{"id":{"repo_id":"greece","oai_identifier":"oai:10442/1292"},"canonical_url":"https://search.dev.ndltd.org/etd/greece/oai:10442/1292","repository":{"repo_id":"greece","name":"Greek National Archive of PhD Theses","base_url":"https://phdtheses.ekt.gr/eadd_oai/request"},"display":{"title":"ΙΣΟΡΡΟΠΙΑ ΑΝΤΑΛΛΑΞΙΜΩΝ-ΔΙΑΛΥΤΩΝ ΜΟΡΦΩΝ ΚΑΛΙΟΥ-ΜΑΓΝΗΣΙΟΥ ΣΤΑ ΕΔΑΦΗ","abstract":"THE EXCHANGE CHARACTERISTICS OF THE PAIR POTASSIUM-MAGNESIUM WAS STUDIED IN THREE REPRESENTATIVE RED MEDITERRANEAN SOILS USING THERMODYNAMIC PRINCIPLES. THE EXCHANGE REACTION WAS STUDIED IN BOTH DIRECTIONS IN AN ATTEMPT TO INVESTIGATE ITS REVERSIBILITY AND TO RELATE IT WITH THE MINERALOGICAL COMPOSITION OF THE SOILS. COMPARISON OF THE EXPERIMENTAL ISOTHERMS TO THE NON-PREFERENCE ISOTHERMS REVEALED THAT ALL THREE SOILS EXHIBITED HIGH PREFERENCE FOR POTASSIUM RELATIVE TO MAGNESIUM IONS. THE VALUES OF THE THERMODYNAMIC PARAMETERS KEQ, ΔGO, ΔΗO, ΔSO FOR THE K_MG EXCHANGE, CALCULATED FROM THE EXPERIMENTAL EXCHANGE ISOTHERMS, CONFIRMED THE SOILS' PREFERENCE FOR POTASSIUM. THESE VALUES WERE INFLUENCED MAINLY BY THE TYPE OF CLAY MINERALS PREVAILING IN THE CLAY FRACTION OF THE SOILS STUDIED. THE EXCHANGE REACTION OF THE PAIR K-MG WAS NOT COMPLETELY REVERSIBLE BUT EXHIBITED HYSTERESIS, THE MAGNITUDE OF WHICH WAS MORE PRONOUNCED IN THOSE SOILS WHERE MICA-TYPE MINERALS DOMINATED THE CLAY FRACTION. HYSTERESIS EFFECTS WERE ATTRIBUTED TO THE COMBINED ACTION OF CLAY FLOCCULATION DURING THE EXCHANGE EXPERIMENTS AND TO CHANGES OCCURRING IN THE MICA-TYPE