Surface air temperature change in the Wuyi Mountains,southeast China

Detecting changes in surface air temperature in mid-and low-altitude mountainous regions is essential for a comprehensive understanding of warming trend with altitude.We use daily surface air temperature data from 64 meteorological stations in Wuyi Mountains and its adjacent regions to analyze the spatio-temporal patterns of temperature change.The results show that Wuyi Mountains have experienced significant warming from 1961 to 2018.The warming trend of the mean temperature is 0.20℃/decade,the maximum temperature is 0.17℃/decade,and the minimum temperature is 0.26℃/decade.In 1961-1990,more than 63%of the stations showed a decreasing trend in annual mean temperature,mainly because the maximum temperature decreased during this period.However,in 1971-2000,1981-2010 and 1991-2018,the maximum,minimum and mean temperatures increased.The fastest increasing trend of mean temperature occurred in the southeastern coastal plains,the quickest increasing trend of maximum temperature occurred in the northwestern mountainous region,and the increase of minimum temperature occurred faster in the southeastern coastal and northwestern mountainous regions than that in the central area.Meanwhile,this study suggests that elevation does not affect warming in the Wuyi Mountains.These results are beneficial for understanding climate change in humid subtropical middle and low mountains.

Comparison of Soil Organic Carbon Content in Different Soil Types of Wuyi Mountains

[Objective] The aim was to explore the soil organic carbon（SOC）content from different types of soil and its influencing factors.[Method] Soil samples were collected from Wuyi Mountains,and the physical and chemical properties were measured and the relationship between SOC content and soil physical and chemical properties,altitude,average annual temperature was analyzed.[Result] SOC content ranged from 14.91 to 112.34 g/kg,and SOC content was significant positive correlated with available nutrients（available N,P and K）and total nitrogen.[Conclusion] This study indicated that the physical and chemical properties of soil,altitude,average annual temperature had a significant influence on the SOC content of Wuyi Mountains.

Comparative Studies on Tourist Satisfaction of World Heritage Sites——A Case Study of Huangshan Mountain,Lushan Mountain and Wuyi Mountain

Through the questionnaire survey and comparative studies on tourist satisfaction of tourism services among three world heritage sites,i.e.Huangshan Mountain,Lushan Mountain and Wuyi Mountain,this study pointed out the problems in tourism services of three scenic areas and then put forward relevant countermeasures for the management of scenic areas.

Throughfall and stemflow nutrient depositions to soil in asubtropical evergreen broadleaved forest in the Wuyi Mountains

A study concerning the throughfall and stemflow chemistry in the Castanopsis eyrei forest was conducted during 1993—1994. The results showed that the net throughfall nutrient fluxes showed consistent canopy effects on precipitation chemistry. In general, potassium, calcium, magnesium, sodium and sulphur were added to precipitation by foliage, whereas the canopy absorbed nitrogen and phosphorus from precipitation. In stemflow, negative net deposition occurred for phosphorus only, and the rest nutrients were added to precipitation by tree stems and branches. The total net depositions of nutrients in both throughfall and stemflow followed the sequence of potassium>calcium>sodium>magnesium>sulphur, ranging between 2 56—52 54 kg/(hm 2·a). For potassium and calcium, net throughfall was the largest pathway, and the net throughfall contribution to the total yearly nutrient return to the forest soil was 54% and 42% respectively. Although the net stemflow contribution to the total yearly nutrient return was small (between 0 and 13%), stemflow represented the largest pathway of water and nutrient input to the stemflow zone of the forest floor in the C.eyrei forest ecosystem.

Crustal Electrical Structure and Deep Metallogenic Potential in Northern Wuyi Area(South China),based on Magnetotelluric Data

The northern Wuyi area,which is located in the northern Wuyi metallogenic belt,has superior mineralization conditions.The Pingxiang-Guangfeng-Jiangshan-Shaoxing fault(PSF)extends across the whole region regardless of whether or how the PSF relates to the near-surface mineralization.We carried out an MT survey in the region and obtained a reliable 2D model of the crustal electrical structure to a depth of 30 km.In the resistivity model,we inferred that a continuous high conductivity belt that ranges from the shallow to deep crust is a part of the PSF.Then,we estimated the fluid content and pressure gradient to identify the deep sources of fluid as well as its pattern of motion pattern.Finally,we proposed a model for the deep metallogenic migration processes that combines geological data,fluid content data,pressure gradient data,and the subsurface resistivity model.The model analysis showed that the Jiangnan orogenic belt and the Cathaysia block formed the PSF during the process of com.The deep fluid migrated upward through the PSF to the shallow crust.Therefore,we believe that the PSF is an ore-forming fluid migration channel and that it laid the material basis for large-scale mineralization in the shallow crust.

