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  • 1
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    Springer
    Pure and applied geophysics 8 (1946), S. 94-103 
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Description / Table of Contents: Summary The conditions are given to a climatic cycle in order to have a physically reality. To 30 long series of annual values of climatic elements has been applied the periodal analysis after the method of Vercelli. In all the cases results with strong evidence a remarkable oscillation of 5,6 years. Attention is drawn to the physically reality of that cycle. It has an amplitude often greater that all other component-waves; the period remains almost constant, the phase change from region to region.
    Abstract: Zusammenfassung Es werden die Bedingungen, damit ein klimatischer Cyklus als eine physische Realität betrachtet werden kann, angegeben. Man untersucht die periodalen Analysen von längeren Reihen klimatischer Elemente und es wird die Existenz, die bemerkenswerte Amplitude und die physische Realität des 5,6 jährigen Cyklus angedeutet. Derselbe ist immer vorhanden, in allen geophysischen Faktoren und in allen Erdteilen. Der Cycklus hat eine grosse Amplitude, ofter mehr als jeder andere. Behält constant seine Periode. Die Phase wechselt je nach der Zone. Er stellt im allgemeinen eigenartige Dämpfungen vor.
    Notes: Riassunto Date le condizioni perchè un ciclo climatico possa considerarsi una realtà fisica ed esaminate le analisi periodali di lunghe serie di elementi climatici si mette in evidenza l'esistenza, la notevole ampiezza e la realtà fisica del ciclo di 5,6 anni. Esso si presenta sempre, in tutti i fattori geofisici e in tutte le regioni della terra. E' molto ampio, spesso più di ogni altro. Mantiene costante il periodo; la fase varia con la regione. Presenta particolari smorzamenti di carattere universale.
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  • 2
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    Pure and applied geophysics 8 (1946), S. 104-117 
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
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  • 3
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    Pure and applied geophysics 8 (1946), S. 160-166 
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Description / Table of Contents: Summary After the characteristics of the seismic instruments, is given the statistics of the activity of the Seismographics Observatory at Prato (Italy) from January 1, 1931, to December 31, 1945.
    Notes: Riassunto Premesse le caratteristiche degli strumenti, viene esposta una statistica dell'attività dell'Osservatorio dal suo inizio, al 1 gennaio 1931, a tutto il 31 dicembre 1945.
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  • 4
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    Pure and applied geophysics 8 (1946), S. 191-196 
    ISSN: 1420-9136
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  • 5
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    Pure and applied geophysics 9 (1946), S. 30-36 
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Description / Table of Contents: Summary From tidal records is examined the variation of the mean sealevel observed in the last 70 years in the ports of Venice, Trieste and Pola. The variation is attributed to the glacial eustatic. The mean sea-level increase for every ten years of 3,8 cm for Venice, 1,7 cm for Trieste and 1,6 cm for Pola. The remarkable value for Venice is caused from a contemporary abatement of the coast.
    Abstract: Zusammenfassung Man prüft auf Grund mareographischer Angaben Veränderungen des mittleren Wasserstandes, welche, in den letzten 70 Jahren in den Häfen von Venedig, Triest und Pola beobachtet wurden. Die Bewegung wird der glazialen Eustatik zugeschrieben. Es ergibt sich, dass das Meeresniveau in Venedig um 3,8 cm., in Triest 1,7 cm. und in Pola 1,6 cm. für Jahrzehnt steigt. Die mittlere Erhöhung der drei Häfen beträgt 2,4 cm. für Jahrzehnt. Der ansehnliche Wert von Venedig wird einer gleichzeitigen Senkung der Küstenzone zugeeignet.
    Notes: Riassunto Si esamina, sul fondamento di dati mareografici, la variazione del medio livello marino avvenuta negli ultimi 70 anni nei porti di Venezia, Trieste e Pola. Il movimento si attribuisce all'eustatismo glaciale. Risulta che il livello del mare aumenta di 3,8 cm. per decennio a Venezia, di 1,7 a Trieste e di 1,6 a Pola. L'aumento medio per i tre porti è di 2,4 cm. per decennio. Il notevole valore di Venezia è dovuto ad un contemporaneo abbassamento della zona costiera.
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  • 6
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    Pure and applied geophysics 9 (1946), S. 106-113 
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
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  • 7
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    Pure and applied geophysics 9 (1946), S. 81-94 
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Description / Table of Contents: Summary The caracteristics of the landslide of C. le Rive (Comune di Fumane, Verona), the topographical, geological and hydrographical (at the surface and underground) conditions of the region, the meteorological circumstances come before are examined, and all the necessary works are advised in order to prevent its repeating and enlarging. It is tried to put the phenomenon in the most important italian classifications. It corresponds to theSharpe's slump, that we may translate, with a strict meaning, «smottamento».
