Rashin gurɓataccen ruwa
| Bayanai | |
|---|---|
| Ƙaramin ɓangare na |
environmental impact of mercury (en) |

Mercury ƙarfe ne mai nauyi wanda ke zagayawa cikin yanayi, ruwa, da ƙasa a cikin siffofi daban-daban zuwa sassa daban-daban na duniya. Saboda wannan sake zagayowar mercury na halitta, ba tare da la'akari da wane ɓangare na duniya ya saki mercury ba zai iya shafar wani ɓangare daban-daban na duniya yana sa gurɓataccen mercury ya zama damuwa a duniya. Yanzu an gano gurɓataccen Mercury a matsayin matsala ta duniya kuma an gabatar da wayar da kan jama'a a kan shirin aiki na kasa da kasa don rage hayakin mercury na mutum da tsaftace gurɓatawar mercury. 2002 Global Mercury Assessment ya kammala cewa "ya kamata a jinkirta ayyukan kasa da kasa don magance matsalar mercury ta duniya". Daga cikin mahalli da yawa da ke ƙarƙashin tasirin gurɓataccen mercury, teku ɗaya ce wacce ba za a iya watsi da ita ba saboda tana da ikon yin aiki a matsayin "kayan ajiya" don mercury. Dangane da binciken samfurin da aka yi kwanan nan an kiyasta jimlar mercury da aka saki cikin teku ya kai kusan 80,000 zuwa 45,000 metric ton kuma kashi biyu bisa uku na wannan adadin an kiyasta za a same su a cikin ruwa da bai kai matakin 1000m ba inda yawancin kifi ke rayuwa. Mercury na iya tarawa a cikin sarkar abinci na ruwa a cikin nau'in methylmercury mai guba wanda zai iya haifar da haɗarin lafiya ga masu amfani da abincin teku. Dangane da kididdigar, kusan kashi 66% na amfani da kifi na duniya ya fito ne daga teku. Sabili da haka, yana da mahimmanci a saka idanu da kuma tsara matakan mercury na teku don hana ƙarin mercury daga isa ga yawan mutane ta hanyar amfani da abincin teku.
Tushen
[gyara sashe | gyara masomin]Sakin Mercury yana faruwa ta hanyar tsarin halitta da na ɗan adam. Hanyoyin halitta galibi sune geogenic kamar ayyukan dutsen wuta da hayaki na ƙasa ta hanyar ƙasa. Dutsen wuta yana fitar da mercury daga tafkunan karkashin kasa a lokacin fashewa. Ana yawan lura da hayaki na ƙasa a yankunan da ke kusa da iyakokin farantin-tectonic inda aka wadatar da ƙasa da ma'adanai kamar cinnabar (marasa narkewa mercury sulfide, HgS). Ana saki wannan mercury, yawanci a matsayin gishiri, ko dai ta hanyar yanayi na duwatsu ko ta hanyar halayen geothermal. Duk da yake abubuwan da suka faru na halitta suna da alaƙa da wani kashi na hayaki na yau da kullun, hayaki na mutum kadai ya kara yawan mercury a cikin muhalli sau uku. Global Mercury Assessment 2013 ya bayyana cewa manyan hanyoyin samar da mercury sune sana'a da ƙananan ma'adinai na zinariya, ƙone man fetur, da kuma samar da ƙarfe marasa ƙarfe. Sauran tushe kamar samar da siminti, sharar kayan masarufi, crematoria, wuraren da aka gurbata, da masana'antar chloralkali suma suna ba da gudummawa a cikin ƙananan kashi.[2]
Mercury mai laushi
[gyara sashe | gyara masomin]Mercury na iya shiga teku da bude teku sakamakon motsi na rafi da sake sanya gurbataccen datti daga birane.[3] Misali, babban jimlar abun ciki na Hg har zuwa 5 MG / kg kuma matsakaicin kimanin 2 MG / kg yana faruwa a cikin turɓaya na saman da kuma turɓaya a cikin Kogin Mersey, Burtaniya, saboda fitarwa daga masana'antun tarihi da ke gefen kogin da ya haɗa da masana'antu kamar masana'antar chlor-alkali ta tarihi.[3] An kuma nuna cewa an yi amfani da sediments tare da tsawon kilomita 100 na Thames Estuary suna da jimlar abubuwan Hg har zuwa 12 MG / kg da kuma matsakaicin 2 MG / kg tare da mafi girman maida hankali da aka samu a zurfin da kewaye da London.[4] Ragewa mai mahimmanci a hankali da ƙididdigar ƙididdigat a cikin abun ciki na Hg yana faruwa a cikin Thames a matsayin sakamakon nesa mafi girma daga tushen tarihi da na yanzu, sorption da kuma a cikin kogi a cikin laka ya kai, da kuma narkewa ta yashi na ruwa daga Tekun Arewa.[4] Sabanin haka, sinadarin da ke shiga cikin teku daga koguna marsh na gabar gabashin Amurka da mangroves da ke gefen Tekun Kudancin China gabaɗaya suna da matsakaiciyar Hg (<0.5 MG / kg).[5][6]
Manazarta
[gyara sashe | gyara masomin]- ↑ Batrakova, N., Travnikov, O. and Rozovskaya, O. (2014) "Chemical and physical transformations of mercury in the ocean: a review". Ocean Science, 10 (6): 1047–1063. doi:10.5194/os-10-1047-2014
- ↑ Cite error: Invalid
<ref>tag; no text was provided for refs namedME2013 - ↑ 3.0 3.1 Vane, C.H.; Jones, D.G.; Lister, T.R. (2009). "Mercury contamination in surface sediments and sediment cores of the Mersey Estuary, UK" (PDF). Marine Pollution Bulletin. 58 (6): 940–946. doi:10.1016/j.marpolbul.2009.03.006. ISSN 0025-326X. PMID 19356771.
- ↑ 4.0 4.1 Vane, Christopher H.; Beriro, Darren J.; Turner, Grenville H. (2015). "Rise and fall of mercury (Hg) pollution in sediment cores of the Thames Estuary, London, UK". Earth and Environmental Science Transactions of the Royal Society of Edinburgh. 105 (4): 285–296. doi:10.1017/S1755691015000158. ISSN 1755-6910.
- ↑ Vane, C.H.; Harrison, I.; Kim, A.W.; Moss-Hayes, V.; Vickers, B.P.; Horton, B.P. (2008). "Status of organic pollutants in surface sediments of Barnegat Bay – Little Egg Harbor Estuary, New Jersey, USA" (PDF). Marine Pollution Bulletin. 56 (10): 1802–1808. doi:10.1016/j.marpolbul.2008.07.004. ISSN 0025-326X. PMID 18715597.
- ↑ Vane, C.H.; Harrison, I.; Kim, A.W.; Moss-Hayes, V.; Vickers, B.P.; Hong, K. (2009). "Organic and metal contamination in surface mangrove sediments of South China" (PDF). Marine Pollution Bulletin. 58 (1): 134–144. doi:10.1016/j.marpolbul.2008.09.024. ISSN 0025-326X. PMID 18990413.