MINERALS UPON POTASSIUM DEPLETION.","abstract_html":"THE EXCHANGE CHARACTERISTICS OF THE PAIR POTASSIUM-MAGNESIUM WAS STUDIED IN THREE REPRESENTATIVE RED MEDITERRANEAN SOILS USING THERMODYNAMIC PRINCIPLES. THE EXCHANGE REACTION WAS STUDIED IN BOTH DIRECTIONS IN AN ATTEMPT TO INVESTIGATE ITS REVERSIBILITY AND TO RELATE IT WITH THE MINERALOGICAL COMPOSITION OF THE SOILS. COMPARISON OF THE EXPERIMENTAL ISOTHERMS TO THE NON-PREFERENCE ISOTHERMS REVEALED THAT ALL THREE SOILS EXHIBITED HIGH PREFERENCE FOR POTASSIUM RELATIVE TO MAGNESIUM IONS. THE VALUES OF THE THERMODYNAMIC PARAMETERS KEQ, ΔGO, ΔΗO, ΔSO FOR THE K_MG EXCHANGE, CALCULATED FROM THE EXPERIMENTAL EXCHANGE ISOTHERMS, CONFIRMED THE SOILS' PREFERENCE FOR POTASSIUM. THESE VALUES WERE INFLUENCED MAINLY BY THE TYPE OF CLAY MINERALS PREVAILING IN THE CLAY FRACTION OF THE SOILS STUDIED. THE EXCHANGE REACTION OF THE PAIR K-MG WAS NOT COMPLETELY REVERSIBLE BUT EXHIBITED HYSTERESIS, THE MAGNITUDE OF WHICH WAS MORE PRONOUNCED IN THOSE SOILS WHERE MICA-TYPE MINERALS DOMINATED THE CLAY FRACTION. HYSTERESIS EFFECTS WERE ATTRIBUTED TO THE COMBINED ACTION OF CLAY FLOCCULATION DURING THE EXCHANGE EXPERIMENTS AND TO CHANGES OCCURRING IN THE MICA-TYPE MINERALS UPON POTASSIUM DEPLETION.","abstract_has_math":false,"creators":["Σινάνης, Κωνσταντίνος"],"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":["ACTIVITY COEFFICIENT OF EXCHANGEABLE IONS","ENTHALPYOF EXCHANGE","ENTROPY OF EXCHANGE","EXCHANGEABLE K","EXCHANGEABLE MG","FREE ENERGY OF EXCHANGE","HYSTERESIS