    Notes: Riassunto Vengono esaminate le caratteristiche della frana di C. le Rive in Comune di Fumane (Verona), lc condizioni topografiche, geologiche, idrografiche (superficiali e sotterranee) della zona, le circostanze meteorologiche che l'hanno preceduta, e vengono indicati i lavori possibili e necessari per evitare che essa si ripeta e si estenda. Si cerca poi di collocare la frana nelle più importanti classificazioni italiane. Essa corrisponde aglislumps delSharpe, che possiamo tradurre, con preeisazione di significato, come «smottamenti».
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  • 8
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    Pure and applied geophysics 9 (1946), S. 113-114 
    ISSN: 1420-9136
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  • 9
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    Pure and applied geophysics 9 (1946), S. 122-136 
    ISSN: 1420-9136
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  • 10
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    Pure and applied geophysics 8 (1946), S. 133-144 
    ISSN: 1420-9136
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  • 11
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    Pure and applied geophysics 8 (1946), S. 145-159 
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Description / Table of Contents: Summary After some hints on the new volcanoes of Greece and volcanic afflorescences of the Egeus sea and eastern Greece, the Author, after the micro and macroseismical data of some earthquakes occurred during the years 1928–1945, asserts that they belong in the category of magmatical earthquakes. From the study of conditions and disposition of the epicenters, he deduces a relation among the seismical and volcanic activities, and infers that the studied phenomena are the proof of the duration of magmatical actions in the interior of the examined countries.
    Notes: Riassunto Premessi brevi cenni sui vulcani nuovi della Grecia e sugli affioramenti vulcanici del mar Egeo e della Grecia orientale, l'Autore, in base ai dati micro e macrosismici di alcuni terremoti avvenuti durante gli anni 1928–1945, afferma trattarsi di sismi magmatici. Dallo studio delle distribuzioni degli epicentri e delle condizioni sotto le quali ebbero luogo detti sismi, si deduce una relazione fra l'attività sismica e quella vulcanica, concludendo che i fenomeni studiati sonc una prova della continuazione delle azioni magmatiche verificantisi nell'interno delle regioni esaminate.
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  • 12
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    Pure and applied geophysics 8 (1946), S. 167-179 
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Description / Table of Contents: Summary By applying the periodal analysis to the rainfall gathered in Florence from the year 1913 to 1918, the component waves of the years 35; 30; 28–14; 16; 11; 8; 5,3; 4; 3; 2 have been found. A comparison between these components and those corresponding of Trieste, Padua and Mantua has been ascertained. ThroughSchuster's Criterion, modified byStumpff, the waves of a period inferior to 14 years and superior to 35 years have proved evident.
    Abstract: Zummenfassung Bei Anwendung der Periodogrammanalyse an die in den Jahren 1813 bis 1918 in Florenz aufgesammelten atmosphärischen Niederschläge, sind Wellen aus den folgenden Jahren bestehend: 35; 30; 28–14; 16; 11; 8; 5,3; 4; 3; 2 gefunden worden. Es wurde ein Verhältnis zwischen diesen Beständen und den entsprechenden von Triest, Padua und Mantova festgestellt. Auf Grund desSchuster-ischen und vonK. Stumpff berichtigten Kriteriums, wurden die Wellenperioden von unter 14 Jahren und von über 35 Jahren als reellen befunden.
    Notes: Riassunto Applicando l'analisi periodale alle precipitazioni atmosferiche raccolte a Firenze dal 1813 al 1918 si sono trovate onde componenti di anni 35; 30; 28–14; 16; 11; 8; 5,3; 4; 3; 2. Si è stabilito un confronto tra queste componenti e quelle corrispondenti di Trieste, Padova e Mantova. Per mezzo del criterio diSchuster, modificato daStumpff, si sono riscontrate reali le onde di periodo inferiore a 14 anni e superiore a 35 anni.
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  • 13
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    Pure and applied geophysics 9 (1946), S. 1-18 
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Description / Table of Contents: Summary Principally, on the base of the numerous measures of gravity established after 1930, and of the new compensated values for the reference stations, and with suitable hypothesis to reduce to a minimum the causes of error, which are examined and discussed, it is calculated the value ofg e in the two hypothesis ofBouguer and isostatical (h c =−113,7 km). The result is 978,043 in Potsdam System.
