liu Dongsheng. Loess and the environment[M]. Beijing: China Ocean Press, 1985: 31-48. ]
[7]	An Z S, Liu D T, Lu H Y, et al. The long-term paleomonsoon variation recorded by the loess-paleosol sequence in central China[J]. Quaternary International, 1990, 7-8:91-95. doi: 10.1016/1040-6182(90)90042-3
[8]	郭正堂, 彭淑贞, 郝青振, 等. 晚第三纪中国西北干旱化的发展及其与北极冰盖形成演化和青藏高原隆升的关系[J]. 第四纪研究, 1999, 19(6):556-567.
	[ Guo Zhengtang, Peng Shuzhen, Hao Qingzhen, et al. Late Tertiary development of aridification in northwestern China: Link with the Arctic ice-sheet formation and Tibetan uplifts[J]. Quaternary Sciences, 1999, 19(6):556-567. ]
[9]	安芷生, 孙东怀, 陈明扬, 等. 黄土高原红粘土序列与晚第三纪的气候事件[J]. 第四纪研究, 2000, 20(5):435-446.
	[ An Zhisheng, Sun Donghuai, Chen Mingyang, et al. Red clay sequences in Chinese Loess Plateau and recorded paleoclimate events of the Late Tertiary[J]. Quaternary Sciences, 2000, 20(5):435-446. ]
[10]	Guo Z T, Ruddiman W F, Hao Q Z, et al. Onset of Asian desertification by 22 Myr ago inferred from loess deposits in China[J]. Nature, 2002, 416(6877):159-163. doi: 10.1038/416159a
[11]	Ding Z L, Derbyshire E, Yang S L, et al. Stepwise expansion of desert environment across northern China in the past 3.5 Ma and implications for monsoon evolution[J]. Earth and Planetary Science Letters, 2005, 237(1-2):45-55. doi: 10.1016/j.epsl.2005.06.036
[12]	Rea D K, Snoeckx H, Joseph L H. Late Cenozoic eolian deposition in the North Pacific: Asian drying, Tibetan uplift, and cooling of the northern hemisphere[J]. Paleoceanography, 1998, 13(3):215-224. doi: 10.1029/98PA00123
[13]	Pettke T, Halliday A N, Rea D K. Cenozoic evolution of Asian climate and sources of Pacific seawater Pb and Nd derived from eolian dust of sediment core LL44-GPC3[J]. Paleoceanography and Paleoclimatology, 2002, 17(3):1031, doi: 10.1029/2001PA000673. doi: 10.1029/2001PA000673
[14]	Gehrels G, Kapp P, DeCelles P, et al. Detrital zircon geochronology of pre-Tertiary strata in the Tibetan-Himalayan orogen[J]. Tectonics, 2011, 30(5): TC5016, doi: 10.1029/2011tc002868. doi: 10.1029/2011tc002868
[15]	Sun D H, Bloemendal J, Rea D K, et al. Grain size distribution function of polymodal sediments in hydraulic and aeolian environments, and numerical partitioning of the sedimentary components[J]. Sedimentary Geology, 2002, 152(3-4):263-277. doi: 10.1016/S0037-0738(02)00082-9
[16]	Li G J, Chen J, Chen Y, et al. Dolomite as a tracer for the source regions of Asian dust[J]. Journal of Geophysical Research, 2007, 112(D17):D17201, doi: 10.1029/2007jd008676. doi: 10.1029/2007jd008676
[17]	Meng X, Liu L, Zhao W, et al. Distant Taklimakan Desert as an important source of aeoliandeposits on the Chinese Loess Plateau as evidenced by carbonate minerals[J]. Geophysical Research Letters, 2019, 46(9):4854-4862. doi: 10.1029/2018GL081551
[18]	Jeong G Y, Lee K S. A mineral tracer toward high-resolution dust provenance on the Chinese Loess Plateau: SEM, TEM, and sulfur isotopes of sulfate inclusions in biotite[J]. American Mineralogis, 2010, 95(1):64-72. doi: 10.2138/am.2010.3234
