Open AccessTemporal stability of stratifications using different dendrometric variables and geostatistical interpolation
Author(s) -
Aliny Aparecida dos Reis,
Andressa Ribeiro,
Rafaella Carvalho Mayrinck,
José Márcio de Mello,
Anderson Pedro Bernardina Batista,
Antônio Carlos Ferraz Filho
Publication year - 2022
Publication title -
ciência florestal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.381
H-Index - 21
eISSN - 1980-5098
pISSN - 0103-9954
DOI - 10.5902/1980509843274
Subject(s) - basal area , kriging , mathematics , statistics , stratum , forest inventory , environmental science , forestry , hydrology (agriculture) , geography , forest management , geology , paleontology , geotechnical engineering
Stratifying a forest results in more precise and cheaper inventories. This study aimed to select the stratifying variable that estimates more precise and stable inventory over the years for a eucalyptus plantation in Minas Gerais state, Brazil. The continuous forest inventory was performed annually from 2.7 to 6.8 years, and based on the field measurements, arithmetic mean diameter (d), height (h), dominant height (Hdom), basal area (G), volume (V), and mean annual increment in volume (MAI) were calculated. Semivariograms were generated and the exponential, spherical and Gaussian models were fit for each stratifying variable for each measurement date. The models were assessed by the reduced mean error and its deviation, being the exponential model selected. Maps showing the spatial distribution of all variables were generated for each measurement age, using ordinary kriging. Next, the study area was divided in four strata based on each stratifying variable for each measurement age. The stability of each stratifying variables for each measurement age were assessed by: 1) coincident strata area; 2) stability of total strata area; 3) plot permanency on each stratum; and 4) inventory error using stratified random sampling procedures. All variables in all ages presented spatial dependence structure. G and Hdom were the stratifying variables that generated the most and the least coincident strata area over the years, respectively. G and height (h and Hdom) were the stratifying variables yielding the least and most plot stratum changes, respectively. The same trend was observed for the total strata area stability. Stratifying based on MAI and V yielded the smaller inventory error, and h and Hdom yielded the largest. G was selected as the best stratifying variable because it yielded small inventory errors and was the most stable variable in terms of coincident strata area, total strata area and plot stratum changes over the years.