    Abstract: Zusammenfassung Auf Grund vor allem der zahlreichen nach 1930 ausgeführten Schweremessungen, der neuen kompensierten Werte fur die Hauptstationen, und durch geeignete Hypothesen um die Fehlerursachen, welche geprüft und erötert werden, zu reduzieren, wird esg e in den beiden Hypothesen vonBouguer und der Isostasie (h c =−113,7 km) berechnet. Das Resultat ist 978,043 im Potsdamer System.
    Notes: Riassunto Sulla base soprattutto delle numerose misure di gravità successive al 1930, dei nuovi valori compensati per le stazioni di riferimento e con opportune ipotesi per ridurre al minimo le cause di errore, che vengono esaminate e discusse, si procede al calcolo dig e nelle due ipotesi diBouguer ed isostatica (hc=−113,7 km). Il risultato è 978,043 nel sistema di Potsdam.
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  • 14
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    Pure and applied geophysics 8 (1946), S. 73-80 
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  • 15
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    Pure and applied geophysics 8 (1946), S. 129-132 
    ISSN: 1420-9136
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  • 16
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    Pure and applied geophysics 8 (1946), S. 180-191 
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  • 17
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    Pure and applied geophysics 8 (1946), S. 1-42 
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Description / Table of Contents: Summary The frequency of the earthquakes in Albania is a sign of the general instability of this territory. The progress of the geological knowledge in Albania gives to make a tectonic synthesis; the results are compared with the seismic characters. The seismology of the region is essentially bonded to the tectonics; in the South-Albania by consequence specially of tectonic settlements, in the North by tangential movements, while probably in the costal plain are continuous movements of emersion. In appendix are given list of earthquales and description of the geological situation of the towns and greatest villages, also in account of the buildings.
    Abstract: Zusammenfassung Die Erdbebentätigkeit in Albanien stellt ein scharfe Zeichen der allgemeinen Unbeständigkeit dieser Teil des Adria-Beckens dar. Da die Fortschritte unserer geologischen Kentnisse eine tektonische Synthese erlauben, werden die betreffenden Ergebnisse mit den seismischen Eigentümlichkeiten verglichen. Aus der Erörterung folgt wie die Seismizität der Gegend von den tektonischen Verhätnisse abhängt, nämlich in der Weise, dass in Süd-Albanien als eine Folge der Setzungsbewegungen zu betrachten ist, während in Nord-Albanien mit den Tangential-Bewegungen verknüpft sein soll. An der Küste verschiedene Anzeige lassen stetige Hebungsbewegungen vermuten. Am Schluss folgt ein Verzeichnis der wichtigsten Erdbeben, sowie Angabe über die geologische Lage der Städte und grossen Dörfer im Verhältnis mit der konstruktiven Eigentümlichkeiten der Gebäude.
    Notes: Riassunto La frequenza dei terremoti in Albania à altamente significativa di una generale instabilità di quella parte del territorio adriatico. Permettendo ora i progressi della conoscenza geologica del territorio albanese di tentare una sintesi tettonica, i risultati di questa vengono messi a confronto con i caratteri sismici della regione. Dalla discussione di tutti gli elementi attualmente noti si espone come la sismicità della regione, dipendendo in linea generale dalle condizioni tettoniche, si manifesta nelle regioni meridionali come conseguenza specialmente di movimenti di assestamento, mentre nelle settentrionali para ancora in collegamento con i moti tangenziali; nella regione costiera diversi indizi farebbero ritenere probabile dei continuati moti di emersione. Seguono un elenco dei principali terremoti avvenuti nella regione ed alcuni dati sulla posizione geologica dei centri abitati e sulle caratteristiche costruttive degli edifici.
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  • 18
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    Pure and applied geophysics 8 (1946), S. 81-93 
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Description / Table of Contents: Summary It is shown that the «conventional» base-value of gravity at Potsdam (981, 274), considered until few years ago as one of the more precisious results, is instead affected very probably by a big error. This is demonstred first by the new absolute measure at Washington, and seems to be confirmed by the absolute measure at Leningrad too, for which definitive results are not yet known. — A new «international» reference system is therefore proposed, based no more on only one absolute measure of gravity, but on the most important ones until now executed. The relative differences between them result from a new compensation of the international net of the reference-stations excuted from the Author. — We shall be very thankfull to all those Geodesists who will kindly begun the discussion on this problem for its definitive solution.
