This article examines the relationship between headwear design and overall clothing styling,emphasizing the importance of headwear in conveying personal style and cultural identity.It traces the evolution of Chinese a...This article examines the relationship between headwear design and overall clothing styling,emphasizing the importance of headwear in conveying personal style and cultural identity.It traces the evolution of Chinese and Western headwear throughout history,highlighting the interplay between headwear and the wearer's personal charac-teristics,life events,and cultural background.The article concludes by emphasizing that headwear design is not only a reflection of fashion,but also a manifestation of cultural depth and individuality.展开更多
Soil bulk density is a basic but important physic soil property related to soil porosity,soil moisture and hydraulic conductivity,which is crucial to soil quality assessment and land use management.In this study,we ev...Soil bulk density is a basic but important physic soil property related to soil porosity,soil moisture and hydraulic conductivity,which is crucial to soil quality assessment and land use management.In this study,we evaluated the spatial variability of soil bulk density in the 0–20,20–40,40–60 and 60–100 cm layers as well as its affecting factors in Southwest China’s agricultural intensive area.Results indicated the mean value of surface soil bulk density(0–20 cm)was 1.26 g cm^(–3),significantly lower than that of subsoil(20–100 cm).No statistical difference existed among the subsoil with a mean soil bulk density of 1.54 g cm^(–3).Spatially,soil bulk density played a similar spatial pattern in soil profile,whereas obvious differences were found in details.The nugget effects for soil bulk density in the 0–20 and 20–40 cm layers were 27.22 and27.02%while 12.06 and 3.46%in the 40–60 and 60–100 cm layers,respectively,gradually decreasing in the soil profile,indicating that the spatial variability of soil bulk density above 40 cm was affected by structural and random factors while dominated by structural factors under 40 cm.Soil organic matter was the controlling factor on the spatial variability of soil bulk density in each layer.Land use and elevation were another two dominated factor controlling the spatial variability of soil bulk density in the 0–20 and 40–60 cm layers,respectively.Soil genus was one of the dominated factors controlling the spatial variability of soil bulk below 40 cm.展开更多
The western Kunlun orogen in the northwest Tibet Plateau is related to subduction and collision of Proto-and Paleo-Tethys from early Paleozoic to early Mesozoic. This paper presents new LA-ICPMS zircon U-Pb ages and L...The western Kunlun orogen in the northwest Tibet Plateau is related to subduction and collision of Proto-and Paleo-Tethys from early Paleozoic to early Mesozoic. This paper presents new LA-ICPMS zircon U-Pb ages and Lu-Hf isotopes, whole-rock major and trace elements, and Sr–Nd isotopes of two Ordovician granitoid plutons(466–455 Ma) and their Silurian mafic dikes(～436 Ma) in the western Kunlun orogen. These granitoids show peraluminous high-K calcalkaline characteristics, with(^(87)Sr/^(86)Sr)_i value of 0.7129–0.7224, ε_(Nd)(t) values of -9.3 to -7.0 and zircon ε_(Hf)(t) values of -17.3 to -0.2, indicating that they were formed by partial melting of ancient lower-crust(metaigneous rocks mixed with metasedimentary rocks) with some mantle materials in response to subduction of the Proto-Tethyan Ocean and following collision. The Silurian mafic dikes were considered to have been derived from a low degree of partial melting of primary mafic magma. These mafic dikes show initial ^(87)Sr/^(86)Sr ratios of 0.7101–0.7152 and ε_(Nd)(t) values of -3.8 to -3.4 and zircon ε_(Hf)(t) values of -8.8 to -4.9, indicating that they were derived from enriched mantle in response to post-collisional slab break-off. Combined with regional geology, our new data provide valuable insight into late evolution of the Proto-Tethys.展开更多
