{"id":{"repo_id":"greece","oai_identifier":"oai:10442/1288"},"canonical_url":"https://search.dev.ndltd.org/etd/greece/oai:10442/1288","repository":{"repo_id":"greece","name":"Greek National Archive of PhD Theses","base_url":"https://phdtheses.ekt.gr/eadd_oai/request"},"display":{"title":"ΤΑΞΙΝΟΜΗΣΗ ΚΑΙ ΕΚΤΙΜΗΣΗ ΠΕΔΙΝΩΝ ΕΔΑΦΩΝ ΛΕΥΚΟΚΑΛΛΙΕΡΓΕΙΑΣ ΣΤΗ Β. ΕΛΛΑΔΑ","abstract":"PHYSICAL CHARACTERISTICS OF THE SOIL ARE THE MOST IMPORTANT FACTORS FOR POPLAR GROWTH AND MORE SPECIFICALLY SOIL TEXTURE, SOIL STRUCTURE AND HYDROLOGICAL CONDITIONS. BEST SITES FOR POPLAR CLASSES I AND II, ARE SANDY, LOAMY AND CLAY LOAMYSOILS WITH GROUND WATER SURFACE BETWEEN 80CM AND 250CM MOST OF THE YEAR. LIGHTTEXTURED SOILS, LOAMY SAND WITH RICH IN ORGANIC MATTER HORIZONS IN DEPTH MORE THAN 80CM, OR CLAY AND SILTY CLAY SOILS WITH ADEQUATE ORGANIC MATTER WITH GOOD AERATION AND MOISTURE CLASSIFIED IN THE II CLASS WHEN THE SURFACE OF GROUND WATER OCCURS BETWEEN 80CM AND 250CM, MEADIUM QUALITY SITES, CLASS III, ARE SOILS LOAMY SAND WITH FINE TEXTURED LAYERS IN MORE THAN 80CM DEPTH, WITH PLATY STRUCTURE AND LOW ORGANIC MATTER CONTENT. SITE QUALITY CLASSES IV AND V ARE SANDY SOILS AND SOILS WITH GROUND WATER LEVEL IN DEPTH LESS THAN 80CM OR MORE THAN 250CM.SOILS HEAVY TEXTURED WITH LOW ORGANIC MATTER CONTENT AND COMPACTED AS WELL AS SALINE AND ALKALINE SOILS WAS CLASSIFIED IN THE IV AND V SITE PRODUCTIVITY CLASSES.","abstract_html":"PHYSICAL CHARACTERISTICS OF THE SOIL ARE THE MOST IMPORTANT FACTORS FOR POPLAR GROWTH AND MORE SPECIFICALLY SOIL TEXTURE, SOIL STRUCTURE AND HYDROLOGICAL CONDITIONS. BEST SITES FOR POPLAR CLASSES I AND II, ARE SANDY, LOAMY AND CLAY LOAMYSOILS WITH GROUND WATER SURFACE BETWEEN 80CM AND 250CM MOST OF THE