In classic thermodynamics, deterioration (S) and hotness (T) are two befriended thermodynamic variables whose spatial equatings are unknown but whose fruit (TS) is, like heat (Q), an strength (ML2T-2). This poses an ultimate obstacle inform of an "thermodynamic 2nd society" when individual wants to expand the soil and water thermodynamic interplay and allow for possibility the hierarchically organized construction in aggregates of the dimensional stage. This question has currently developed accompanying what has existed named “intrinsic soil water thermodynamics” where all thermodynamic variables had expected “integral” to fit into the “tangible and intrinsic forming” example of Hydrostructural Pedology. With their spatial similarity, all the thermodynamic variables, being intrinsic, perform at the various organizational levels of a soil skyline, containing those, microscopic and tiny, of the fluid chapters of the pedostructure. With this new viewpoint, the Carnot phase definitely ratifies the agreement between the established thermodynamic wording and the integral variables and equatings of the new thermodynamics model. However, a entirely various understanding of the Carnot phase and the Clausius prejudice is emphasize here, individual that has nothing commotion accompanying the question of reversibility/irreversibility but moderately accompanying the fundamental tangible process at the footing of the thermodynamic balance and allure developing with opportunity. The Clausius prejudice is elucidated and new fields of research are arising in view.
Author(s) Details:
E. Braudeau,
VALORHIZ,
R&D Department. 1900, Boulevard de la Lironde, PSIII, Parc Scientifique
Agropolis F34980 Montferrier sur Lez., France.
Please see the link here: https://stm.bookpi.org/NPGEES-V3/article/view/9372
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