A process-based 3D numerical model for surfzone hydrodynamics and beach evolution was established. Comparisons between the experimental data and model results proved that the model could effectively describe the hydro...A process-based 3D numerical model for surfzone hydrodynamics and beach evolution was established. Comparisons between the experimental data and model results proved that the model could effectively describe the hydrodynamics, sediment transport feature and sandbar migration process in the surfzone with satisfactory precision. A series of numerical simulations on the wave breaking and shoaling up to a barred beach were carried out based on the model system. Analyzed from the model results, the wave-induced current system in the surfzone consists of two major processes, which are the phase-averaged undertow caused by wave breaking and the net drift caused by both of the nonlinear wave motion and surface roller effect. When storm waves come to the barred beach, the strong offshore undertow along the beach suppresses the onshore net drift, making the initial sandbar migrate to the seaside. Under the condition of calm wave environment, both the undertow and net drift flow to the shoreline at the offshore side of the sandbar, and then push the initial sandbar to the shoreline. The consideration of surface roller has significant impact on the modeling results of the sandbar migration. As the roller transfer rate increases, the sandbar moves onshore especially under the storm wave condition.展开更多
The lack of preserved basement results in uncertain placements of many terranes in Southeast Asia.Here,we flag the first evidence of the oldest basement in Indonesian Borneo,which can help locate terranes in Borneo on...The lack of preserved basement results in uncertain placements of many terranes in Southeast Asia.Here,we flag the first evidence of the oldest basement in Indonesian Borneo,which can help locate terranes in Borneo on the northern margin of Gondwana in the early Paleozoic and explain the regional tectonic setting of the island.Two schist samples from the Embuoi Complex in the Semitau Block,Northwest Kalimantan yielded zircon U-Pb dates of 453.3±1.9 Ma and 462.4±2.6 Ma,respectively,representing the formation time of the protolith.Petrographic,internal structural and high Th/U ratios of zircons indicate that the protolith of schists is of magmatic origin.The zircons haveεHf(t)values of−4.1 to+1.1 and Hf model ages of 1.37–1.69 Ga,indicating they were derived from a mixed source of juvenile crust with old components.By comparison of zircon age distribution,two-stage Hf model ages andεHf(t)variations of the early Paleozoic igneous rocks from Semitau with those of South China,Tengchong–Baoshan,and Indochina,the Semitau Block was most likely a part of or placed next to the Indochina Block of northern Gondwana during the early Paleozoic.Such a similar tectono-magmatic pattern on northern Gondwana formed a prolonged early Paleozoic arc-related belt associated with subduction of the Proto-Tethyan Ocean.展开更多
Orogens can generally be divided into two types:accretionary and collisional.The fundamental differences in deep-crustal compositions and architecture from accretion to collision and how to identify them is not well u...Orogens can generally be divided into two types:accretionary and collisional.The fundamental differences in deep-crustal compositions and architecture from accretion to collision and how to identify them is not well understood.This is one of the major aims of the IGCP 662 project(www.igcp662.org.cn).展开更多