YEAR. LIGHTTEXTURED SOILS, LOAMY SAND WITH RICH IN ORGANIC MATTER HORIZONS IN DEPTH MORE THAN 80CM, OR CLAY AND SILTY CLAY SOILS WITH ADEQUATE ORGANIC MATTER WITH GOOD AERATION AND MOISTURE CLASSIFIED IN THE II CLASS WHEN THE SURFACE OF GROUND WATER OCCURS BETWEEN 80CM AND 250CM, MEADIUM QUALITY SITES, CLASS III, ARE SOILS LOAMY SAND WITH FINE TEXTURED LAYERS IN MORE THAN 80CM DEPTH, WITH PLATY STRUCTURE AND LOW ORGANIC MATTER CONTENT. SITE QUALITY CLASSES IV AND V ARE SANDY SOILS AND SOILS WITH GROUND WATER LEVEL IN DEPTH LESS THAN 80CM OR MORE THAN 250CM.SOILS HEAVY TEXTURED WITH LOW ORGANIC MATTER CONTENT AND COMPACTED AS WELL AS SALINE AND ALKALINE SOILS WAS CLASSIFIED IN THE IV AND V SITE PRODUCTIVITY CLASSES.","abstract_has_math":false,"creators":["Χατζόπουλος, Αριστείδης"],"institution":"Αριστοτέλειο Πανεπιστήμιο Θεσσαλονίκης (ΑΠΘ)","degree_name":null,"degree_level":null,"degree_discipline":null,"degree_department":null,"school":null,"contributors":[],"advisors":[],"committee_chairs":[],"committee_members":[],"year":1990,"date_issued":"1990","date_published":"1990","updated_at":"2026-07-24T02:24:49Z","subjects":["Poplar cultivation","POPLAR GROWTH","SOIL CLASSIFICATION","SOIL FACTORS","ΕΔΑΦΟΛΟΓΙΚΟΙ ΠΑΡΑΓΟΝΤΕΣ-ΑΝΑΠΤΥΞΗ ΛΕΥΚΗΣ","ΤΑΞΙΝΟΜΗΣΗ ΕΔΑΦΩΝ-ΛΕΥΚΟΚΑΛΛΙΕΡΓΕΙΑ","ΦΥΣΙΚΕΣ ΚΑΙ ΧΗΜΙΚΕΣ ΙΔΙΟΤΗΤΕΣ ΤΟΥ ΕΔΑΦΟΥΣ","Γεωπονικές Επιστήμες και Κτηνιατρική","Agricultural and Veterinary Sciences","Γεωπονία, Δασολογία και Αλιεία","Agriculture, Forestry and Fisheries"],"languages":["gre"],"rights":[],"rights_urls":[],"identifier_entries":[{"key":"dc:identifier","label":"Identifier","values":["10.12681/eadd/1288"],"render_values":[{"text":"10.12681/eadd/1288","href":"https://doi.org/10.12681/eadd/1288","code":true