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פותח על ידי קלירמאש פתרונות בע"מ -
Soil hydraulic properties as stochastic processes: II. Errors of estimates in a heterogeneous field.
Year:
1982
Authors :
רוסו, דוד
;
.
Volume :
46
Co-Authors:
Russo, D., Div. of Soil Physics, ARO, Bet Dagan, Israel.
Bresler, E., Div. of Soil Physics, ARO, Bet Dagan, Israel.
Facilitators :
From page:
20
To page:
26
(
Total pages:
7
)
Abstract:
Results of integral scales and coefficient of variations from Part I are applied to evaluate errors in estimating average values of several hydraulic properties. Based on the Ergodic Hypothesis and on standard statistical theory, an equation is derived to calculate the total field area and number of measurements needed to estimate (for a prescribed error) ensemble averages of a given hydraulic property. -from Authors
Note:
Related Files :
integral scale
kriging.
soil water retentivity
Spatial variability
עוד תגיות
תוכן קשור
More details
DOI :
Article number:
Affiliations:
Database:
סקופוס
Publication Type:
Language:
אנגלית
Editors' remarks:
ID:
26427
Last updated date:
02/03/2022 17:27
Creation date:
17/04/2018 00:22
Scientific Publication
Soil hydraulic properties as stochastic processes: II. Errors of estimates in a heterogeneous field.
46
Russo, D., Div. of Soil Physics, ARO, Bet Dagan, Israel.
Bresler, E., Div. of Soil Physics, ARO, Bet Dagan, Israel.
Soil hydraulic properties as stochastic processes: II. Errors of estimates in a heterogeneous field.
Results of integral scales and coefficient of variations from Part I are applied to evaluate errors in estimating average values of several hydraulic properties. Based on the Ergodic Hypothesis and on standard statistical theory, an equation is derived to calculate the total field area and number of measurements needed to estimate (for a prescribed error) ensemble averages of a given hydraulic property. -from Authors
Scientific Publication
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