Stereoselective Degradation of Estradiol and Trenbolone Isomers in Alluvial Sediment

2016 ◽  
Vol 50 (24) ◽  
pp. 13256-13264 ◽  
Author(s):  
Yun Zhang ◽  
Daniel D. Snow ◽  
Shannon L. Bartelt-Hunt

Geology ◽  
2000 ◽  
Vol 28 (9) ◽  
pp. 803-806 ◽  
Author(s):  
Clifford S. Riebe ◽  
James W. Kirchner ◽  
Darryl E. Granger ◽  
Robert C. Finkel


Chirality ◽  
2000 ◽  
Vol 12 (2) ◽  
pp. 53-62 ◽  
Author(s):  
H�l�ne Georges ◽  
Nathalie Presle ◽  
Thierry Buronfosse ◽  
Sylvie Fournel-Gigleux ◽  
Patrick Netter ◽  
...  


Author(s):  
L. Sung ho ◽  
H. Dong soo

The preservation of historic cities requires a balance between conservation and development because the urban structures of the old and new city are interwoven on same space. Existing restoration plans rely on old records and excavation reports and are based on the present topography. However, historic cities have undergone significant natural and anthropogenic topographic changes such as alluvial sediment accumulation and uneven terrain construction. Therefore, considering only the present topography is misleading. Thus, to understand a historic city’s structure more appropriately, it is necessary to comprehend the ancient geographic environment. This study provides an analysis and GIS visualization of the ancient topography of a historic city, Sabi capital city of the Baekje Dynasty, which collapsed 1,500 years ago.



2014 ◽  
Vol 108 ◽  
pp. 34-41 ◽  
Author(s):  
Yinghuan Wang ◽  
Baoyuan Guo ◽  
Yongxin Gao ◽  
Peng Xu ◽  
Yanfeng Zhang ◽  
...  


2006 ◽  
Vol 40 (24) ◽  
pp. 7950-7951 ◽  
Author(s):  
Wolfgang Bicker ◽  
Michael Lämmerhofer ◽  
Wolfgang Lindner


2020 ◽  
Vol 11 (1) ◽  
Author(s):  
David B. Kemp ◽  
Peter M. Sadler ◽  
Veerle Vanacker

AbstractHumans are primary agents of geomorphic change, and rates of anthropogenic landscape change likely far exceed the pace of change expected from natural geologic processes. Nevertheless, our understanding of the impact of humans on the natural landscape is limited by difficulties in accurately comparing past and present rates of change across wide spatial and temporal scales. Here, we present a compilation of  >4000 rates of alluvial sediment accumulation that provide an indirect record of North American erosion, mass transfer and sediment storage from the late Pleistocene to the present day. Continent-wide rates of alluvium accumulation were broadly stable for ~40,000 years, but increased 10-fold during the rapid expansion of agriculture and river system modification associated with European colonization. Interpreted in terms of mass transfer, humans have moved as much sediment in North America in the past century as natural processes can transfer in 700–3000 years.



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