[19]	Lü T Y, Sun J M. Luminescence sensitivities of quartz grains from eolian deposits in northern China and their implications for provenance[J]. Quaternary Research, 2011, 76(2):181-189. doi: 10.1016/j.yqres.2011.06.015
[20]	Lü T Y, Sun J M, Feathers J K, et al. Spatiotemporal variations and implications of luminescence sensitivity of quartz grains on the Chinese Loess Plateau since the last interglaciation[J]. Quaternary Research, 2020, 99:10-14.
[21]	Sun J M. Provenance of loess material and formation of loess deposits on the Chinese Loess Plateau[J]. Earth and Planetary Science Letters, 2002, 203(3-4):845-859. doi: 10.1016/S0012-821X(02)00921-4
[22]	Liu C Q, Masuda A, Okada A, et al. Isotope geochemistry of Quaternary deposits from the arid lands in northern China[J]. Earth and Planetary Science Letters, 1994, 127(1-4):25-38. doi: 10.1016/0012-821X(94)90195-3
[23]	Rao W B, Yang J D, Chen J, et al. Sr-Nd isotope geochemistry of eolian dust of the arid-semiarid areas in China: Implications for loess provenance and monsoon evolution[J]. Science Bulletin, 2006, 51(12):1401-1412. doi: 10.1007/s11434-006-2008-1
[24]	Chen J, Li G J, Yang J D, et al. Nd and Sr isotopic characteristics of Chinese deserts: Implications for the provenances of Asian dust[J]. Geochimica et Cosmochimica Acta, 2007, 71(15):3904-3914. doi: 10.1016/j.gca.2007.04.033
[25]	Ferrat M, Weiss D J, Strekopytov S, et al. Improved provenance tracing of Asian dust sources using rare earth elements and selected trace elements for palaeomonsoon studies on the eastern Tibetan Plateau[J]. Geochimica et Cosmochimica Acta, 2011, 75(21):6374-6399. doi: 10.1016/j.gca.2011.08.025
[26]	Shi Z G, Liu X D. Distinguishing the provenance of fine-grained eolian dust over the Chinese Loess Plateau from a modelling perspective[J]. Tellus B, 2011, 63(5):959-970. doi: 10.1111/j.1600-0889.2011.00561.x
[27]	Zhang X Y, Gong S L, Zhao T L, et al. Sources of Asian dust and role of climate change versus desertification Asian dust emission[J]. Geophysical Research Letters, 2003, 30(24): doi: 10.1029/2003GL018206. doi: 10.1029/2003GL018206
[28]	张小曳. 有关中国黄土高原黄土物质的源区及其输送方式的再评述[J]. 第四纪研究, 2007, 27(2):181-186.
	[ Zhang Xiaoye. Review on sources and transport of loess materials on the Chinese Loess Plateau[J]. Quaternary Sciences, 2007, 27(2):181-186. ]
[29]	Li Y R, Shi W H, Aydin A, et al. Loess genesis and worldwide distribution[J]. Earth-Science Reviews, 2019, 201:102947, doi: 10.10 16/j.earscirev.2019.102947. doi: 10.10 16/j.earscirev.2019.102947
[30]	Wang F, Sun D H, Chen F H, et al. Formation and evolution of the Badain Jaran Desert, north China, as revealed by a drill core from the desert centre and by geological survey[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2015, 426:139-158. doi: 10.1016/j.palaeo.2015.03.011
[31]	Fan Y X, Mou X S, Wang Y D, et al. Quaternary paleoenvironmental evolution of the Tengger Desert and its implications for the provenance of the loess of the Chinese Loess Plateau[J]. Quaternary Science Reviews, 2018, 197:21-34. doi: 10.1016/j.quascirev.2018.08.002
