Izingozi ze-lawn moss yenkundla yegalofu

Imikhuba yemvelo kanye nokwenzeka kwendawo ye-moss
Utshani obusezingeni eliphezulu buyisiqinisekiso esibalulekile sezinzuzo ezinhle zezinkundla zegalofu kanyeizinkundla zemidlalo. Izingadi zenkundla yegalofu zivame ukuniselwa, futhi ukuma kweminye imigwaqo emikhulu nezihlahla kungadala kalula indawo emanzi, okuholela ekukhuleni kwenani elikhulu le-moss, okunzima ukulisusa uma selimile izimpande. Ngenxa yokuvela kwe-moss, akugcini nje ngokukhula kwengadi okubuthakathaka, kodwa futhi nokufa kwengadi kubangelwa. Ngaphezu kwalokho, ukuvela kwenani elikhulu le-moss kuzobhubhisa nokuhlanzeka kwengadi futhi kunciphise ngqo ukuhlobisa kanye nenani lokusetshenziswa kwengadi. Ukuqonda amaphethini okwenzeka kwe-moss kubaluleke kakhulu ekwakheni izinyathelo zesayensi zokuvimbela nokulawula i-moss kanye nokunikeza indima egcwele yengadi.
I-Moss iyisitshalo esiphansi esakhiwe yi-symbiosis ye-algae eluhlaza kanye ne-fungi ethile. Ikhula kakhulu inamathele. Ngokuvamile ikhuliswa ezindaweni ezimanzi nezimnyama, isakazeke kabanzi, ihlukahlukene ngezinhlobo, futhi iningi ngenani. Ivame ukukhula emhlabathini omanzi nodaluliwe ezindaweni ezinomswakama ophansi ezindaweni ezishisayo, ezishisayo nezifudumele. Izici eziyinhloko zemvelo ezithinta ukukhula kwe-moss ngamanzi nokukhanya. Umswakama wayo ofanele wokukhula ungaphezu kuka-32%, kanti izinga lokushisa layo lokukhula elifanele lingu-10-21°C. I-Moss ingasakazeka ngezindlela ezahlukene. Izinhlobo eziningi zikhiqiza ama-sporangia amancane aqukethe ama-spores emaqabungeni awo. Lawa ma-spores angasakazwa ngomoya, amanzi noma ukuhamba ngemva kokuthintana nomhlabathi. Ngemva kokuba ama-spores evuthiwe, aqala ukwakha izicubu ezifana nesitshalo, okuyisigaba sokuqala sokuthuthukiswa kwe-moss. Uma ihlangabezana nezimo ezifanele zomsingathi kanye nezemvelo, izohluma futhi ikhiqize ama-gametophyte amasha anesimo seqabunga, azobe esemunca amanzi namaminerali ngama-rhizome futhi akhe amagatsha amasha, ngaleyo ndlela aqhubeke nokuzala.

Ukulimala kwe-moss ezinkundleni zegalofu
Ukhula luvame ukwenzeka esimweni sezulu esifudumele, esinomswakama, nesinamafu. Ukulimala kotshani kwenzeka kakhulu ekwindla nasehlobo enyakatho, kanye nasekwindla, ebusika nasentwasahlobo eningizimu. Ukhula luvela lapho ukuvunda kwenhlabathi kunganele noma kungavundiswanga kahle, kumanziswe kakhulu, utshani lunomthunzi kakhulu, inhlabathi ayimuncekanga kahle noma inhlabathi incane kakhulu, kanye nenhlanganisela yalezi zimo ezimbi. Uma sekunokhula otshanini, izinyathelo kumele zithathwe ngokushesha, ngaphandle kwalokho ukhula luzosabalala yonke indawo futhi lwenze kube nzima ukulawula ukhula.
I-Moss ayinaso isakhiwo sangempela semithambo yegazi, kodwa ingenza i-photosynthesis futhi imunce ngqo amanzi nezakhamzimba. Isakazeka kalula ngomoya, ngamanzi noma ngokuhamba. Ngemva kokuba ama-spores ehlume, akha izicubu ezifana nezitshalo ezimunca amanzi namaminerali ngokusebenzisa ama-rhizoid afana nezimpande futhi zikhiqize amahlumela amasha, kamuva akhula abe yiziqu ezintsha. Yisitshalo esinezimpande ezingajulile esimboza umhlabathi, esingaminyanisa utshani futhi siqede izinqolobane zezakhamzimba enhlabathini, okubangela ukukhula kabi kwetshani, ukuphuzi ngisho nokufa okukhulu kotshani betshani. Ngakho-ke, kufanele kunakwe ekunakekelweni.
Izingozi ze-moss zingafingqwa kanje:
(1) Ukumboza umhlabathi kungacinanisa utshani futhi kuqede izakhamzimba ezigciniwe enhlabathini, okubangela ukuba ukukhula kotshani obusemhlabathini kube buthaka futhi kubangele ngisho nokufa kotshani obusemhlabathini, okuholela ekuchithweni komanyolo kanye nezindleko zokulungisa ezikhulayo.
(2) Ukubhubhisa ukufana kotshani botshani bese kunciphisa ngokuqondile inani lokuhlobisa kanye nokusetshenziswa kotshani.
(3) Ukuvimbela izivakashi ukuthi zingadlali ibhola.
(4) Kuthinta ukungena kwamanzi nomoya, okubangelaukuminyana kwenhlabathi.