A lokacin hakowa, recirculation da ƙari na hakowa ruwa ba makawa za su yi mu'amala da stratum ruwaye da kuma haifar da ci gaba da sinadaran canje-canje, wanda zai canza hakowa kaddarorin da kai ga canje-canje a cikin nau'in ion da kuma maida hankali na hako ruwa tacewa. na iya narkar da kasan Layer na bangon shinge mai narkewa a cikin nau'i daban-daban, a gefe guda, ions a cikin ruwa mai hakowa kuma na iya shiga tare da ions a cikin ruwan stratum, don haka musayar ion mai ƙarfi yana faruwa a cikin ɗan gajeren lokaci. Za a iya amfani da chromatography don nazarin canje-canjen ions a cikin hakowa mai tace ruwa wanda ke amsa yanayin stratum a kaikaice.
A cikin bincike mai zurfi, yana daya daga cikin matsalolin hakowa don yin rawar jiki ta hanyar gypsum stratum cikin nasara. Ion chromatography zai iya ƙayyade yanayin ma'adanai masu narkewa da kuma tsinkaya na musamman.
Ion chromatography, a matsayin fasaha na chromatographic, an fi amfani dashi don ƙayyade anions da cations a cikin samfurori don gwadawa.Saboda kyakkyawan zaɓin sa, babban hankali, sauri da dacewa, an yi amfani da shi a wurare da yawa.A cikin cikakken bincike na bincike. wurin yin laka ta hanyar ion chromatography, ta hanyar nazarin bambance-bambancen yawancin manyan abubuwan ion a cikin hakowa ruwa, ana iya yin hukunci akan yanayin samar da ruwa na stratum a cikin lokaci, kuma ana iya yanke hukunci akan halayen stratum.
Lokacin aikawa: Afrilu-18-2023