[32]	Zheng H B, Wei X C, Tada R, et al. Late Oligocene-early Miocene birth of the Taklimakan Desert[J]. Proceedings of the National Academy of Sciences, 2015, 112(25):7662-7667. doi: 10.1073/pnas.1424487112
[33]	Rittner M, Vermeesch P, Carter A, et al. The provenance of Taklamakan Desert sand[J]. Earth and Planetary Science Letters, 2016, 437:127-137. doi: 10.1016/j.epsl.2015.12.036
[34]	Stevens T, Palk C, Carter A, et al. Assessing the provenance of loess and desert sediments in northern China using U-Pb dating and morphology of detrital zircons[J]. Geological Society of America Bulletin, 2010, 122(7-8):1331-1344. doi: 10.1130/B30102.1
[35]	Stevens T, Carter A, Watson T P, et al. Genetic linkage between the Yellow River, the Mu Us Desert and the Chinese Loess Plateau[J]. Quaternary Science Reviews, 2013, 78(19):355-368. doi: 10.1016/j.quascirev.2012.11.032
[36]	Pullen A, Kapp P, Mccallister A T, et al. Qaidam Basin and northern Tibetan Plateau as dust sources for the Chinese Loess Plateau and paleoclimatic implications[J]. Geology, 2011, 39(11):1031-1034. doi: 10.1130/G32296.1
[37]	Fan Y X, Li Z J, Wang F, et al. Provenance variations of the Tengger Desert since 2.35 Ma and its linkage with the northern Tibetan Plateau: Evidence from U-Pb age spectra of detrital zircons[J]. Quaternary Science Reviews, 2019, 223:105916, doi: 10.1016/j.quascirev.2019.105916. doi: 10.1016/j.quascirev.2019.105916
[38]	Xiao G Q, Zong K Q, Li G J, et al. Spatial and glacial-interglacial variations in provenance of the Chinese Loess Plateau[J]. Geophysical Research Letters, 2012, 39(20):L20715, doi: 10.1029/2012 GL053304. doi: 10.1029/2012 GL053304
[39]	Che X D, Li G J. Binary sources of loess on the Chinese Loess Plateau revealed by U-Pb ages of zircon[J]. Quaternary Research, 2013, 80(3):545-551. doi: 10.1016/j.yqres.2013.05.007
[40]	Bird A, Stevens T, Rittner M, et al. Quaternary dust source variation across the Chinese Loess Plateau[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2015, 435:254-264. doi: 10.1016/j.palaeo.2015.06.024
[41]	Nie J S, Stevens T, Rittner M, et al. Loess Plateau storage of northeastern Tibetan Plateau-derived Yellow River sediment[J]. Nature Communications, 2015, 6(1):8511, doi: 10.1038/ncomms9511. doi: 10.1038/ncomms9511
[42]	Zhang H Z, Lu H Y, Stevens T, et al. Expansion of dust provenance and aridification of Asia since ~7.2 Ma revealed by detrital zircon U-Pb dating[J]. Geophysical Research Letters, 2018, 45(24):13437-13448.
[43]	马榕, 张婉莹, 何梦颖. 基于碎屑锆石U-Pb年龄对黄土高原黄土的空间物源差异分析[J]. 海洋地质前沿, 2019, 35(1):35-42.
	[ Ma Rong, Zhang Wanying, He Mengying. Spatial provenance difference of the loess on Loess Plateau based on detrital zircons U-Pb ages[J]. Marine Geology Frontiers, 2019, 35(1):35-42. ]
[44]	Fenn K, Stevens T, Bird A, et al. Insights into the provenance of the Chinese Loess Plateau from joint zircon U-Pb and garnet geochemical analysis of last glacial loess[J]. Quaternary Research: An Interdisciplinary Journal, 2017, 89(3):645-659.