Altaids:The conception The Altaids is tectonically sandwiched between the Baltica and Siberia cratons to the north and the Tarim and North China cratons to the south(Sengor et al.,1993).This huge orogen has been also ...Altaids:The conception The Altaids is tectonically sandwiched between the Baltica and Siberia cratons to the north and the Tarim and North China cratons to the south(Sengor et al.,1993).This huge orogen has been also called the Altaid collage(Yakubchuk,2004),Central Asian Orogenic Belt(CAOB)(Jahn et al.,2000a),or Central Asian Orogenic System(Briggs et al.,2007).Long before these terms,the Altaids even had been called the Asian Foldbelt,Ural-Mongolian Foldbelt,or Ural-Amurian Foldbelt,mostly by the former Soviet Union scientists(Yakubchuk,2004).展开更多
目的:分析宫颈高危型人乳头瘤病毒(high risk human papilloma virus,HR-HPV)感染患者中医体质类型分布特点,为中医药调理体质防治宫颈HR-HPV感染提供依据。方法:选择2019年1月至2020年12月就诊于河南中医药大学第一附属医院妇科门诊及...目的:分析宫颈高危型人乳头瘤病毒(high risk human papilloma virus,HR-HPV)感染患者中医体质类型分布特点,为中医药调理体质防治宫颈HR-HPV感染提供依据。方法:选择2019年1月至2020年12月就诊于河南中医药大学第一附属医院妇科门诊及体检中心的420例宫颈HR-HPV感染者作为观察组,选择420例同时段宫颈HR-HPV检测阴性者为对照组。分析两组中医体质类型分布情况、观察组不同年龄段中医体质类型分布情况、观察组不同HR-HPV基因型别中医体质类型。结果:观察组中医体质分布依次为:痰湿质(30.50%)>湿热质(19.00%)>平和质(15.50%)>阳虚质(14.80%)>气虚质(10.00%)>阴虚质(5.90%)>瘀血质(2.70%)>气郁质(1.70%);对照组中医体质分布依次为:平和质(73.30%)>湿热质(8.40%)>阴虚质(5.70%)>痰湿质(4.50%)>气虚质(4.30%)>阳虚质/瘀血质(1.80%)>气郁质(0.20%)。两组中医体质类型比较,差异具有统计学意义(P<0.05),其中,痰湿质、湿热质、阳虚质、气虚质,两组间比较,差异具有统计学意义(P<0.001)。观察组体质类型居前三位的是痰湿质、湿热质、阳虚质,占全部体质类型的64.30%。对照组平和质324例,占比73.50%,观察组平和质81例,占比15.50%,两组间比较,差异具有统计学意义(P<0.001)。观察组中,痰湿质、阳虚质、阴虚质主要见于46~55岁,湿热质、气虚质、气郁质主要见于36~45岁,组间比较差异具有统计学意义(P<0.05)。两组宫颈HR-HPV16、18型和非16、18型中医体质比较,差异无统计学意义(P>0.05)。结论:痰湿质、湿热质、阳虚质为宫颈HR-HPV感染人群的易感体质;痰湿质、湿热质、阳虚质与年龄具有相关性,痰湿质多见于36~45岁,湿热质、阳虚质多见于46~55岁,HR-HPV基因型别与中医体质类型之间无明显相关性。展开更多
文摘This article examines the relationship between headwear design and overall clothing styling,emphasizing the importance of headwear in conveying personal style and cultural identity.It traces the evolution of Chinese and Western headwear throughout history,highlighting the interplay between headwear and the wearer's personal charac-teristics,life events,and cultural background.The article concludes by emphasizing that headwear design is not only a reflection of fashion,but also a manifestation of cultural depth and individuality.
基金supported by the National Natural Science Foundation of China (4120124)the Science Fund of the Education Department of Sichuan Province, China (16ZB0048)
文摘Soil bulk density is a basic but important physic soil property related to soil porosity,soil moisture and hydraulic conductivity,which is crucial to soil quality assessment and land use management.In this study,we evaluated the spatial variability of soil bulk density in the 0–20,20–40,40–60 and 60–100 cm layers as well as its affecting factors in Southwest China’s agricultural intensive area.Results indicated the mean value of surface soil bulk density(0–20 cm)was 1.26 g cm^(–3),significantly lower than that of subsoil(20–100 cm).No statistical difference existed among the subsoil with a mean soil bulk density of 1.54 g cm^(–3).Spatially,soil bulk density played a similar spatial pattern in soil profile,whereas obvious differences were found in details.The nugget effects for soil bulk density in the 0–20 and 20–40 cm layers were 27.22 and27.02%while 12.06 and 3.46%in the 40–60 and 60–100 cm layers,respectively,gradually decreasing in the soil profile,indicating that the spatial variability of soil bulk density above 40 cm was affected by structural and random factors while dominated by structural factors under 40 cm.Soil organic matter was the controlling factor on the spatial variability of soil bulk density in each layer.Land use and elevation were another two dominated factor controlling the spatial variability of soil bulk density in the 0–20 and 40–60 cm layers,respectively.Soil genus was one of the dominated factors controlling the spatial variability of soil bulk below 40 cm.
