Ukuguquka kwe-evapotranspiration

  • I-Evapotranspiration ukulahlekelwa kwamanzi ezitshalweni nangaphezulu komhlabathi ngenhlanganisela yokuhwamuka nokuphefumula.
  • Ikalwa ngo-mm futhi ibalulekile ekulinganisweni kwamanzi kwezolimo kanye nemvelo.
  • Kunezinhlobo ezimbili: i-evapotranspiration (PET) engaba khona kanye ne-evapotranspiration (ETR), lapho i-ETR ihlale ingaphansi noma ilingana ne-ETP.
  • Umehluko phakathi kwe-ETP ne-ETR ukhombisa ukushoda kwamanzi, okuwukhiye wokuthuthukisa ukuchelela ezitshalweni.

Ukuguqulwa kwesitshalo

Impela wake wezwa ngomkhuba we ukuphefumula lapho kukhulunywa ngezitshalo. Ngempela, kuyinto eyenzeka lapho izitshalo zilahlekelwa amanzi ezicutshini zazo ngenxa yezimo ezimbili ezisebenza zizonke: ukuhwamuka ngakolunye uhlangothi nomjuluko kolunye. I-Evapotranspiration ingachazwa njengokucatshangelwa ngokuhlanganyela kwalezi zinqubo ezimbili ngasikhathi sinye.

Kulokhu okuthunyelwe sizokukhombisa ukuthi le ndlela isebenza kanjani nokubaluleka kwayo ku umjikelezo wamanzi, kanye nokuthi izithinta kanjani ezolimo kanye nemikhuba yazo.

Kuyini i-evapotranspiration

Ibhalansi ye-Hydric

Siqala ngokuchaza kahle izinqubo ezenziwa ngasikhathi sinye yilabo esibashoyo. Inqubo yokuqala ukuhwamuka. Kuyinto ebonakalayo leyo kuphawula ukuguquka kwesimo samanzi sisuke kuketshezi kuya emswakeni. Lokhu kuhlanganisa nezinqubo ze-sublimation ezenzeka lapho amanzi esesimweni seqhwa noma iqhwa futhi eshintsha ngokuqondile abe umhwamuko ngaphandle kokudlula esimweni soketshezi. Ngaphezu kwalokho, kubalulekile ukuqaphela ukuthi i-evapotranspiration idlala indima ebalulekile ku- Isimo sezulu ezifundeni ezahlukene.

Ukuhwamuka kwenzeka ebusweni benhlabathi nasezitshalweni njengoba izulu liba khona. Ngenxa yamazinga okushisa, isenzo semisebe yelanga noma umoya, amaconsi amanzi ayenemvula agcina ehwamuka. Enye indawo lapho ukuhwamuka kwenzeka khona kusendaweni yamanzi njengemifula, amachibi namadamu. Kwenzeka futhi emhlabathini ngamanzi angena ngaphakathi. Se ivame ukuhwamuka isuke endaweni ejulile iye phezulu. Lawa ngamanzi angene nje noma ezindaweni zokukhipha.

Ngakolunye uhlangothi, sinenqubo yokujuluka. Kuyinto yezinto eziphilayo ezenzeka ezitshalweni. Kuyinqubo abalahlekelwa ngayo amanzi bese bewathela emkhathini. Lezi zitshalo zithatha amanzi ngezimpande ezisuka emhlabathini. Ingxenye yala manzi isetshenziselwa ukukhula kwabo nemisebenzi ebalulekile futhi enye ingxenye badlulela emkhathini.

amanzi angaphansi komhlaba
I-athikili ehlobene:
I-Hydrogeology nokuthi ukuguquka kwesimo sezulu kuyithinta kanjani imithombo yamanzi angaphansi komhlaba

Izilinganiso nokusetshenziswa

Isiteshi sokulinganisa i-Evapotranspiration

Njengoba lezi zimo ezimbili kunzima ukuzikala ngokwehlukana, zenzeka ndawonye njenge-evapotranspiration. Ezimweni eziningi lokhu kufundwa, udinga ukwazi inani lamanzi alahlekile emkhathini nokuthi inqubo elahlekile ngayo ayinandaba. Le datha iyadingeka ukwenza izilinganiso zamanzi zenani lamanzi awelayo maqondana nenani lamanzi alahlekile. Umphumela uzoba ibhalansi enhle uma amanzi enqwabelana noma sinensada yemithombo, noma ibhalansi engalungile uma silahlekelwa amanzi aqoqiwe noma izinsiza. Ukuze uqonde kangcono lo mqondo, kuyasiza ukubonisana nolwazi mayelana amazinga e-reservoir eSpain.

Kulabo abafunda ukuvela kwamanzi, lezi zibhalansi zamanzi zibaluleke kakhulu. Lezi zifundo zigxile ekwandisweni kwemithombo yamanzi yendawo. Lokho kusho ukuthi, wonke amanzi anethwa yimvula akhishwe emanzini alahlekile nge-evapotranspiration, azoba umthamo wamanzi atholakalayo ukuthi sizoba nakho cishe. Vele, kufanele futhi sicabangele inani lamanzi angena ngokuya ngohlobo lomhlabathi noma ubukhona bamanzi.

I-Evapotranspiration iyinhlobonhlobo ebalulekile emkhakheni wesayensi yezolimo. Kuthathwa njengento ebalulekile uma kucatshangelwa izidingo zamanzi ezitshalweni ukuze zikhule ngendlela efanele. Kunamafomula amaningi ezibalo asetshenziselwa ukuthola idatha edingekayo mayelana ne-evapotranspiration kanye nebhalansi yamanzi. Ngaphezu kwalokho, kuyisihluthulelo sokuhlola i- umthelela wokuguquka kwesimo sezulu kulezi zilinganiso.

Iyunithi elinganiswa ngayo ingama-mm. Ukukunikeza umbono, usuku olushisayo lwasehlobo luyakwazi ukuhwamuka phakathi kuka-3 no-4 mm. Kwesinye isikhathi, uma izindawo ezilinganisiwe ziningi ezimileni, umuntu angakhuluma nangama-cubic metres ehektheleni ngalinye lomhlaba.

Amafu ahlakazeka kanjani?
I-athikili ehlobene:
Ukuqonda Inqubo Yokuhlakazwa Kwamafu: Izinto, Izindlela, kanye Nomthelela Wazo Esimeni Sezulu

Izinhlobo ze-evapotranspiration

I-Evapotranspiration kwezolimo

Ukuze ukwazi ukuhlukanisa kahle idatha kubhalansi yamanzi, idatha ye-evapotranspiration ihlukaniswe ngezindlela eziningi. Esokuqala i-evapotranspiration engaba khona (i-ETP). Le mininingwane iyona ekhombisa kithi ukuthi yini ebingakhiqizwa ngomswakama womhlabathi futhi ikhava yezimila ibisesimweni esifanelekile. Lokho wukuthi, inani lamanzi ebelizohwamuka futhi liphume uma izimo zezemvelo bezikulungele.

Ngakolunye uhlangothi esinakho i-evapotranspiration yangempela (ETR). Kulokhu, silinganisa inani langempela lamanzi i-evapotranspires ngokuya ngezimo ezikhona esimweni ngasinye.

Kulezi zincazelo kusobala ukuthi i-ETR ingaphansi noma ilingana ne-ETP. Lokhu kuzokwenzeka ngo-100% wesikhathi. Isibonelo, ehlane, i-ETP icishe ibe ngu-6mm / ngosuku. Kodwa-ke, i-ETR ayinaqanda, ngoba awekho amanzi e-evapotranspire. Ngezinye izikhathi, zombili izinhlobo zizofana, inqobo nje uma izimo ezifanele zinikezwa futhi kukhona ikhava yesitshalo enhle.

Akudingekile ukusho ukuthi, i-evapotranspiration iyisici esingasithakazelisi nhlobo. Kusho ukulahlekelwa yimithombo yamanzi engeke isetshenziswe. Kubalulekile futhi ukukhumbula ukuthi amanzi angenye nje ingxenye yomjikelezo we-hydrological, nokuthi ngokushesha noma kamuva, yonke into ekhishwe yi-evapotranspired izophinde ibe nemvula ngolunye usuku. Mayelana nalokhu, kuyathakazelisa ukufunda ngakho imiphumela yokugawulwa kwamahlathi esimweni sezulu.

isimo sesomiso eSpain
I-athikili ehlobene:
Isimo sesomiso eSpain: Iqiniso kanye Nezimpendulo

Ukubaluleka kwezolimo

I-Evapotranspiration kwezolimo

Zonke izincazelo ezingenhla zibalulekile ekubalweni kobunjiniyela bezitshalo. Lapho sisebenzisa amanani we-ETP ne-ETR ku-hydrology, kubhekelwa kuphela ngaphakathi kwebhalansi ephelele yomcengezi. Lezi zinto yilezo ezikhombisa inani lamanzi alahlekile kulokho okugxile. Ukubheka umthamo wamanzi angaphezulu atholakalayo, njengasemgodini, ukungena ngaphakathi nakho kuyinto enciphisa inani lamanzi atholakalayo.

Ukubaluleka kwe-evapotranspiration kwanda kakhulu lapho singena emkhakheni wezolimo. Kulezi zimo, Umehluko phakathi kwe-ETP ne-ETR ungaba ukushoda, ngoba esimweni sezulu samanje kubalulekile ukuthi izitshalo zihlale zinamanzi anele.. Kwezolimo, lo mehluko uhloselwe ukuthi ube ngu-zero, njengoba kusho ukuthi izitshalo zihlale zinamanzi anele okuphuma lapho ziwadinga. Ngale ndlela songa amanzi okunisela futhi, ngenxa yalokho, sinciphisa izindleko zokukhiqiza. Ukuze kuzuzwe ukusetshenziswa kahle kwamanzi ekucheleni, kubalulekile ukuqonda ukuhlukaniswa kwesimo sezulu kusukela esifundeni lapho litshalwe khona.

Imfuneko yamanzi okunisela ibizwa ngalo mehluko phakathi kwe-evapotranspiration.

isomiso nokubaluleka kwesibukeli
I-athikili ehlobene:
Isibukeli Sesomiso

Shiya umbono wakho

Ikheli lakho le ngeke ishicilelwe. Ezidingekayo ibhalwe nge *

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  1. Ubhekele imininingwane: Miguel Ángel Gatón
  2. Inhloso yedatha: Lawula Ugaxekile, ukuphathwa kwamazwana.
  3. Ukusemthethweni: Imvume yakho
  4. Ukuxhumana kwemininingwane: Imininingwane ngeke idluliselwe kubantu besithathu ngaphandle kwesibopho esisemthethweni.
  5. Isitoreji sedatha: Idatabase ebanjwe yi-Occentus Networks (EU)
  6. Amalungelo: Nganoma yisiphi isikhathi ungakhawulela, uthole futhi ususe imininingwane yakho.