[45]	Zhang X Y, Arimoto R, An Z S. Dust emission from Chinese desert sources linked to variations in atmospheric circulation[J]. Journal of Geophysical Research Atmospheres, 1997, 102(D23):28041-28047. doi: 10.1029/97JD02300
[46]	Sun Y B, Tada R, Chen J, et al. Tracing the provenance of fine-grained dust deposited on the central Chinese loess plateau[J]. Geophysical Research Letters, 2008, 35(1):L01804, doi: 10.1029/2007gl031672. doi: 10.1029/2007gl031672
[47]	孙博亚, 张云翔, 弓虎军, 等. 洛川黄土碎屑锆石的粒度特征及其古气候意义[J]. 西北大学学报: 自然科学版, 2011, 41(1):119-126.
	[ Sun Boya, Zhang Yunxiang, Gong Hujun, et al. The grain size of the detrital zircon of Luochuan and its paleoclimate implication[J]. Journal of Northwest University: Natural Science Edition, 2011, 41(1):119-126. ]
[48]	Gallet S, Jahn B, Torii M. Geochemical characterization of the Luochuan loess-paleosol sequence, China, and paleoclimatic implications[J]. Chemical Geology, 1996, 133(1-4):67-88. doi: 10.1016/S0009-2541(96)00070-8
[49]	Jahn B M, Gallet S, Han J M. Geochemistry of the Xining, Xifeng and Jixian sections, Loess Plateau of China: Eolian dust provenance and paleosol evolution during the last 140 ka[J]. Chemical Geology, 2001, 178(1-4):71-94. doi: 10.1016/S0009-2541(00)00430-7
[50]	杨杰东, 陈骏, 张兆峰, 等. 距今7 Ma以来甘肃灵台剖面Nd和Sr同位素特征[J]. 地球化学, 2005, 34(1):1-6.
	[ Yang Jiedong, Chen Jun, Zhang Zhaofeng, et al. Variations in ¹⁴³Nd/¹⁴⁴Nd and ⁸⁷Sr/⁸⁶Sr of Lingtai profile over the past 7 Ma[J]. Geochimica, 2005, 34(1):1-6. ]
[51]	Jeong G Y, Hillier S, Kemp R A. Changes in mineralogy of loess-paleosol sections across the Chinese Loess Plateau[J]. Quaternary Research, 2011, 75(1):245-255. doi: 10.1016/j.yqres.2010.09.001
[52]	Nie J S, Peng W B. Automated SEM-EDS heavy mineral analysis reveals no provenance shift between glacial loess and interglacial paleosol on the Chinese Loess Plateau[J]. Aeolian Research, 2014, 13:71-75. doi: 10.1016/j.aeolia.2014.03.005
[53]	Licht A, Pullen A, Kapp P, et al. Eolian cannibalism: Reworked loess and fluvial sediment as the main sources of the Chinese Loess Plateau[J]. Geological Society of America Bulletin, 2016, 128(5-6): B31375.1, doi: 10.1130/B31375.1. doi: 10.1130/B31375.1
[54]	Pullen A, Ibáñez-Mejía M, Gehrels G E, et al. What happens when n=1000? Creating large-n geochronological datasets with LA-ICP-MS for geologic investigations[J]. Journal of Analytical Atomic Spectrometry, 2014, 29(6):971-980. doi: 10.1039/C4JA00024B
[55]	Vermeesch P. How many grains are needed for a provenance study?[J]. Earth and Planetary Science Letters, 2004, 224(3-4):441-451. doi: 10.1016/j.epsl.2004.05.037
[56]	Xiong J G, Zhang H P, Zhao X D, et al. Origin of the youngest Cenozoic aeolian deposits in the southeastern Chinese Loess Plateau[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2020, 561, doi: 10.1016/j.palaeo.2020.110080. doi: 10.1016/j.palaeo.2020.110080
[57]	Sun J M. Nd and Sr isotopic variations in Chinese eolian deposits during the past 8 Ma: Implications for provenance change[J]. Earth and Planetary Science Letters, 2005, 240(2):454-466. doi: 10.1016/j.epsl.2005.09.019