基金funded by the Strategic Priority Research Program of Chinese Academy of Sciences,Grant No.XDA20070304the Fundamental Research Funds for the Chinese Academy of Geological Sciences(YYWF201601)+1 种基金projects of China Geological Survey(DD20160004,20160083-1,12120115000801,121201101000150014)the National Natural Science Foundation of China(grant 41772232)
文摘The western Kunlun orogen in the northwest Tibet Plateau is related to subduction and collision of Proto-and Paleo-Tethys from early Paleozoic to early Mesozoic. This paper presents new LA-ICPMS zircon U-Pb ages and Lu-Hf isotopes, whole-rock major and trace elements, and Sr–Nd isotopes of two Ordovician granitoid plutons(466–455 Ma) and their Silurian mafic dikes(～436 Ma) in the western Kunlun orogen. These granitoids show peraluminous high-K calcalkaline characteristics, with(^(87)Sr/^(86)Sr)_i value of 0.7129–0.7224, ε_(Nd)(t) values of -9.3 to -7.0 and zircon ε_(Hf)(t) values of -17.3 to -0.2, indicating that they were formed by partial melting of ancient lower-crust(metaigneous rocks mixed with metasedimentary rocks) with some mantle materials in response to subduction of the Proto-Tethyan Ocean and following collision. The Silurian mafic dikes were considered to have been derived from a low degree of partial melting of primary mafic magma. These mafic dikes show initial ^(87)Sr/^(86)Sr ratios of 0.7101–0.7152 and ε_(Nd)(t) values of -3.8 to -3.4 and zircon ε_(Hf)(t) values of -8.8 to -4.9, indicating that they were derived from enriched mantle in response to post-collisional slab break-off. Combined with regional geology, our new data provide valuable insight into late evolution of the Proto-Tethys.
基金financially supported by the National Key Research and Development Program of China(Grant No.2016YFC0402603)the National Natural Science Foundation of China(Grant Nos.51779112,51509119,and 51609029)+2 种基金the Project of Tianjin Natural Science Foundation(Grant No.16JCQNJC06900)the Open Project of State Key Laboratory of Hydrology-Water Resources and Hydraulic Engineering(Grant No.2014492211)the Fundamental Research Funds for the Central Public Welfare Research Institutes(Grant Nos.TKS170101and TKS170202)
文摘A process-based 3D numerical model for surfzone hydrodynamics and beach evolution was established. Comparisons between the experimental data and model results proved that the model could effectively describe the hydrodynamics, sediment transport feature and sandbar migration process in the surfzone with satisfactory precision. A series of numerical simulations on the wave breaking and shoaling up to a barred beach were carried out based on the model system. Analyzed from the model results, the wave-induced current system in the surfzone consists of two major processes, which are the phase-averaged undertow caused by wave breaking and the net drift caused by both of the nonlinear wave motion and surface roller effect. When storm waves come to the barred beach, the strong offshore undertow along the beach suppresses the onshore net drift, making the initial sandbar migrate to the seaside. Under the condition of calm wave environment, both the undertow and net drift flow to the shoreline at the offshore side of the sandbar, and then push the initial sandbar to the shoreline. The consideration of surface roller has significant impact on the modeling results of the sandbar migration. As the roller transfer rate increases, the sandbar moves onshore especially under the storm wave condition.
基金supported by the National Natural Science Foundation of China(Grant Nos.41802243,41772232 and 42161144007)the fund from the Key Laboratory of Deep-Earth Dynamics of Ministry of Natural Resources(Grant No.J1901-27)+1 种基金the Outlay Research Fund of the Institute of Geology,Chinese Academy of Geological Sciences(Grant No.J2008)the China Geological Survey Program(Grant Nos.DD20190358,DD20221646 and DD20190001).This study is a contribution to International Geoscience Programme(IGCP)project 662“Orogenic architecture and crustal growth from accretion to collision.”We thank two anonymous reviewers for their helpful suggestions and constructive comments that helped us to improve this manuscript.
