煤田地质与勘探
煤田地質與勘探
매전지질여감탐
COAL GEOLOGY & EXPLORATION
2010年
1期
33-36
,共4页
刘钦甫%郑丽华%张金山%王帅%丁述理
劉欽甫%鄭麗華%張金山%王帥%丁述理
류흠보%정려화%장금산%왕수%정술리
煤矸石%铵伊利石%氮%环境效应
煤矸石%銨伊利石%氮%環境效應
매안석%안이리석%담%배경효응
coal gangue%ammonium illite%nitrogen%environmental effects
通过对晋东南和豫中地区几个煤矿矸石堆及其周围的土壤和水体、井下矸石取样分析,发现这些矿的煤矸石中全氮的背景值为0.4%-0.8%.在中高煤变质程度地区,含铵伊利石夹矸中全氮高达1.0%-1.6%,铵伊利石的存在对于矸石堆中全氮含量的提高具有贡献.在矸石山周围积水中,具有较高的氮含量,说明雨水比较容易从矸石堆中将氮淋滤出来.煤矸石堆周围土壤中的氮含量并不高,说明煤矸石淋滤物并没有发生明显的横向迁移,可能主要表现为垂向渗透,有可能对地下水造成潜在的氮污染.
通過對晉東南和豫中地區幾箇煤礦矸石堆及其週圍的土壤和水體、井下矸石取樣分析,髮現這些礦的煤矸石中全氮的揹景值為0.4%-0.8%.在中高煤變質程度地區,含銨伊利石夾矸中全氮高達1.0%-1.6%,銨伊利石的存在對于矸石堆中全氮含量的提高具有貢獻.在矸石山週圍積水中,具有較高的氮含量,說明雨水比較容易從矸石堆中將氮淋濾齣來.煤矸石堆週圍土壤中的氮含量併不高,說明煤矸石淋濾物併沒有髮生明顯的橫嚮遷移,可能主要錶現為垂嚮滲透,有可能對地下水造成潛在的氮汙染.
통과대진동남화예중지구궤개매광안석퇴급기주위적토양화수체、정하안석취양분석,발현저사광적매안석중전담적배경치위0.4%-0.8%.재중고매변질정도지구,함안이리석협안중전담고체1.0%-1.6%,안이리석적존재대우안석퇴중전담함량적제고구유공헌.재안석산주위적수중,구유교고적담함량,설명우수비교용역종안석퇴중장담림려출래.매안석퇴주위토양중적담함량병불고,설명매안석림려물병몰유발생명현적횡향천이,가능주요표현위수향삼투,유가능대지하수조성잠재적담오염.
Based on the analysis of samples from coal gangue,soil and leached water around gangue pile,it was found that the background content of total nitrogen in coal gangue is about 0.4%-0.8%.but the total nitrogen content in ammonium illite-bearing gangue is up to 1.0%-1.6%.So that,the existence of ammonium illite in the area of high metamorphic coal will contribute to the elevated nitrogen content.The leached water around coal gangue has high content of nitrogen,which shows that the nitrogen in the gangue is easy to be leached out by rain.The soil around the coal gangue has lower nitrogen content,which shows that leached water does not flow laterally,but possibly infiltres vertically,which may cause potential nitrogen pollution.