[58]	Alley R B, Andrews J T, Brigham-Grette J, et al. History of the Greenland Ice Sheet: Paleoclimatic insights[J]. Quaternary Science Reviews, 2010, 29(15-16):1728-1756. doi: 10.1016/j.quascirev.2010.02.007
[59]	Polyak L, Alley R B, Andrews J T, et al. History of sea ice in the Arctic[J]. Quaternary Science Reviews, 2010, 29(15-16):1757-1778. doi: 10.1016/j.quascirev.2010.02.010
[60]	Raymo M E, Huybers P. Unlocking the mysteries of the ice ages[J]. Nature, 2008, 451(7176):284-285. doi: 10.1038/nature06589
[61]	Guo Z T, Sun B, Zhang Z S, et al. A major reorganization of Asian climate regime by the Early Miocene[J]. Climate of the Past, 2008, 4(3):153-174. doi: 10.5194/cp-4-153-2008
[62]	Li J J, Fang X M, Van der Voo R, et al. Magnetostratigraphic dating of river terraces: Rapid and intermittent incision by the Yellow River of the northeastern margin of the Tibetan Plateau during the Quaternary[J]. Journal of Geophysical Research Atmospheres, 1997, 102(B5):10121-10132. doi: 10.1029/97JB00275
[63]	Li J J, Fang X M, Van der Voo R, et al. Late Cenozoic magnetostratigraphy (11-0 Ma) of the Dongshanding and Wangjiashan sections in the Longzhong Basin, western China[J]. Geologie En Mijnbouw, 1997, 76(1-2):121-134.
[64]	Li J J, Fang X M, Song C H, et al. Late Miocene-Quaternary rapid stepwise uplift of the NE Tibetan Plateau and its effects on climatic and environmental changes[J]. Quaternary Research, 2014, 81(3):400-423. doi: 10.1016/j.yqres.2014.01.002
[65]	Lu H Y, Vandenberghe J, An Z S. Aeolian origin and palaeoclimatic implications of the ‘red clay’ (north China) as evidenced by grain-size distribution[J]. Journal of Quaternary Science, 2001, 16(1):89-97. doi: 10.1002/(ISSN)1099-1417
[66]	Ding Z L, Sun J M, Yang S L, et al. Preliminary magnetostratigraphy of a thick eolian red clay-loess sequence at Lingtai, the Chinese Loess Plateau[J]. Geophysical Research Letters, 1998, 25(8):1225-1228. doi: 10.1029/98GL00836
[67]	Ding Z L, Sun J M, Liu T S, et al. Wind-blown origin of the Pliocene red clay formation in the central Loess Plateau, China[J]. Earth and Planetary Science Letters, 1998, 161(1-4):135-143. doi: 10.1016/S0012-821X(98)00145-9
[68]	Nie J S, Peng W B, Moller A, et al. Provenance of the upper Miocene-Pliocene red clay deposits of the Chinese Loess Plateau[J]. Earth and Planetary Science Letters, 2014, 407:35-47. doi: 10.1016/j.epsl.2014.09.026
[69]	Pan F, Li J X, Xu Y, et al. Provenance of Neogene eolian red clay in the Altun region of western China: Insights from U-Pb detrital zircon age data[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2016, 459:488-494. doi: 10.1016/j.palaeo.2016.07.020
[70]	Pan F, Li J X, Xu Y, et al. Uplift of the Lyuliang Mountains at ca. 5.7 Ma: Insights from provenance of the Neogene eolian red clay of the eastern Chinese Loess Plateau[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2018, 502:63-73. doi: 10.1016/j.palaeo.2018.04.024
[71]	Shang Y, Beets C J, Tang H, et al. Variations in the provenance of the Late Neogene red clay deposits in northern China[J]. Earth and Planetary Science Letters, 2016, 439:88-100. doi: 10.1016/j.epsl.2016.01.031