文摘The lack of preserved basement results in uncertain placements of many terranes in Southeast Asia.Here,we flag the first evidence of the oldest basement in Indonesian Borneo,which can help locate terranes in Borneo on the northern margin of Gondwana in the early Paleozoic and explain the regional tectonic setting of the island.Two schist samples from the Embuoi Complex in the Semitau Block,Northwest Kalimantan yielded zircon U-Pb dates of 453.3±1.9 Ma and 462.4±2.6 Ma,respectively,representing the formation time of the protolith.Petrographic,internal structural and high Th/U ratios of zircons indicate that the protolith of schists is of magmatic origin.The zircons haveεHf(t)values of−4.1 to+1.1 and Hf model ages of 1.37–1.69 Ga,indicating they were derived from a mixed source of juvenile crust with old components.By comparison of zircon age distribution,two-stage Hf model ages andεHf(t)variations of the early Paleozoic igneous rocks from Semitau with those of South China,Tengchong–Baoshan,and Indochina,the Semitau Block was most likely a part of or placed next to the Indochina Block of northern Gondwana during the early Paleozoic.Such a similar tectono-magmatic pattern on northern Gondwana formed a prolonged early Paleozoic arc-related belt associated with subduction of the Proto-Tethyan Ocean.
基金supported frnancially by the NSFC projects(Grant Nos.U1403291,41802074,41830216,41572052)projects of the China Geological Survey(Grant Nos.1212011120477,1212010611803,1212010811033,12120113096500,12120113094000 and DD20160123)+1 种基金the IGCP 662 project’Orogenic Architecture and Crustal Growth from Accretion to Collision’the IUGS Big Science Program’Deep-time Digital Earth(DDE)’.
文摘Orogens can generally be divided into two types:accretionary and collisional.The fundamental differences in deep-crustal compositions and architecture from accretion to collision and how to identify them is not well understood.This is one of the major aims of the IGCP 662 project(www.igcp662.org.cn).
文摘Altaids:The conception The Altaids is tectonically sandwiched between the Baltica and Siberia cratons to the north and the Tarim and North China cratons to the south(Sengor et al.,1993).This huge orogen has been also called the Altaid collage(Yakubchuk,2004),Central Asian Orogenic Belt(CAOB)(Jahn et al.,2000a),or Central Asian Orogenic System(Briggs et al.,2007).Long before these terms,the Altaids even had been called the Asian Foldbelt,Ural-Mongolian Foldbelt,or Ural-Amurian Foldbelt,mostly by the former Soviet Union scientists(Yakubchuk,2004).
文摘目的:分析宫颈高危型人乳头瘤病毒(high risk human papilloma virus,HR-HPV)感染患者中医体质类型分布特点,为中医药调理体质防治宫颈HR-HPV感染提供依据。方法:选择2019年1月至2020年12月就诊于河南中医药大学第一附属医院妇科门诊及体检中心的420例宫颈HR-HPV感染者作为观察组,选择420例同时段宫颈HR-HPV检测阴性者为对照组。分析两组中医体质类型分布情况、观察组不同年龄段中医体质类型分布情况、观察组不同HR-HPV基因型别中医体质类型。结果:观察组中医体质分布依次为:痰湿质(30.50%)>湿热质(19.00%)>平和质(15.50%)>阳虚质(14.80%)>气虚质(10.00%)>阴虚质(5.90%)>瘀血质(2.70%)>气郁质(1.70%);对照组中医体质分布依次为:平和质(73.30%)>湿热质(8.40%)>阴虚质(5.70%)>痰湿质(4.50%)>气虚质(4.30%)>阳虚质/瘀血质(1.80%)>气郁质(0.20%)。两组中医体质类型比较,差异具有统计学意义(P<0.05),其中,痰湿质、湿热质、阳虚质、气虚质,两组间比较,差异具有统计学意义(P<0.001)。观察组体质类型居前三位的是痰湿质、湿热质、阳虚质,占全部体质类型的64.30%。对照组平和质324例,占比73.50%,观察组平和质81例,占比15.50%,两组间比较,差异具有统计学意义(P<0.001)。观察组中,痰湿质、阳虚质、阴虚质主要见于46~55岁,湿热质、气虚质、气郁质主要见于36~45岁,组间比较差异具有统计学意义(P<0.05)。两组宫颈HR-HPV16、18型和非16、18型中医体质比较,差异无统计学意义(P>0.05)。结论:痰湿质、湿热质、阳虚质为宫颈HR-HPV感染人群的易感体质;痰湿质、湿热质、阳虚质与年龄具有相关性,痰湿质多见于36~45岁,湿热质、阳虚质多见于46~55岁,HR-HPV基因型别与中医体质类型之间无明显相关性。