OF EXCHANGE","ION EXCHANGE ISOTHERMS","ΑΝΤΑΛΛΑΞΙΜΟ MG","ΑΝΤΑΛΛΑΞΙΜΟ Κ","ΕΛΕΥΘΕΡΗ ΕΝΕΡΓΕΙΑ ΑΝΤΑΛΛΑΓΗΣ","ΕΝΘΑΠΙΑ ΑΝΤΑΛΛΑΓΗΣ","ΕΝΤΡΟΠΙΑ ΑΝΤΑΛΛΑΓΗΣ","ΙΣΟΘΕΡΜΟΙ ΑΝΤΑΛΛΑΓΗΣ","ΣΥΝΤΕΛΕΣΤΗΣ ΕΝΕΡΓΟΤΗΤΑΣ ΑΝΤΑΛΛΑΞΙΜΩΝ","ΥΣΤΕΡΗΣΗ ΑΝΤΑΛΛΑΓΗΣ","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/1292"],"render_values":[{"text":"10.12681/eadd/1292","href":"https://doi.org/10.12681/eadd/1292","code":true}]}]},"links":{"outbound_url":"http://hdl.handle.net/10442/hedi/1292","outbound_label":"Handle","outbound_source":"dc:identifier"},"metadata_groups":[{"id":"people","label":"People","entries":[{"key":"dc:creator","label":"Author","values":["Σινάνης, Κωνσταντίνος"]}]},{"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":["ACTIVITY COEFFICIENT OF EXCHANGEABLE IONS","ENTHALPYOF EXCHANGE","ENTROPY OF EXCHANGE","EXCHANGEABLE K","EXCHANGEABLE MG","FREE ENERGY OF EXCHANGE","HYSTERESIS OF EXCHANGE","ION EXCHANGE ISOTHERMS","ΑΝΤΑΛΛΑΞΙΜΟ MG","ΑΝΤΑΛΛΑΞΙΜΟ Κ","ΕΛΕΥΘΕΡΗ ΕΝΕΡΓΕΙΑ ΑΝΤΑΛΛΑΓΗΣ","ΕΝΘΑΠΙΑ ΑΝΤΑΛΛΑΓΗΣ","ΕΝΤΡΟΠΙΑ ΑΝΤΑΛΛΑΓΗΣ","ΙΣΟΘΕΡΜΟΙ ΑΝΤΑΛΛΑΓΗΣ","ΣΥΝΤΕΛΕΣΤΗΣ ΕΝΕΡΓΟΤΗΤΑΣ ΑΝΤΑΛΛΑΞΙΜΩΝ","ΥΣΤΕΡΗΣΗ ΑΝΤΑΛΛΑΓΗΣ","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/1292","http://hdl.handle.net/10442/hedi/1292"]}]},{"id":"additional","label":"Additional Metadata","entries":[{"key":"dc:description","label":"Description","values":["THE EXCHANGE CHARACTERISTICS OF THE PAIR POTASSIUM-MAGNESIUM WAS STUDIED IN THREE REPRESENTATIVE RED MEDITERRANEAN SOILS USING THERMODYNAMIC PRINCIPLES. THE EXCHANGE REACTION WAS STUDIED