From biodiversity to geodiversity and soil diversity. A spatial understanding of soil in ecological studies of the forest landscape

From biodiversity to geodiversity and soil diversity. A spatial understanding of soil in ecological studies of the forest landscape. In field ecology we have to satisfy 'geographical' objectives because of the spatial nature of the landscape, rather than theoretical 'typological'...

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Published in:Journal of tropical forest science Vol. 12; no. 2; pp. 388 - 405
Main Author: Thwaites, R.N. (Queensland Univ., St Lucia, Qld 4072 (Australia). School of Land and Food Sciences and Co-operative Research Centre for Tropical Rainforest Ecology and Management)
Format: Journal Article
Language:English
Published: Forest Research Institute Malaysia 01-04-2000
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Abstract From biodiversity to geodiversity and soil diversity. A spatial understanding of soil in ecological studies of the forest landscape. In field ecology we have to satisfy 'geographical' objectives because of the spatial nature of the landscape, rather than theoretical 'typological' objectives. To understand and maintain biodiversity we must have some understanding of geodiversity. We therefore have to adjust our attitude to the dynamism of the soil system accodingly through geoecology. This is best undertaken by using soil-landscape analysis within a geomorphological paradigm which treats soil as layers of material with spatial extent. The recommendation is for viewing a 3-dimensional micro-catchment, or 'catenary unit', rather than the soil profile, as the fundamantal natural unit of study. The soil profile, or pedon, is best used for observation and generic classification only. Soil diversity is best expressed as variations in selected soil attributes that are ecologically relevant rather than preconceived soil types developed for agricultural or other purposes. Classifying soil atrributes by 'fuzzy logic' (or by other mathematical clustering means) suits this form of spatial analysis for soil attribute prediction. A fuzzy classification gives a set of multiple possibilities of soil attributes at any one point, compared with an intuitive conjecture that is likely from a soil profile classification.
AbstractList From biodiversity to geodiversity and soil diversity. A spatial understanding of soil in ecological studies of the forest landscape. In field ecology we have to satisfy 'geographical' objectives because of the spatial nature of the landscape, rather than theoretical 'typological' objectives. To understand and maintain biodiversity we must have some understanding of geodiversity. We therefore have to adjust our attitude to the dynamism of the soil system accodingly through geoecology. This is best undertaken by using soil-landscape analysis within a geomorphological paradigm which treats soil as layers of material with spatial extent. The recommendation is for viewing a 3-dimensional micro-catchment, or 'catenary unit', rather than the soil profile, as the fundamantal natural unit of study. The soil profile, or pedon, is best used for observation and generic classification only. Soil diversity is best expressed as variations in selected soil attributes that are ecologically relevant rather than preconceived soil types developed for agricultural or other purposes. Classifying soil atrributes by 'fuzzy logic' (or by other mathematical clustering means) suits this form of spatial analysis for soil attribute prediction. A fuzzy classification gives a set of multiple possibilities of soil attributes at any one point, compared with an intuitive conjecture that is likely from a soil profile classification.
In field ecology we have to satisfy 'geographical' objectives because of the spatial nature of the landscape, rather than theoretical 'typological' objectives. To understand and maintain biodiversity we must have some understanding of geodiversity. We therefore have to adjust our attitude to the dynamism of the soil system accordingly through geoecology. This is best undertaken by using soil-landscape analysis within a geomorphological paradigm which treats soil as layers of material with spatial extent. The recommendation is for viewing a 3-dimensional micro-catchment, or 'catenary unit', rather than the soil profile, as the fundamental natural unit of study. The soil profile, or pedon, is best used for observation and generic classification only. Soil diversity is best expressed as variations in selected soil attributes that are ecologically relevant rather than preconceived soil types developed for agricultural or other puproses. Classifying soil attributes by 'fuzzy logic' (or by other mathematical clustering means) suits this form of spatial analysis for soil attribute prediction. A fuzzy classification gives a set of multiple possibilities of soil attributes at any one point, compared with an intuitive conjecture that is likely from a soil profile classification. Dalam ekologi lapangan kita mestilah memenuhi objektif geografi kerana ruang semula jadi landskap, lebih daripada objektif tipologi secara teori. Untuk memahami dan mengekalkan biodiversiti kita mestilah memahami sedikit sebanyak mengenai geodiversiti. Oleh itu mestilah menyesuaikan sikap kita terhadap dinamis sistem tanah melalui geoekologi. Ini dapat dilakukan dengan menggunakan analisis landskap-tanah dalam satu paradigma geomorfologi yang menganggap tanah sebagai satu lapisan bahan dengan tambahan ruang. Cadangan tersebut adalah untuk melihat mikro-tadahan tiga dimensi, atau 'unit katenari', lebih daripada profil tanah, sebagai satu unit semula jadi asas dalam kajian tersebut. Profil tanah, atau pedon, hanya sesuai digunakan untuk cerapan dan pengkelasan umum sahaja. Diversiti tanah diungkapkan sebagai kepelbagaian dalam sifat-sifat tanah yang terpilih yang berkaitan secara ekologi berbanding dengan jenis tanah yang membenih yang dibangunkan untuk pertanian atau tujuan lain. Mengkelaskan sifat-sifat tanah secara 'logik kabur' (atau secara kelompok matematik yang lain) sesuai dengan bentuk analisis ruang untuk ramalan ciri-ciri tanah. Pengkelasan kabur memberikan satu set kemungkinan berganda dalam ciri-ciri tanah pada mana-mana tempat, berbanding dengan agakan gerak hati yang mungkin daripada pengkelasan profil tanah.
Author Thwaites, R.N. (Queensland Univ., St Lucia, Qld 4072 (Australia). School of Land and Food Sciences and Co-operative Research Centre for Tropical Rainforest Ecology and Management)
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Snippet From biodiversity to geodiversity and soil diversity. A spatial understanding of soil in ecological studies of the forest landscape. In field ecology we have...
In field ecology we have to satisfy 'geographical' objectives because of the spatial nature of the landscape, rather than theoretical 'typological' objectives....
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StartPage 388
SubjectTerms Agrology
BIODIVERSIDAD
BIODIVERSITE
BIODIVERSITY
BOSQUES
CLASIFICACION DE SUELOS
CLASSIFICATION DES SOLS
ECOLOGIA
ECOLOGIA FORESTAL
ECOLOGICAL SOIL TYPES
ECOLOGIE
ECOLOGIE FORESTIERE
ECOLOGY
ENQUETE PEDOLOGIQUE
FOREST ECOLOGY
FOREST SOILS
FORESTS
FORET
Landscape ecology
Pedogenesis
RECONOCIMIENTO DE SUELOS
SOIL
SOIL CLASSIFICATION
Soil composition
Soil ecology
Soil plant interactions
Soil science
SOIL SURVEYS
SOL
SOL DE FORET
SUELO
SUELO FORESTAL
TIPOS ECOLOGICOS DE SUELOS
Tropical soils
TYPE DE SOL ECOLOGIQUE
Title From biodiversity to geodiversity and soil diversity. A spatial understanding of soil in ecological studies of the forest landscape
URI https://www.jstor.org/stable/23616473
Volume 12
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