Understanding and prospects of provenance and time-spatial differences in the Loess Plateau based on detrital zircon chronology

RichHTML

PDF (PC)

Like

Knowledge

Abstract

Cite this article

share this article

Figures/Tables 6

References 71

Related Articles 15

Metrics

Comments

Recommended 0

[1]	REN Taotao,LI Shuangshuang,DUAN Keqin,HE Jinping. Spatiotemporal variation characteristics and influencing factors of heat wave and precipitation deficit flash drought in the Loess Plateau [J]. Arid Land Geography, 2023, 46(3): 360-370.
[2]	AN Bin,XIAO Weiwei,LIU Yufeng,LIU Quanyu. Temporal and spatial evolution of relative humidity in the Loess Plateau during 1955—2021 [J]. Arid Land Geography, 2023, 46(12): 1939-1950.
[3]	ZHUO Jing,HU Hao,HE Huijuan,WANG Zhi,YANG Chengrui. Spatiotemporal variation and driving factors of ecological vulnerability in the Loess Plateau of northern Shaanxi [J]. Arid Land Geography, 2023, 46(11): 1768-1777.
[4]	QIAN Wei, WANG Chun, DAI Wen, LU Wangda, LI Min, TAO Yu, LI Mengqi. Extraction of check dam system in small watershed of Loess Plateau based on deep learning and OBIA [J]. Arid Land Geography, 2023, 46(11): 1803-1812.
[5]	SHA Guoliang,WEI Tianxing,CHEN Yuxuan,FU Yanchao,REN Kang. Characteristics of soil particle size distribution of typical plant communities on the hilly areas of Loess Plateau [J]. Arid Land Geography, 2022, 45(4): 1224-1234.
[6]	YE Wenli,YANG Xinjun,WU Kongsen,WANG Yin. Spatio-temporal characteristics and influencing factors of social-ecological system resilience in the Loess Plateau [J]. Arid Land Geography, 2022, 45(3): 912-924.
[7]	JI Zhenxia,HOU Qingqing,PEI Tingting,CHEN Ying,XIE Baopeng,WU Huawu. Sensitive response of vegetation phenology to seasonal drought in the Loess Plateau [J]. Arid Land Geography, 2022, 45(2): 557-565.
[8]	SUN Jianwu,GAO Junbo,MA Zhifei,YU Chao,ZHANG Xinyi. Comparison of spatial poverty trap formation mechanisms in different geographical environments: A case of Dabie Mountains and Loess Plateau [J]. Arid Land Geography, 2022, 45(2): 650-659.
[9]	TIAN Darui,TANG Hao,TAN Jingbin. Suitable spatial patterns for settlements in hilly-gully region of the Loess Plateau in northern Shaanxi: A case of Donggou, Mizhi County [J]. Arid Land Geography, 2022, 45(1): 263-276.
[10]	JIANG Li,WEI Tianxing,LI Yiran,WEI Anqi. Effects of topographical factors on tree species distribution of shelter forest in Loess hilly region of northern Shaanxi [J]. Arid Land Geography, 2021, 44(6): 1763-1771.
[11]	AN Bin,XIAO Weiwei,ZHANG Shulan,ZHU Ni,ZHANG Jiandong. Spatial and temporal characteristics of surface temperature in the Loess Plateau during 1961—2017 [J]. Arid Land Geography, 2021, 44(3): 778-785.
[12]	WANG Jun,LI Guang,NIE Zhigang,DONG Lixia,YAN Lijuan. Simulation study of response of spring wheat yield to drought stress in the Loess Plateau of central Gansu [J]. Arid Land Geography, 2021, 44(2): 494-506.
[13]	YAO Xueling,YANG Guojing,WANG Shuai,GUO Xiujiang. Soil moisture response and stability to rainfall in different depths in Loess Plateau [J]. Arid Land Geography, 2021, 44(2): 507-513.
[14]	MIAO Yu,GAO Guanlong,LI Wei. Environmental response and modeling of stomatal conductance of apple trees on the Loess Plateau [J]. Arid Land Geography, 2021, 44(2): 525-533.
[15]	LI Yuxin,XUE Dongqian,MA Beibei,DONG Chaoyang. Spatial evolution and remote characteristics of rural poverty in the Loess Plateau, China [J]. Arid Land Geography, 2021, 44(2): 534-543.