Wuyi Mountain

Listed as a World Cultural and Natural Heritage Site in 1999 Location:Wuyishan City,Fujian Province Best Time to Visit:Between June and August WUYI Mountain,located in southeast China’s Fujian Province,contains the largest and most representative example of a largely

Confirmation and Preliminary Study of Aluminous A-Type Granites in the Wuyi Mountain Area, Eastern Jiangxi Province, China

Widespread in the Wuyi Mountain area of eastern Jiangxi are petrochemically peraluminous granites and they are characterized as being high in silica (SiO\-2>75%) and highly alkaline (ALK=6.9%-7.5%) with K\-2O>Na\-2O and rather high ratios of FeO\+T/MgO (11.3-17.9). The rocks have low contents of CaO, MgO, TiO\-2 and P\-2O\-5 . The granites are enriched in REE (ΣREE=210.3-496.8 μg/g) with remarkable negative Eu anomalies, but depleted in Eu, Ba, Sr, V, Co, and Ni, with 10000×Ga/Al ratios, varying from 6.1 to 9.8. It is clear that these granites are obviously different from the I\| and S\|type granites, but are quite similar to those typical A\|type granites such as aluminous A\|type granites in the coastal areas of Fujian Province.

The age and tectonic environment of the rhyolitic rocks on the western side of Wuyi Mountain,South China

During the geological survey of the metamorphic rocks in Xingning-Wuhua region on the western side of Wuyi Mountain, South China, we discovered the Neoproterozoic rhyolite and rhyolitic greywacke for the first time that outcrop in the Proterozoic metamorphic rocks near Jingnan Town of Xingning County, eastern Guangdong Province. A systematic research on petrology, geochemistry and geochronology of rhyolitic rocks was conducted to understand their tectonic setting and formation age. The Jingnan rhyolite is interbedded with a coeval greywacke, with a total thickness of 60 m; both rhyolite and greywacke display a similar folding and metamorphic pattern. Meta-rhyolite consists of groundmass and phenocrystals including sanidine, orthoclase, and quartz with distinct undulose extinction; the groundmass has been recrystallized into fine-grain feldspar, quartz and sericite aggregation. Meta-greywacke is composed of crystallinoclastic grains (sanidine, orthoclase, quartz and oligoclase) and clay groundmass. Zircon grains used for the SHRIMP U-Pb analysis are light brown-colored and euhedral or subeuhedral. Dating data suggest two age groups; eight grains of magmatype zircon with an idiomorphic form yield an age of 972±8 Ma, and the other seven weakly corroded grains of zircon with euhedral to subeuhedral shape construct an average age of 1097±11 Ma, which were captured from older rocks by an uplifting magma, implying that a late Mesoproterozoic basement exists in the Nanling region. In addition, one Paleoproterozoic age, 2035±11 Ma, is obtained from a rounded detrital zircon, indicating that a Paleoproterozoic thermal event took place in the South China. Geochemically, the Jingnan rhyolitic rocks are characterized by high K2O content, intermediate Al2O3 content, with the ACNK value 0.98―1.11, and belonging to high-K alkaline series. They are rich in ΣREE, Rb, Th and Ce, depleted in Ba, Sr, Eu, Ti, P and Nb-Ta, and with moderate negative Eu and Sr anomalies. These features indicate that the Jingnan volcanic rocks have an affinity of continental arc that is similar to those of acid volcanic rocks in the SE-China Coastal Region, in other words, a Neoproterozoic tectonomagma event might have taken place in the western Wuyi region, leading to an eruption of high-K calc-alkaline granitic magma.

Timing of the formation of the Tianhuashan Basin in northern Wuyi as constrained by geochronology of volcanic and plutonic rocks

The Tianhuashan Basin is one of the most important volcanic basins in the northern Wuyi,southeastern China,comprising two successive volcanic units,the Daguding Formation and the overlying Ehuling Formation,along with several small associated igneous intrusions.The Lengshuikeng super-large-scale Ag-Pb-Zn deposit,which is closely related to these volcanic-intrusive rocks,is located in the northwestern part of the basin.In order to understand the basin evolution and magmatism,we determined LA-ICP-MS U-Pb zircon ages for the volcanic successions and associated intrusive rocks.U-Pb zircon dating of volcanic units yielded precise ages of 144±1 Ma for crystal tuff in the lower member of the Daguding Formation,142±1 Ma for andesite within the upper member of the Daguding Formation,140±1 Ma for tuffite of the first(i.e.,lowermost) member of the Ehuling Formation,and 137±1 Ma for rhyolitic ignimbrite within the third volcano-stratigraphic member of the Ehuling Formation.Three types of intrusive igneous rocks(quartz syenite porphyry,K-feldspar granite porphyry,and rhyolite porphyry) yielded precise weighted mean 206 Pb/238 U ages of 144±1,140±1,and 140±1 Ma,respectively,suggesting that these intrusions along with the aforementioned volcanics were all emplaced during the Early Cretaceous.In addition,the weighted mean 206 Pb/238 U ages determined on zircon from two samples of a granite porphyry intrusion,which hosts ore mineralization of the Lengshuikeng Ag-Pb-Zn deposit,are 158±1 and 157±1 Ma,indicating emplacement in the Late Jurassic.These new geochronological results for igneous rocks of the Tianhuashan Basin constrain the timing of volcanic and plutonic activity in the basin,and have important implications for our understanding the tectonic history of the region,and for identifying metallogenic types and the timing of ore deposition of the Lengshuikeng deposit.

Guarding Wuyi

This site in the Peal River Delta abounds in unusual towers built for defense and as a refuge from natural disasters Jiangmen, in the Pearl River Delta in south China, is an enchanting city. Under its jurisdiction are Xinhui District and Taishan, Kaiping, Enping and Heshan cities, historically known as Wuyi (five counties) because of their shared popular customs.

Fairyland: Wuyi Mountain

ASK where fairyland is on earth andsome people will say you need look nofurther than Wuyi Mountain. Located on theboarder of Fujian and Jiangxi provinces, WuyiMountain is famous for its unique landscapeand rich cultural background. A legend says that in remote antiquity thisarea was a place often stricken by floods.People lived a miserable life. Peng Yi workednight and day, eating in the wind and sleepingin the dew. He rallied the people together andwith their hoes they opened the mountain,controlled the water and finally changed

China-Canada Project Teaches Wuyi Women Tailoring

HOT as it was, He Suhua was exceptionally happy at the opening ceremony of the Seventh Dress-making Training Class in Wuyi County, as part of the China Canada Women in Development Project. He, a head of women at Huaifu Village, dressed in clothes made by a woman who had studied in the third dress-making training class, led 11 new trainees to the county

添加武夷岩茶对米粉丝品质、体外消化特性和抗氧化活性的影响

为开发具有抗消化性和抗氧化活性的功能米粉制品,研究添加武夷岩茶对米粉丝品质、体外消化特性和抗氧化活性的影响。采用质构仪和感官评价法测定米粉丝的质构和感官品质,采用GC-MS法检测风味成分,采用FRAP法、DPPH和ABTS+自由基清除法测定抗氧化活性,采用体外模拟消化法检测米粉丝的体外消化特性。结果表明,与未添加武夷岩茶的米粉丝(对照组)相比,添加2.9%~7.0%武夷岩茶的米粉丝断条率无明显变化(P>0.05),添加8.3%武夷岩茶的米粉丝断条率显著增加(P<0.05);添加2.9%~8.3%武夷岩茶的米粉丝硬度、粘聚性、胶着性、咀嚼性和回复性显著低于对照组(P<0.05),而气味和食味分值显著高于对照组(P<0.05);添加5.7%武夷岩茶的米粉丝保留了岩茶的主要香气物质(香叶醇、2-苯乙醇、苯乙醛、(E)-2-己烯醛),且其米粉丝弹性显著高于对照组和其余岩茶组(P<0.05)。与对照组相比,添加5.7%武夷岩茶的米粉丝中快消化淀粉(RDS)比例下降8.69%,抗性淀粉(RS)比例增加14.34%,对DPPH和ABTS+自由基的清除能力显著增强(P<0.05),总抗氧化能力是对照组的7.48倍。在米粉丝中添加武夷岩茶能够赋予米粉丝独特风味,显著增强米粉丝的抗消化性和抗氧化活性,提高了米粉丝的营养保健价值。