IN BOTH DIRECTIONS IN AN ATTEMPT TO INVESTIGATE ITS REVERSIBILITY AND TO RELATE IT WITH THE MINERALOGICAL COMPOSITION OF THE SOILS. COMPARISON OF THE EXPERIMENTAL ISOTHERMS TO THE NON-PREFERENCE ISOTHERMS REVEALED THAT ALL THREE SOILS EXHIBITED HIGH PREFERENCE FOR POTASSIUM RELATIVE TO MAGNESIUM IONS. THE VALUES OF THE THERMODYNAMIC PARAMETERS KEQ, ΔGO, ΔΗO, ΔSO FOR THE K_MG EXCHANGE, CALCULATED FROM THE EXPERIMENTAL EXCHANGE ISOTHERMS, CONFIRMED THE SOILS' PREFERENCE FOR POTASSIUM. THESE VALUES WERE INFLUENCED MAINLY BY THE TYPE OF CLAY MINERALS PREVAILING IN THE CLAY FRACTION OF THE SOILS STUDIED. THE EXCHANGE REACTION OF THE PAIR K-MG WAS NOT COMPLETELY REVERSIBLE BUT EXHIBITED HYSTERESIS, THE MAGNITUDE OF WHICH WAS MORE PRONOUNCED IN THOSE SOILS WHERE MICA-TYPE MINERALS DOMINATED THE CLAY FRACTION. HYSTERESIS EFFECTS WERE ATTRIBUTED TO THE COMBINED ACTION OF CLAY FLOCCULATION DURING THE EXCHANGE EXPERIMENTS AND TO CHANGES OCCURRING IN THE MICA-TYPE MINERALS UPON POTASSIUM DEPLETION.","Η ΑΝΤΑΛΛΑΓΗ ΤΩΝ ΚΑΤΙΟΝΤΩΝ ΚΑΛΙΟΥ ΚΑΙ ΜΑΓΝΗΣΙΟΥ ΜΕΛΕΤΗΘΗΚΕ ΣΕ ΤΡΙΑ ΑΝΤΙΠΡΟΣΩΠΕΥΤΙΚΑ ΕΡΥΘΡΑ ΜΕΣΟΓΕΙΑΚΑ ΕΔΑΦΗ ΜΕ ΤΗΝ ΕΦΑΡΜΟΓΗ ΤΩΝ ΑΡΧΩΝ ΤΗΣ ΘΕΡΜΟΔΥΝΑΜΙΚΗΣ. Η ΑΝΤΑΛΛΑΓΗ ΜΕΛΕΤΗΘΗΚΕ ΑΜΦΙΔΡΟΜΑ ΣΕ ΜΙΑ ΠΡΟΣΠΑΘΕΙΑ ΕΛΕΓΧΟΥ ΤΗΣ ΑΝΤΙΣΤΡΕΨΙΜΟΤΗΤΑΣ ΤΗΣΚΑΙ ΣΥΣΧΕΤΙΣΜΟΥ ΤΗΣ ΜΕ ΤΗΝ ΟΡΥΚΤΟΛΟΓΙΚΗ ΣΥΣΤΑΣΗ ΤΩΝ ΕΔΑΦΩΝ. KΑΤΑΣΚΕΥΑΣΘΗΚΑΝ ΟΙΙΣΟΘΕΡΜΟΙ ΑΝΤΑΛΛΑΓΗΣ ΚΑΙ ΣΥΓΚΡΙΝΟΜΕΝΕΣ ΠΡΟΣ ΤΙΣ ΙΣΟΘΕΡΜΟΥΣ ΜΗ ΕΚΛΕΚΤΙΚΗΣ ΠΡΟΣΡΟΦΗΣΗΣ ΥΠΟΔΗΛΩΣΑΝ ΠΡΟΤΙΜΗΣΗ ΚΑΙ ΤΩΝ ΤΡΙΩΝ ΕΔΑΦΩΝ ΓΙΑ ΤΟ ΚΑΛΙΟ ΣΕ ΣΧΕΣΗ ΜΕ ΤΟ ΜΑΓΝΗΣΙΟ. ΑΠΟ ΤΙΣ ΙΣΟΘΕΡΜΟΥΣ ΥΠΟΛΟΓΙΣΤΗΚΑΝ ΤΑ ΘΕΡΜΟΔΥΝΑΜΙΚΑ ΜΕΓΕΘΗ KEQ, ΔGO, ΔΗΟ,ΔSO ΑΠΟ ΤΙΣ ΤΙΜΕΣ ΤΩΝ ΟΠΟΙΩΝ ΕΠΙΒΕΒΑΙΩΘΗΚΕ Η ΠΡΟΤΙΜΗΣΗ ΤΩΝ ΕΔΑΦΩΝ ΓΙΑ ΤΟ ΚΑΛΙΟΠΟΥ ΥΠΟΔΗΛΩΘΗΚΕ ΑΠΟ ΤΙΣ ΙΣΟΘΕΡΜΟΥΣ ΚΑΙ ΚΑΘΟΡΙΣΤΗΚΕ ΤΟ ΜΕΓΕΘΟΣ ΤΗΣ. ΟΙ ΤΙΜΕΣ ΤΩΝ ΠΡΟΗΓΟΥΜΕΝΩΝ ΘΕΡΜΟΔΥΝΑΜΙΚΩΝ ΜΕΓΕΘΩΝ ΔΙΑΜΟΡΦΩΘΗΚΑΝ ΚΑΤΑ ΚΥΡΙΟ ΛΟΓΟ ΑΠΟ ΤΗΝ ΕΠΙΔΡΑΣΗ ΤΗΣ ΟΡΥΚΤΟΛΟΓΙΚΗΣ ΣΥΣΤΑΣΗΣ ΤΩΝ ΑΡΓΙΛΛΩΝ ΤΩΝ ΕΔΑΦΩΝ Η ΟΠΟΙΑ ΚΑΘΟΡΙΣΕ ΚΑΙ ΤΟ ΜΕΓΕΘΟΣ ΤΗΣ ΕΚΛΕΚΤΙΚΟΤΗΤΑΣ ΤΟΥΣ. ΟΙ ΑΝΤΙΔΡΑΣΕΙΣ ΑΝΤΑΛΛΑΓΗΣ ΒΡΕΘΗΚΕ ΟΤΙ ΔΕΝ ΗΤΑΝ ΠΛΗΡΩΣ ΑΝΤΙΣΤΡΕΠΤΕΣ, ΠΡΑΓΜΑ ΠΟΥ ΑΠΟΤΕΛΕΙ ΑΠΑΡΑΙΤΗΤΗ ΠΡΟΥΠΟΘΕΣΗ ΤΗΣ ΘΕΡΜΟΔΥΝΑΜΙΚΗΣ ΜΕΤΑΧΕΙΡΙΣΗΣ ΤΟΥΣ, ΑΛΛΑ ΕΚΔΗΛΩΝΑΝ ΥΣΤΕΡΗΣΗ ΤΟ ΜΕΓΕΘΟΣ ΤΗΣ ΟΠΟΙΑΣ ΚΥΜΑΝΘΗΚΕ ΚΥΡΙΩΣ ΑΝΑΛΟΓΑ ΜΕ ΤΗΝ ΠΕΡΙΕΚΤΙΚΟΤΗΤΑ ΤΩΝ ΕΔΑΦΩΝ ΣΕ ΜΑΡΜΑΡΥΓΙΕΣ. Η ΘΕΡΜΟΔΥΝΑΜΙΚΗ ΜΕΤΑΧΕΙΡΙΣΗ ΤΩΝ ΣΥΣΤΗΜΑΤΩΝ ΚΡΙΘΗΚΕ ΕΓΚΥΡΗ ΠΑΡΑ ΤΗΝ ΕΚΔΗΛΩΣΗ ΤΗΣ ΥΣΤΕΡΗΣΗΣ ΔΕΔΟΜΕΝΟΥ ΟΤΙ Η ΕΜΦΑΝΙΣΗ ΤΗΣ ΑΠΟΔΟΘΗΚΕ ΣΕ ΦΥΣΙΚΑ ΑΙΤΙΑ."]},{"key":"dc:title","label":"Title","values":["ΙΣΟΡΡΟΠΙΑ ΑΝΤΑΛΛΑΞΙΜΩΝ-ΔΙΑΛΥΤΩΝ ΜΟΡΦΩΝ ΚΑΛΙΟΥ-ΜΑΓΝΗΣΙΟΥ ΣΤΑ ΕΔΑΦΗ","EXCHANGEABLE-SOLUBLE POTASSIUM-MAGNESIUM EQUILLIBRIUM IN SOILS"]}]}],"canonical_facts":{"dc:creator":["Σινάνης, Κωνσταντίνος"],"dc:date":["1990"],"dc:description":["THE EXCHANGE CHARACTERISTICS OF THE PAIR POTASSIUM-MAGNESIUM WAS STUDIED IN THREE REPRESENTATIVE RED MEDITERRANEAN SOILS USING THERMODYNAMIC PRINCIPLES. THE EXCHANGE REACTION WAS STUDIED IN BOTH DIRECTIONS IN AN ATTEMPT TO INVESTIGATE ITS REVERSIBILITY AND TO RELATE IT WITH THE MINERALOGICAL COMPOSITION OF THE SOILS. COMPARISON OF THE EXPERIMENTAL ISOTHERMS TO THE NON-PREFERENCE ISOTHERMS REVEALED THAT ALL THREE SOILS EXHIBITED HIGH