}]}]},"links":{"outbound_url":"http://hdl.handle.net/10442/hedi/1288","outbound_label":"Handle","outbound_source":"dc:identifier"},"metadata_groups":[{"id":"people","label":"People","entries":[{"key":"dc:creator","label":"Author","values":["Χατζόπουλος, Αριστείδης"]}]},{"id":"academic_context","label":"Academic Context","entries":[{"key":"dc:date","label":"Dc Date","values":["1990"]},{"key":"dc:publisher","label":"Institution","values":["Αριστοτέλειο Πανεπιστήμιο Θεσσαλονίκης (ΑΠΘ)","Aristotle University Of Thessaloniki (AUTH)"]},{"key":"dc:type","label":"Dc Type","values":["PhD Thesis"]}]},{"id":"subjects_keywords","label":"Subjects and Keywords","entries":[{"key":"dc:subject","label":"Dc Subject","values":["Poplar cultivation","POPLAR GROWTH","SOIL CLASSIFICATION","SOIL FACTORS","ΕΔΑΦΟΛΟΓΙΚΟΙ ΠΑΡΑΓΟΝΤΕΣ-ΑΝΑΠΤΥΞΗ ΛΕΥΚΗΣ","ΤΑΞΙΝΟΜΗΣΗ ΕΔΑΦΩΝ-ΛΕΥΚΟΚΑΛΛΙΕΡΓΕΙΑ","ΦΥΣΙΚΕΣ ΚΑΙ ΧΗΜΙΚΕΣ ΙΔΙΟΤΗΤΕΣ ΤΟΥ ΕΔΑΦΟΥΣ","Γεωπονικές Επιστήμες και Κτηνιατρική","Agricultural and Veterinary Sciences","Γεωπονία, Δασολογία και Αλιεία","Agriculture, Forestry and Fisheries"]}]},{"id":"language_rights","label":"Language and Rights","entries":[{"key":"dc:language","label":"Dc Language","values":["gre"]}]},{"id":"identifiers","label":"Identifiers","entries":[{"key":"dc:identifier","label":"Identifier","values":["10.12681/eadd/1288","http://hdl.handle.net/10442/hedi/1288"]}]},{"id":"additional","label":"Additional Metadata","entries":[{"key":"dc:description","label":"Description","values":["PHYSICAL CHARACTERISTICS OF THE SOIL ARE THE MOST IMPORTANT FACTORS FOR POPLAR GROWTH AND MORE SPECIFICALLY SOIL TEXTURE, SOIL STRUCTURE AND HYDROLOGICAL CONDITIONS. BEST SITES FOR POPLAR CLASSES I AND II, ARE SANDY, LOAMY AND CLAY LOAMYSOILS