Reduced evapotranspiration following the removal of deeprootedtree spe translation - Reduced evapotranspiration following the removal of deeprootedtree spe Indonesian how to say

Reduced evapotranspiration followin

Reduced evapotranspiration following the removal of deeprooted
tree species, such as Eucalyptus mat-ginata Sm., in
wrstern Australia has resulted in increased water storage in
below ground aquifers (Sharmaet al. 1987; Peck and Williamson
1987) and increased salination of groundwater and streamflow
in areas subject to this phenomenon (MacPherson and Peck
1987). However, this effect would only be sustained with
permanent clearance. In areas with frequent low cloud or fog,
substantial inputs of water occur from canopy drip. Trees trap
moisture from these sources more efficiently than lower forms
of vegetation (Goudie 1990) and, where canopy drip forms a
major contribution to site water inputs, clear-cutting may result
in a net decrease in soil moisture until the forest regrows.
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Reduced evapotranspiration following the removal of deeprootedtree species, such as Eucalyptus mat-ginata Sm., inwrstern Australia has resulted in increased water storage inbelow ground aquifers (Sharmaet al. 1987; Peck and Williamson1987) and increased salination of groundwater and streamflowin areas subject to this phenomenon (MacPherson and Peck1987). However, this effect would only be sustained withpermanent clearance. In areas with frequent low cloud or fog,substantial inputs of water occur from canopy drip. Trees trapmoisture from these sources more efficiently than lower formsof vegetation (Goudie 1990) and, where canopy drip forms amajor contribution to site water inputs, clear-cutting may resultin a net decrease in soil moisture until the forest regrows.
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Mengurangi evapotranspirasi setelah penghapusan deeprooted
. Jenis pohon, seperti Eucalyptus mat-ginata Sm, di
wrstern Australia telah menghasilkan peningkatan penyimpanan air di
bawah akuifer tanah (Sharmaet al 1987;. Peck dan Williamson
1987) dan peningkatan salinasi air tanah dan debit sungai
di daerah tunduk pada fenomena ini (MacPherson dan Peck
1987). Namun, efek ini hanya akan dipertahankan dengan
izin permanen. Di daerah dengan sering awan rendah atau kabut,
masukan substansial air terjadi dari kanopi menetes. Pohon perangkap
uap air dari sumber-sumber ini lebih efisien daripada bentuk yang lebih rendah
dari vegetasi (Goudie 1990) dan, di mana bentuk tetes kanopi
kontribusi besar untuk input air situs, tebang habis dapat mengakibatkan
penurunan bersih dalam kelembaban tanah sampai hutan tumbuh kembali.
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