PREFERENCE FOR POTASSIUM RELATIVE TO MAGNESIUM IONS. THE VALUES OF THE THERMODYNAMIC PARAMETERS KEQ, ΔGO, ΔΗO, ΔSO FOR THE K_MG EXCHANGE, CALCULATED FROM THE EXPERIMENTAL EXCHANGE ISOTHERMS, CONFIRMED THE SOILS' PREFERENCE FOR POTASSIUM. THESE VALUES WERE INFLUENCED MAINLY BY THE TYPE OF CLAY MINERALS PREVAILING IN THE CLAY FRACTION OF THE SOILS STUDIED. THE EXCHANGE REACTION OF THE PAIR K-MG WAS NOT COMPLETELY REVERSIBLE BUT EXHIBITED HYSTERESIS, THE MAGNITUDE OF WHICH WAS MORE PRONOUNCED IN THOSE SOILS WHERE MICA-TYPE MINERALS DOMINATED THE CLAY FRACTION. HYSTERESIS EFFECTS WERE ATTRIBUTED TO THE COMBINED ACTION OF CLAY FLOCCULATION DURING THE EXCHANGE EXPERIMENTS AND TO CHANGES OCCURRING IN THE MICA-TYPE MINERALS UPON POTASSIUM DEPLETION.","Η ΑΝΤΑΛΛΑΓΗ ΤΩΝ ΚΑΤΙΟΝΤΩΝ ΚΑΛΙΟΥ ΚΑΙ ΜΑΓΝΗΣΙΟΥ ΜΕΛΕΤΗΘΗΚΕ ΣΕ ΤΡΙΑ ΑΝΤΙΠΡΟΣΩΠΕΥΤΙΚΑ ΕΡΥΘΡΑ ΜΕΣΟΓΕΙΑΚΑ ΕΔΑΦΗ ΜΕ ΤΗΝ ΕΦΑΡΜΟΓΗ ΤΩΝ ΑΡΧΩΝ ΤΗΣ ΘΕΡΜΟΔΥΝΑΜΙΚΗΣ. Η ΑΝΤΑΛΛΑΓΗ ΜΕΛΕΤΗΘΗΚΕ ΑΜΦΙΔΡΟΜΑ ΣΕ ΜΙΑ ΠΡΟΣΠΑΘΕΙΑ ΕΛΕΓΧΟΥ ΤΗΣ ΑΝΤΙΣΤΡΕΨΙΜΟΤΗΤΑΣ ΤΗΣΚΑΙ ΣΥΣΧΕΤΙΣΜΟΥ ΤΗΣ ΜΕ ΤΗΝ ΟΡΥΚΤΟΛΟΓΙΚΗ ΣΥΣΤΑΣΗ ΤΩΝ ΕΔΑΦΩΝ. KΑΤΑΣΚΕΥΑΣΘΗΚΑΝ ΟΙΙΣΟΘΕΡΜΟΙ ΑΝΤΑΛΛΑΓΗΣ ΚΑΙ ΣΥΓΚΡΙΝΟΜΕΝΕΣ ΠΡΟΣ ΤΙΣ ΙΣΟΘΕΡΜΟΥΣ ΜΗ ΕΚΛΕΚΤΙΚΗΣ ΠΡΟΣΡΟΦΗΣΗΣ ΥΠΟΔΗΛΩΣΑΝ ΠΡΟΤΙΜΗΣΗ ΚΑΙ ΤΩΝ ΤΡΙΩΝ ΕΔΑΦΩΝ ΓΙΑ ΤΟ ΚΑΛΙΟ ΣΕ ΣΧΕΣΗ ΜΕ ΤΟ ΜΑΓΝΗΣΙΟ. ΑΠΟ ΤΙΣ ΙΣΟΘΕΡΜΟΥΣ ΥΠΟΛΟΓΙΣΤΗΚΑΝ ΤΑ ΘΕΡΜΟΔΥΝΑΜΙΚΑ ΜΕΓΕΘΗ KEQ, ΔGO, ΔΗΟ,ΔSO ΑΠΟ ΤΙΣ ΤΙΜΕΣ ΤΩΝ ΟΠΟΙΩΝ ΕΠΙΒΕΒΑΙΩΘΗΚΕ Η ΠΡΟΤΙΜΗΣΗ ΤΩΝ ΕΔΑΦΩΝ ΓΙΑ ΤΟ ΚΑΛΙΟΠΟΥ ΥΠΟΔΗΛΩΘΗΚΕ ΑΠΟ ΤΙΣ ΙΣΟΘΕΡΜΟΥΣ ΚΑΙ ΚΑΘΟΡΙΣΤΗΚΕ ΤΟ ΜΕΓΕΘΟΣ ΤΗΣ. ΟΙ ΤΙΜΕΣ ΤΩΝ ΠΡΟΗΓΟΥΜΕΝΩΝ ΘΕΡΜΟΔΥΝΑΜΙΚΩΝ ΜΕΓΕΘΩΝ ΔΙΑΜΟΡΦΩΘΗΚΑΝ ΚΑΤΑ ΚΥΡΙΟ ΛΟΓΟ ΑΠΟ ΤΗΝ ΕΠΙΔΡΑΣΗ ΤΗΣ ΟΡΥΚΤΟΛΟΓΙΚΗΣ ΣΥΣΤΑΣΗΣ ΤΩΝ ΑΡΓΙΛΛΩΝ ΤΩΝ ΕΔΑΦΩΝ Η ΟΠΟΙΑ ΚΑΘΟΡΙΣΕ ΚΑΙ ΤΟ ΜΕΓΕΘΟΣ ΤΗΣ ΕΚΛΕΚΤΙΚΟΤΗΤΑΣ ΤΟΥΣ. ΟΙ ΑΝΤΙΔΡΑΣΕΙΣ ΑΝΤΑΛΛΑΓΗΣ ΒΡΕΘΗΚΕ ΟΤΙ ΔΕΝ ΗΤΑΝ ΠΛΗΡΩΣ ΑΝΤΙΣΤΡΕΠΤΕΣ, ΠΡΑΓΜΑ ΠΟΥ ΑΠΟΤΕΛΕΙ ΑΠΑΡΑΙΤΗΤΗ ΠΡΟΥΠΟΘΕΣΗ ΤΗΣ ΘΕΡΜΟΔΥΝΑΜΙΚΗΣ ΜΕΤΑΧΕΙΡΙΣΗΣ ΤΟΥΣ, ΑΛΛΑ ΕΚΔΗΛΩΝΑΝ ΥΣΤΕΡΗΣΗ ΤΟ ΜΕΓΕΘΟΣ ΤΗΣ ΟΠΟΙΑΣ ΚΥΜΑΝΘΗΚΕ ΚΥΡΙΩΣ ΑΝΑΛΟΓΑ ΜΕ ΤΗΝ ΠΕΡΙΕΚΤΙΚΟΤΗΤΑ ΤΩΝ ΕΔΑΦΩΝ ΣΕ ΜΑΡΜΑΡΥΓΙΕΣ. Η ΘΕΡΜΟΔΥΝΑΜΙΚΗ ΜΕΤΑΧΕΙΡΙΣΗ ΤΩΝ ΣΥΣΤΗΜΑΤΩΝ ΚΡΙΘΗΚΕ ΕΓΚΥΡΗ ΠΑΡΑ ΤΗΝ ΕΚΔΗΛΩΣΗ ΤΗΣ ΥΣΤΕΡΗΣΗΣ ΔΕΔΟΜΕΝΟΥ ΟΤΙ Η ΕΜΦΑΝΙΣΗ ΤΗΣ ΑΠΟΔΟΘΗΚΕ ΣΕ ΦΥΣΙΚΑ ΑΙΤΙΑ."],"dc:identifier":["10.12681/eadd/1292","http://hdl.handle.net/10442/hedi/1292"],"dc:language":["gre"],"dc:publisher":["Αριστοτέλειο Πανεπιστήμιο Θεσσαλονίκης (ΑΠΘ)","Aristotle University Of Thessaloniki (AUTH)"],"dc:subject":["ACTIVITY COEFFICIENT OF EXCHANGEABLE IONS","ENTHALPYOF EXCHANGE","ENTROPY OF EXCHANGE","EXCHANGEABLE K","EXCHANGEABLE MG","FREE ENERGY OF EXCHANGE","HYSTERESIS OF EXCHANGE","ION EXCHANGE ISOTHERMS","ΑΝΤΑΛΛΑΞΙΜΟ MG","ΑΝΤΑΛΛΑΞΙΜΟ Κ","ΕΛΕΥΘΕΡΗ ΕΝΕΡΓΕΙΑ ΑΝΤΑΛΛΑΓΗΣ","ΕΝΘΑΠΙΑ ΑΝΤΑΛΛΑΓΗΣ","ΕΝΤΡΟΠΙΑ ΑΝΤΑΛΛΑΓΗΣ","ΙΣΟΘΕΡΜΟΙ ΑΝΤΑΛΛΑΓΗΣ","ΣΥΝΤΕΛΕΣΤΗΣ ΕΝΕΡΓΟΤΗΤΑΣ ΑΝΤΑΛΛΑΞΙΜΩΝ","ΥΣΤΕΡΗΣΗ ΑΝΤΑΛΛΑΓΗΣ","Γεωπονικές Επιστήμες και Κτηνιατρική","Agricultural and Veterinary Sciences","Γεωπονία, Δασολογία και Αλιεία","Agriculture, Forestry and Fisheries"],"dc:title":["ΙΣΟΡΡΟΠΙΑ ΑΝΤΑΛΛΑΞΙΜΩΝ-ΔΙΑΛΥΤΩΝ ΜΟΡΦΩΝ ΚΑΛΙΟΥ-ΜΑΓΝΗΣΙΟΥ ΣΤΑ ΕΔΑΦΗ","EXCHANGEABLE-SOLUBLE POTASSIUM-MAGNESIUM EQUILLIBRIUM IN SOILS"],"dc:type":["PhD Thesis"]},"updated_at":"2026-07-24T02:24:49Z"}