In this paper, we conduct research on the college English teaching emphasis from the cultural migration and transformation ofthinking perspectives. College English has long been in for the college English subject stat...In this paper, we conduct research on the college English teaching emphasis from the cultural migration and transformation ofthinking perspectives. College English has long been in for the college English subject status. However, college English as a multidisciplinary,interdisciplinary research in the field of discipline construction, it seems, are still stay in the linguistics, language knowledge in academiccharacteristics for its stage of development. Reform of basic college English teaching, the teacher is still teaching main body, is the teaching oflanguage knowledge, since teachers play an important role in language teaching, the teacher wants to penetrate cultural knowledge in teachingand we must strengthen their own culture. Under this basis, this paper proposes the novel ideals on the related issues that will be meaningful andinnovative.展开更多
. A dialect refers to a local variation of a language which is distinguished fi＇om variants of the same language in grammar, lexis, or pronuneiation. A dialect plays an important role in second language learning. It .... A dialect refers to a local variation of a language which is distinguished fi＇om variants of the same language in grammar, lexis, or pronuneiation. A dialect plays an important role in second language learning. It can be a positive element as well as negative one in second language learning. Pingdu dialect as a kind of mandarin variation has its own structure and pronunciation rules. By contrastive analysis, we study the negative transfer of Pingdu Dialect on English pronunciation. We mainly concentrate on how two initials ＂s＂ and ＂z＂ in pinyin which sound like two English consonants/0 /and/6/influence the pronunciation of English consonants/s/and/z/. We also fred the countermeasures to overcome negative transfer of dialect on the acquisition of English pronunciation, thereby helping EFL learners in certain area of China acquire accurate English pronuneiations and enhance the ability of intercultural eommunication.展开更多
Over one hundred artifacts, including shards, chopped wood, bronze and iron ware debris as well as footprints, have been discovered during archaeological investigations at and around the central Taklamakan Desert Yuan...Over one hundred artifacts, including shards, chopped wood, bronze and iron ware debris as well as footprints, have been discovered during archaeological investigations at and around the central Taklamakan Desert Yuansha Site (38°52′N, 81°35′E). Dating (14C and OSL) and landform study show that the present-day dry Keriya River once sustained an oasis human settle- ment in 2.6 ka BP, historically falling into the Spring and Autumn Period (716-475 BCE) of Chinese history. The chronology and archaeological interpretations also show that some 400 years later, the local Keriya River channel had shifted 40 km southeast to sustain a Western Han (206 BCE-25 CE) Wumi settlement at the Karadun site. In the meantime, river-channel migration had allowed reoccupation of a site west of Yuansha City around 1.9 ka BP (abandoned again by 1.6 ka BP). The remains' chronology shows that this site was affiliated to Wumi culture and Eastern Han (24-220 CE) dynasty rule. Palaeoclimatic records indicate that the migrations of the river and oasis settlers between 2.7 and 1.6 ka BP were coeval with Central Asian climate changes. Yuansha City was built just after the end of 2.8 ka BP glacier advances in western China, suggesting that release of more water during the subsequent glacier recession may have facilitated oasis development such that Iron Age European peoples could settle in the Tarim Basin. As shown from analysis of archeological remains, not only at Yuansha but also in other ancient cities in the Tarim such as Loulan and Jingjue (Niya), conditions around 1.6 ka BP were dry enough to cause oasis decline. Thus, the results reported here enhance our knowledge about environmental changes and their effects on human activities and cultural evolution in western China and will stimulate further interdisciplinary studies of landscape and oasis history in the Tarim Basin.展开更多
文摘In this paper, we conduct research on the college English teaching emphasis from the cultural migration and transformation ofthinking perspectives. College English has long been in for the college English subject status. However, college English as a multidisciplinary,interdisciplinary research in the field of discipline construction, it seems, are still stay in the linguistics, language knowledge in academiccharacteristics for its stage of development. Reform of basic college English teaching, the teacher is still teaching main body, is the teaching oflanguage knowledge, since teachers play an important role in language teaching, the teacher wants to penetrate cultural knowledge in teachingand we must strengthen their own culture. Under this basis, this paper proposes the novel ideals on the related issues that will be meaningful andinnovative.
文摘. A dialect refers to a local variation of a language which is distinguished fi＇om variants of the same language in grammar, lexis, or pronuneiation. A dialect plays an important role in second language learning. It can be a positive element as well as negative one in second language learning. Pingdu dialect as a kind of mandarin variation has its own structure and pronunciation rules. By contrastive analysis, we study the negative transfer of Pingdu Dialect on English pronunciation. We mainly concentrate on how two initials ＂s＂ and ＂z＂ in pinyin which sound like two English consonants/0 /and/6/influence the pronunciation of English consonants/s/and/z/. We also fred the countermeasures to overcome negative transfer of dialect on the acquisition of English pronunciation, thereby helping EFL learners in certain area of China acquire accurate English pronuneiations and enhance the ability of intercultural eommunication.
基金supported by the National Basic Research Program of China (Grant No. 2009CB421308)the National Natural Science Foundation of China (Grant Nos. 40701188 and 40971020)+2 种基金the Natural Science Foundation of Xinjiang Uygur Autonomous Region (Grant No. 2010211A12)the Natural Science Foundation of Xinjiang University (Grant No. BS060112)the Project of Oasis Ecological Key Lab of Education Ministry Xinjiang University (Grant No. XJDX0206-2007-08)
文摘Over one hundred artifacts, including shards, chopped wood, bronze and iron ware debris as well as footprints, have been discovered during archaeological investigations at and around the central Taklamakan Desert Yuansha Site (38°52′N, 81°35′E). Dating (14C and OSL) and landform study show that the present-day dry Keriya River once sustained an oasis human settle- ment in 2.6 ka BP, historically falling into the Spring and Autumn Period (716-475 BCE) of Chinese history. The chronology and archaeological interpretations also show that some 400 years later, the local Keriya River channel had shifted 40 km southeast to sustain a Western Han (206 BCE-25 CE) Wumi settlement at the Karadun site. In the meantime, river-channel migration had allowed reoccupation of a site west of Yuansha City around 1.9 ka BP (abandoned again by 1.6 ka BP). The remains' chronology shows that this site was affiliated to Wumi culture and Eastern Han (24-220 CE) dynasty rule. Palaeoclimatic records indicate that the migrations of the river and oasis settlers between 2.7 and 1.6 ka BP were coeval with Central Asian climate changes. Yuansha City was built just after the end of 2.8 ka BP glacier advances in western China, suggesting that release of more water during the subsequent glacier recession may have facilitated oasis development such that Iron Age European peoples could settle in the Tarim Basin. As shown from analysis of archeological remains, not only at Yuansha but also in other ancient cities in the Tarim such as Loulan and Jingjue (Niya), conditions around 1.6 ka BP were dry enough to cause oasis decline. Thus, the results reported here enhance our knowledge about environmental changes and their effects on human activities and cultural evolution in western China and will stimulate further interdisciplinary studies of landscape and oasis history in the Tarim Basin.