WITH GROUND WATER SURFACE BETWEEN 80CM AND 250CM MOST OF THE YEAR. LIGHTTEXTURED SOILS, LOAMY SAND WITH RICH IN ORGANIC MATTER HORIZONS IN DEPTH MORE THAN 80CM, OR CLAY AND SILTY CLAY SOILS WITH ADEQUATE ORGANIC MATTER WITH GOOD AERATION AND MOISTURE CLASSIFIED IN THE II CLASS WHEN THE SURFACE OF GROUND WATER OCCURS BETWEEN 80CM AND 250CM, MEADIUM QUALITY SITES, CLASS III, ARE SOILS LOAMY SAND WITH FINE TEXTURED LAYERS IN MORE THAN 80CM DEPTH, WITH PLATY STRUCTURE AND LOW ORGANIC MATTER CONTENT. SITE QUALITY CLASSES IV AND V ARE SANDY SOILS AND SOILS WITH GROUND WATER LEVEL IN DEPTH LESS THAN 80CM OR MORE THAN 250CM.SOILS HEAVY TEXTURED WITH LOW ORGANIC MATTER CONTENT AND COMPACTED AS WELL AS SALINE AND ALKALINE SOILS WAS CLASSIFIED IN THE IV AND V SITE PRODUCTIVITY CLASSES.","ΣΠΟΥΔΑΙΟΤΕΡΟΙ ΟΙΚΟΛΟΓΙΚΟΙ ΠΑΡΑΓΟΝΤΕΣ ΑΝΑΠΤΥΞΗΣ ΤΗΣ ΛΕΥΚΗΣ ΕΙΝΑΙ ΟΙ ΦΥΣΙΚΕΣ ΙΔΙΟΤΗΤΕΣ ΤΟΥ ΕΔΑΦΟΥΣ ΚΑΙ ΚΥΡΙΩΣ Η ΥΦΗ, Η ΔΟΜΗ ΚΑΙ ΟΙ ΥΔΡΟΛΟΓΙΚΕΣ ΣΥΝΘΗΚΕΣ. ΠΟΛΥ ΚΑΛΟΙ ΣΤΑΘΜΟΙ ΛΕΥΚΟΚΑΛΛΙΕΡΓΕΙΑΣ, ΙΗΣ ΚΑΙ ΙΙΗΣ ΚΛΑΣΗΣ ΕΙΝΑΙ ΕΔΑΦΗ ΑΜΜΟΠΗΛΩΔΗ, ΠΗΛΩΔΗ, ΑΡΓΙΛΟΠΗΛΩΔΗ ΜΕ ΥΠΟΓΕΙΑ ΣΤΑΘΜΗ ΝΕΡΟΥ ΚΑΤΑ ΤΟ ΜΕΓΑΛΥΤΕΡΟ ΔΙΑΣΤΗΜΑ ΤΗΣ ΒΛΑΣΤΗΤΙΚΗΣ ΠΕΡΙΟΔΟΥ ΣΕ ΒΑΘΟΣ ΑΠΟ 80CM ΜΕΧΡΙ 250CM. ΕΛΑΦΡΑΣ ΜΗΧΑΝΙΚΗΣ ΣΥΣΤΑΣΗΣ ΕΔΑΦΗ, ΠΗΛΟΑΜΜΩΔΗ, ΜΕ ΟΡΙΖΟΝΤΕΣ, ΣΕ ΒΑΘΟΣ ΚΑΤΩ ΑΠΟ 80CM, ΠΛΟΥΣΙΟΥΣ ΣΕ ΟΡΓΑΝΙΚΗ ΟΥΣΙΑ ΚΑΘΩΣ ΚΑΙ ΕΔΑΦΗ ΑΡΓΙΛΩΔΗ ΚΑΙ ΙΛΥΟΑΡΓΙΛΩΔΗ ΜΕ ΕΠΑΡΚΗ ΟΡΓΑΝΙΚΗ ΟΥΣΙΑ ΚΑΙ ΜΕ ΚΑΛΕΣ ΣΥΝΘΗΚΕΣ ΑΕΡΙΣΜΟΥ ΚΑΙ ΥΓΡΑΣΙΑΣ ΚΑΤΑΤΑΧΘΗΚΑΝ ΣΤΗΝ ΙΙΗ ΠΟΙΟΤΙΚΗ ΚΛΑΣΗ. Η ΥΠΟΓΕΙΑ ΣΤΑΘΜΗ ΒΡΙΣΚΕΤΑΙ ΣΕ ΒΑΘΟΣ ΑΠΟ 80CM ΜΕΧΡΙ 250CM. ΜΕΤΡΙΟΙ ΣΤΑΘΜΟΙ, ΙΙΙΗΣ ΚΛΑΣΗΣ ΠΟΙΟΤΗΤΑΣ, ΕΙΝΑΙ ΕΔΑΦΗ ΚΥΡΙΩΣ ΠΗΛΟΑΜΜΩΔΗ ΜΕ ΛΕΠΤΟΤΕΡΟΥΣ ΟΡΙΖΟΝΤΕΣ ΚΑΤΩ ΑΠΟ 80CM ΒΑΘΟΣ, ΦΥΛΛΟΕΙΔΟΥΣ ΔΟΜΗΣ, ΦΤΩΧΟΥΣ ΣΕ ΟΡΓΑΝΙΚΗ ΟΥΣΙΑ. ΣΤΑΘΜΟΙ IVΗΣ ΚΑΙ VΗΣ ΚΛΑΣΗΣ ΕΙΝΑΙ ΕΔΑΦΗ ΑΜΜΩΔΗ ΚΑΘΩΣ ΚΑΙ ΕΔΑΦΗ ΜΕ ΥΠΟΓΕΙΑ ΣΤΑΘΜΗ ΝΕΡΟΥ ΠΑΝΩ ΑΠΟ 80CM'Η ΚΑΤΩ ΑΠΟ 250CM. ΕΔΑΦΗ ΕΠΙΣΗΣ ΒΑΡΙΑΣ ΜΗΧΑΝΙΚΗΣ ΣΥΣΤΑΣΗΣ, ΦΤΩΧΑ ΣΕ ΟΡΓΑΝΙΚΗ ΟΥΣΙΑ ΚΑΙ ΣΥΜΠΙΕΣΜΕΝΑ ΚΑΘΩΣ ΚΑΙ ΑΛΑΤΟΥΧΑ ΚΑΙ ΑΛΚΑΛΙΩΜΕΝΑ ΚΑΤΑΤΑΧΘΗΚΑΝ ΣΤΗΝ IVΗ ΚΑΙ VΗ ΚΛΑΣΗ ΠΟΙΟΤΗΤΑΣ."]