Amatshe asendle adalwa yimvelo ngokwayo ngenxa yemiphumela yemvelo yeminyaka eminyaka. Ukuhlanganiswa okuncane, ukugaya, ukugaya nezinye izinqubo kuholela ekwakheni amatshe emvelo. Kuye endaweni kanye nezinto zokuqala, itshe lasendle lingamelwa yi-sandstone, i-limestone, i-slate, i-meotis, i-dolomite, i-shungite, njll.
Ukusetshenziswa okukhulu kwamatshe asendle ekwakhiweni nasekuqedeni imisebenzi kubangelwa ukuqina okunamandla namandla, ukumelana nemvula yesikhala, ukuhlobisa okuphezulu, ukuhlanzeka kwemvelo nokukhululeka kokusebenza. Futhi kulokhu okuqukethwe, okudalwe izinqubo zemvelo futhi kusetshenzwa ngamakhulu eminyaka, sekude kakhulu kulawo mzamo onamahloni omuntu wokulingisa itshe lemvelo.
Izinhlobo ezidumile zetshe zasendle zokuhlobisa isakhiwo
Amatshe amathathu asendle ajwayelekile okusebenza ngaphandle angama-shell rock (i-limestone), i-sandstone ne-slate.
I-limestone iyidwala le-sedimentary, elichithwa emakolishi ngokuyinhloko ngendlela yokuqhuma. Ukunethezeka kwentuthuko kanye nokukhiqizwa okukhulu kwemvelo kwenza lokhu kutholakala okungabizi kakhulu.
Umthunzi we-limestone ungase uhluke - kusuka kumhlophe kuya kwempunga nokuphuzi. Ngesimo, amapuleti akhiqizwayo ayi-polygonal noma ayinxantathu. Ubuso bungaphansi noma buketshiwe.
Sandstone - elinye itshe lasendle, elisetshenziselwa kakhulu ukubhekene nesigcawu. Kungumphumela wethonya lemimoya namanzi emadwaleni amancane, okuphumela ngenxa yokuthi aphule futhi abe yi-plastushkas noma emithonjeni ye-rectangular and polygonal shape.
Ngaphandle, i-sandstone ifana ne-limestone, kodwa inezinye izakhiwo zomzimba nezomzimba. Lolu hlobo lwamatshe asendle luhlala luqinile futhi lungasetshenziselwa ukugoqa kuphela, kodwa futhi nokugubha.
Amatshe amatshe asetshenziselwa ukwakhiwa ekuqedeni nasekusebenzeni ukuphahleni anezimvelaphi ezimbi (ukuqoqwa kwamadwala angcolile ngenxa yokukhukhula emanzini noma emhlabathini) noma umshini (ukwakheka kwezendlalelo ngenxa yokufuduka kwamatshe). Ngesinye isikhathi emathunzini akhiqizwa emanzini omkhumbi, kunezinsalela zezilwane zasolwandle nezinhlanzi.
Izinzuzo zetshe lasendle le-facade
Kungadingeki ukuthi, itshe lemvelo yinto ehlala njalo eyakhelwe isikhathi eside kakhulu futhi inomthelela omuhle kumathonya ahlukahlukene. Kunoma yisiphi isimo sezulu, itshe lasendle ligcina izindawo zalo zomzimba nokubukeka kokuqala isikhathi eside.
Ukukhululeka kwemvelo kanye nephethini yelitshe eliyingqayizivele elitholakalayo ngenxa yokushisa okwenzeka ngaphakathi kwedwala, okwavela ekusebenzisaneni kwamaminerali. Umphumela onjalo awukwazi ukufezwa ngokuhlakanipha, ngoba itshe lemvelo liyingqayizivele yobuhle bemvelo.
Izakhiwo zezindlu ezinamatshe asendle zihlala zibukeka ngokungafani. Futhi akukho ukwesaba ukuthi ukuphela okunjalo ngelinye ilanga kuzokwenziwa ngefashini. Njengoba nje itshe lisetshenziswe emakhulwini amaningi eminyaka edlule, namuhla akulahlekelwa ukuhambisana futhi akunakwenzeka ukuba ayeke ukufunwa futhi adume esikhathini esizayo esizayo.
Inzuzo eyengeziwe yamatshe asendle, ikakhulukazi igobolondo rock and sandstone - isakhiwo esiyingozi, ngenxa yokuthi itshe "liphefumula". Lokhu kunikeza i-microclimate emihle ngaphakathi kwendlu.
Ukusebenza ngetshe lemvelo kulula kakhulu. Ukuze wenze lokhu, awudingi ngisho nokudala izindawo eziphambili futhi ulungise isimo seqhezu ngalinye - ungafaka amatshe kunoma iyiphi i-oda eliyingozi, okuyiyo kuphela eyenza umphumela wemvelo.
Ngokuvamile, itshe libekwa phansi kwesakhiwo kanye nezindawo zalo ngabanye - ukuvulwa kwamafasitela neminyango, emagumbini, njll. Ukuhlobisa udonga olugcwele akuvamile, ngoba kunzima. Kodwa-ke, uma ufuna, ungenza lokhu futhi uguqule indlu yakho ibe yindlu yasendulo.
| | | |
| | | |
| | | |