近代侨乡建筑装饰审美意识初探——以广东五邑侨乡为例

清同治至民国时期中国侨乡建筑装饰逐渐形成独特的乡村审美意识,它是华侨和侨乡民众接触西方文化后在审美层面主动作出的回应。基于五邑侨乡田野调查获得的装饰素材,结合民众生活方式,从审美趣味、审美题材、审美形式等方面分析,提出洋气美、工业美、杂糅美三种极具侨乡特色的近代审美意识。研究侨乡审美意识可丰富岭南乡村美学内涵,亦对构建以农民为审美主体的当代侨乡乡村美学有重要意义。

农旅融合背景下武夷山民宿业助力乡村振兴对策研究

民宿业在乡村旅游业中占有重要地位,是乡村旅游文化体验的重要组成部分。农旅融合理念下民宿经营者应加强对乡村文化包括乡村古民居、民间习俗等非物质文化遗产的挖掘,将地方特色风土人情融入乡村民宿建设,打造集自然、人文、乡村美食、康养休闲于一体的特色乡村文化体验型民宿品牌。武夷山民宿乡村旅游资源丰富,经营者需融入乡村农业生活体验、茶文化生活体验,设计具有文化创意和乡村美学的民宿起居、休闲空间,提升顾客期待型、魅力型需求体验,从而提高乡村民宿吸引力和村民收入,助力乡村振兴。

武夷山黑麂生境适宜性评价

道路网络建设促进区域社会经济发展的同时也阻隔了野生动物的通行和交流,影响或破坏了生境。武夷山是地球上同纬度生物多样性最丰富的地区之一,栖息着许多珍稀野生动物。本研究以黑麂(Muntiacus crinifrons)为目标物种,对其生境适宜性进行了评价,并借助水文分析模拟动物潜在的运动轨迹。结果表明:黑麂最适宜生境面积占研究区总面积的16.53%,其他依次是一般适宜、较适宜、较不适宜和不适宜,占比分别是29.63%、22.69%、20.77%和10.38%。最适宜生境主要集中于武夷山国家级自然保护区的核心区,通过模拟得到的动物足迹与道路网络叠加,发现5处动物足迹受到道路的阻隔,其中与高速公路相交1处、与省道相交1处、与县道相交1处和与乡道相交2处。研究结果可为制订生境保护和修复政策提供参考,对野生动物保护具有重要意义。

新疆水利工程西域砾岩边坡加固关键技术研究与应用

鉴于西域砾岩边坡长期浸没水中软化变形后失稳、因水位变动对边坡表面掏刷破坏、内外水头差过大导致的滑坡、高速水流对坡脚掏刷导致坡顶崩塌等问题,该地层条件下的水利工程高边坡广泛存在,传统的水利工程边坡加固形式已经无法解决此类边坡的问题。为了保证库区内西域砾岩高边坡稳安全定性,实现工程安全性和经济型的平衡,结合新疆迪那河五一水库工程面临库区内联合进水口西域砾岩高边坡加固的问题,提出了一套适用西域砾岩高边坡加固的方法,该方法成功的解决了西域砾岩边坡在蓄水后遇到的边坡软化失稳和长期安全运行的问题,为今后同处西域砾岩的水利工程边坡处理提供借鉴和帮助。

武夷山野外认药实践虚拟仿真线路与图片库建设实践

实地收集福建省武夷山三港至后山、华光庙、龙渡、挂墩等不同方向的5条实践线路中常见、重点、特色中药资源物种,整合汇总不同线路共400种物种图片,结合物种地理位置信息形成虚拟仿真线路与数字图片库。图片库的建设优化了教学方式,拓展了学生的野外视野,提供了预习与复习的途径,极大地促进了学科的学习氛围与效率。