Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Ling-Pan Du"'
Publikováno v:
Ecotoxicology and Environmental Safety, Vol 262, Iss , Pp 115215- (2023)
Southwestern China has the largest geological phosphorus-rich mountain in the world, which is seriously degraded by mining activities. Understanding the trajectory of soil microbial recovery and identifying the driving factors behind such restoration
Externí odkaz:
https://doaj.org/article/cef7ee5f3d7f4a1bb56067687c07920c
Publikováno v:
Advanced Materials Research. :852-855
Weathered phosphate ore is an important part of phosphate ore resources, it contains a huge reserves of weathered phosphate ore resources in Yunnan regions. With the gradual consumption of the rich phosphate ore resources, recycling for weathering ph
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1ad02afaa3eefe390937a42e5fd47663
https://doi.org/10.4028/www.scientific.net/amr.962-965.852
https://doi.org/10.4028/www.scientific.net/amr.962-965.852
Publikováno v:
Advanced Materials Research. :797-802
Yunnan Dianchi surrounding areas’ phosphate rock is rich in resources, but high grade phosphate rock is less and less. Currently used methods are mainly floatation concentrate, but most of phosphate rock are difficult to flotation of collophane wit
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::49e97f26bd76ce6021059f2c9ed1f038
https://doi.org/10.4028/www.scientific.net/amr.962-965.797
https://doi.org/10.4028/www.scientific.net/amr.962-965.797
Publikováno v:
Advanced Materials Research. :833-836
Weathered phosphate ore is an important part of phosphate ore resources, it contains a huge reserves of this resources in Yunnan regions, and its reserves over 200 million tons. With the gradual consumption of the rich phosphate ore resources, recycl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::eb5cc57ce414fd56f3af27a2c6636d2b
https://doi.org/10.4028/www.scientific.net/amr.962-965.833
https://doi.org/10.4028/www.scientific.net/amr.962-965.833