},{"key":"dc:title","label":"Title","values":["ΤΑΞΙΝΟΜΗΣΗ ΚΑΙ ΕΚΤΙΜΗΣΗ ΠΕΔΙΝΩΝ ΕΔΑΦΩΝ ΛΕΥΚΟΚΑΛΛΙΕΡΓΕΙΑΣ ΣΤΗ Β. ΕΛΛΑΔΑ","LOW-LAND SOIL CLASSIFICATION AND ASSESSMENT FOR POPLAR CULTIVATION IN NORTH GREECE"]}]}],"canonical_facts":{"dc:creator":["Χατζόπουλος, Αριστείδης"],"dc:date":["1990"],"dc:description":["PHYSICAL CHARACTERISTICS OF THE SOIL ARE THE MOST IMPORTANT FACTORS FOR POPLAR GROWTH AND MORE SPECIFICALLY SOIL TEXTURE, SOIL STRUCTURE AND HYDROLOGICAL CONDITIONS. BEST SITES FOR POPLAR CLASSES I AND II, ARE SANDY, LOAMY AND CLAY LOAMYSOILS WITH GROUND WATER SURFACE BETWEEN 80CM AND 250CM MOST OF THE YEAR. LIGHTTEXTURED SOILS, LOAMY SAND WITH RICH IN ORGANIC MATTER HORIZONS IN DEPTH MORE THAN 80CM, OR CLAY AND SILTY CLAY SOILS WITH ADEQUATE ORGANIC MATTER WITH GOOD AERATION AND MOISTURE CLASSIFIED IN THE II CLASS WHEN THE SURFACE OF GROUND WATER OCCURS BETWEEN 80CM AND 250CM, MEADIUM QUALITY SITES, CLASS III, ARE SOILS LOAMY SAND WITH FINE TEXTURED LAYERS IN MORE THAN 80CM DEPTH, WITH PLATY STRUCTURE AND LOW ORGANIC MATTER CONTENT. SITE QUALITY CLASSES IV AND V ARE SANDY SOILS AND SOILS WITH GROUND WATER LEVEL IN DEPTH LESS THAN 80CM OR MORE THAN 250CM.SOILS HEAVY TEXTURED WITH LOW ORGANIC MATTER CONTENT AND COMPACTED AS WELL AS SALINE AND ALKALINE SOILS WAS CLASSIFIED IN THE IV AND V SITE PRODUCTIVITY CLASSES.","ΣΠΟΥΔΑΙΟΤΕΡΟΙ ΟΙΚΟΛΟΓΙΚΟΙ ΠΑΡΑΓΟΝΤΕΣ ΑΝΑΠΤΥΞΗΣ ΤΗΣ ΛΕΥΚΗΣ ΕΙΝΑΙ ΟΙ ΦΥΣΙΚΕΣ ΙΔΙΟΤΗΤΕΣ ΤΟΥ ΕΔΑΦΟΥΣ ΚΑΙ ΚΥΡΙΩΣ Η ΥΦΗ, Η ΔΟΜΗ ΚΑΙ ΟΙ ΥΔΡΟΛΟΓΙΚΕΣ ΣΥΝΘΗΚΕΣ. ΠΟΛΥ ΚΑΛΟΙ ΣΤΑΘΜΟΙ ΛΕΥΚΟΚΑΛΛΙΕΡΓΕΙΑΣ, ΙΗΣ ΚΑΙ ΙΙΗΣ ΚΛΑΣΗΣ ΕΙΝΑΙ ΕΔΑΦΗ ΑΜΜΟΠΗΛΩΔΗ, ΠΗΛΩΔΗ, ΑΡΓΙΛΟΠΗΛΩΔΗ ΜΕ ΥΠΟΓΕΙΑ ΣΤΑΘΜΗ ΝΕΡΟΥ ΚΑΤΑ ΤΟ ΜΕΓΑΛΥΤΕΡΟ ΔΙΑΣΤΗΜΑ ΤΗΣ ΒΛΑΣΤΗΤΙΚΗΣ ΠΕΡΙΟΔΟΥ ΣΕ ΒΑΘΟΣ ΑΠΟ 80CM ΜΕΧΡΙ 250CM. ΕΛΑΦΡΑΣ ΜΗΧΑΝΙΚΗΣ ΣΥΣΤΑΣΗΣ ΕΔΑΦΗ, ΠΗΛΟΑΜΜΩΔΗ, ΜΕ ΟΡΙΖΟΝΤΕΣ, ΣΕ ΒΑΘΟΣ ΚΑΤΩ ΑΠΟ 80CM, ΠΛΟΥΣΙΟΥΣ ΣΕ ΟΡΓΑΝΙΚΗ ΟΥΣΙΑ ΚΑΘΩΣ ΚΑΙ ΕΔΑΦΗ ΑΡΓΙΛΩΔΗ ΚΑΙ ΙΛΥΟΑΡΓΙΛΩΔΗ ΜΕ ΕΠΑΡΚΗ ΟΡΓΑΝΙΚΗ ΟΥΣΙΑ ΚΑΙ ΜΕ ΚΑΛΕΣ ΣΥΝΘΗΚΕΣ ΑΕΡΙΣΜΟΥ ΚΑΙ ΥΓΡΑΣΙΑΣ ΚΑΤΑΤΑΧΘΗΚΑΝ ΣΤΗΝ ΙΙΗ ΠΟΙΟΤΙΚΗ ΚΛΑΣΗ. Η ΥΠΟΓΕΙΑ ΣΤΑΘΜΗ ΒΡΙΣΚΕΤΑΙ ΣΕ ΒΑΘΟΣ ΑΠΟ 80CM ΜΕΧΡΙ 250CM. ΜΕΤΡΙΟΙ ΣΤΑΘΜΟΙ, ΙΙΙΗΣ ΚΛΑΣΗΣ ΠΟΙΟΤΗΤΑΣ, ΕΙΝΑΙ ΕΔΑΦΗ ΚΥΡΙΩΣ ΠΗΛΟΑΜΜΩΔΗ ΜΕ ΛΕΠΤΟΤΕΡΟΥΣ ΟΡΙΖΟΝΤΕΣ ΚΑΤΩ ΑΠΟ 80CM ΒΑΘΟΣ, ΦΥΛΛΟΕΙΔΟΥΣ ΔΟΜΗΣ, ΦΤΩΧΟΥΣ ΣΕ ΟΡΓΑΝΙΚΗ ΟΥΣΙΑ. ΣΤΑΘΜΟΙ IVΗΣ ΚΑΙ VΗΣ ΚΛΑΣΗΣ ΕΙΝΑΙ ΕΔΑΦΗ ΑΜΜΩΔΗ ΚΑΘΩΣ ΚΑΙ ΕΔΑΦΗ ΜΕ ΥΠΟΓΕΙΑ ΣΤΑΘΜΗ ΝΕΡΟΥ ΠΑΝΩ ΑΠΟ 80CM'Η ΚΑΤΩ ΑΠΟ 250CM. ΕΔΑΦΗ ΕΠΙΣΗΣ ΒΑΡΙΑΣ ΜΗΧΑΝΙΚΗΣ ΣΥΣΤΑΣΗΣ, ΦΤΩΧΑ ΣΕ ΟΡΓΑΝΙΚΗ ΟΥΣΙΑ ΚΑΙ ΣΥΜΠΙΕΣΜΕΝΑ ΚΑΘΩΣ ΚΑΙ ΑΛΑΤΟΥΧΑ ΚΑΙ ΑΛΚΑΛΙΩΜΕΝΑ ΚΑΤΑΤΑΧΘΗΚΑΝ ΣΤΗΝ IVΗ ΚΑΙ VΗ ΚΛΑΣΗ ΠΟΙΟΤΗΤΑΣ."],"dc:identifier":["10.12681/eadd/1288","http://hdl.handle.net/10442/hedi/1288"],"dc:language":["gre"],"dc:publisher":["Αριστοτέλειο Πανεπιστήμιο Θεσσαλονίκης (ΑΠΘ)","Aristotle University Of Thessaloniki (AUTH)"],"dc:subject":["Poplar cultivation","POPLAR GROWTH","SOIL CLASSIFICATION","SOIL FACTORS","ΕΔΑΦΟΛΟΓΙΚΟΙ ΠΑΡΑΓΟΝΤΕΣ-ΑΝΑΠΤΥΞΗ ΛΕΥΚΗΣ","ΤΑΞΙΝΟΜΗΣΗ ΕΔΑΦΩΝ-ΛΕΥΚΟΚΑΛΛΙΕΡΓΕΙΑ","ΦΥΣΙΚΕΣ ΚΑΙ ΧΗΜΙΚΕΣ ΙΔΙΟΤΗΤΕΣ ΤΟΥ ΕΔΑΦΟΥΣ","Γεωπονικές Επιστήμες και Κτηνιατρική","Agricultural and Veterinary Sciences","Γεωπονία, Δασολογία και Αλιεία","Agriculture, Forestry and Fisheries"],"dc:title":["ΤΑΞΙΝΟΜΗΣΗ ΚΑΙ ΕΚΤΙΜΗΣΗ ΠΕΔΙΝΩΝ ΕΔΑΦΩΝ ΛΕΥΚΟΚΑΛΛΙΕΡΓΕΙΑΣ ΣΤΗ Β. ΕΛΛΑΔΑ","LOW-LAND SOIL CLASSIFICATION AND ASSESSMENT FOR POPLAR CULTIVATION IN NORTH GREECE"],"dc:type":["PhD Thesis"]},"updated_at":"2026-07-24T02:24:49Z"}