    Abstract: Resumé Ce travail a le but d'exposer le plus clairement possible le problème du système de référence pour les mesures de gravité rélative et de montrer que la valeur fondamentale «conventionnelle» de Potsdam (981,274), considerée il y a quelques années comme un des résultats de la plus grande précision, se présent au contraire frappée très probablement d'une faute considérable. Tout cela est démontré surtout par la nouvelle mesure absolue faite à Washington et il semble être confirmé même par la mesure absolue de Leningrad, dont nous ne connaissons pas encore les résultats définitifs. — C'est pour cela que nous proposons l'adoption d'un nouveau système de référence international, qui soit fondé non plus sur le résultat d'une seule mesure absolue de la gravité, mais sur les plus importantes effectuées jusqu'ici. Les différences rélatives entr'elles resultent d'une nouvelle compensation du reseau international des stations de référence executée par l'Auteur. — Nous serons bien grès à tous ces Géodésiens qui voudront bien commencer la discussion sur ce problème, pur sa résolution définitive.
    Notes: Riassunto Il presente lavoro si prefigge lo scopo di esporre il problema del sistema di riferimento per le misure di gravità relativa e di mostrare che il valore base «convenzionale» di Potsdam (981.274), considerato fino a pochi anni addietro come uno dei risultati di maggiore precisione, si presenta invece affetto molto probabilmente da un notevole errore. Ciò viene dimostrato principalmente dalla nuova misura assoluta al Nat. Bureau of Standards di Washington, e sembra essere confermato anche dalla misura assoluta di Leaingrado, di cui non ci sono ancora noti i risultati definitive. — Si propone perciò l'adozione di un nuovo sistema di riferimento «internazionale», basato cioè non più sul risultato di una sola misura assoluta della gravità, ma sulle più importanti finora eseguite. Le differenze relative fra di esse risultano da una nuova compensazione della rete internazionale delle stazioni di riferimento eseguita dall'A. — Saremo molto grati a tutti quei Geodeti che vorranno cortesemente iniziare la discussione su questo problema.
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  • 19
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    Pure and applied geophysics 9 (1946), S. 19-29 
    ISSN: 1420-9136
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Description / Table of Contents: Summary The above mentioned earthquake was already investigated byP. Caloi only by seismographic data obtaining a depth of 18 Km., while others shocks in the same zone, investigated with similar methods, should have been originated in depths of 37–51 Km. Therefore, the A. has undertake a new determination using a macroseismic method and became a value of only 4–5 Km. The discrepance is particularly great on account of the value of 43 Km. obtained bySchmerwitz also with microseismic methods. The unreliability of similar results for the solution of some important seismologic problem is analised.
    Notes: Riassunto È un terremoto già studiato su dati sismografici daP. Caloi che ha ottenuto una profondità ipocentrale di 18 Km. in disaccordo con i 37–51 calcolati con analoghi metodi per altri terremoti precedenti pure del Veneto. L'A. ha rideterminato la profondità ip. per il terremoto in questione con procedimento macrosismico, deducendo soltanto 4–5 Km. D'altra parte riesaminando i metodi delCaloi si è convinto che i suoi 18 Km. sono quanto mai incerti ed anche in forte contrasto col valore ottenuto pure microsismograficamente dalloSchmerwitz di 43 Km. Al riguardo l'A. ricorda e discute altre notevoli contraddizioni che intervengono in importanti questioni sismologiche.
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  • 20
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    Pure and applied geophysics 9 (1946), S. 73-74 
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    Pure and applied geophysics 8 (1946), S. 43-72 
    ISSN: 1420-9136
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    Description / Table of Contents: Summary The methods for estimate the depth of a earthquake are examined again by the Author, who come to the conclusion that some results of calculation are unreliable. This is explain for the earthquake of 8th June 1934 (Veneto), already examined by P. Caloi, who found a depth of 37 km, by means of elements deduced from seismological diagrams only. Instead, the A., using the method grounded on the decreasing of the intensity with the distance, has obtained 10 km. The analysis of this great discrepance show that some methods, as that of the angle of emergency, should be applied with prudence and limitation to assure reliable results.
    Abstract: Zusammenfassung Der Verf. überprüft die Ergebnisse erhalten in der Tiefe-Bestimmung eines Bebens und zeigt wie einige Schlussfolgerungen unzulässig sind. Das wird ausführlich für das Erdbeben vom 8. Juni 1934 (Venetien) gezeigt, welches P. Caloi schon untersucht hat, erhaltend eine Tiefe von 37 km und zwar allein auf Grund von mikroseismischen Elementen. Dagegen, mit Anwendung des Verfahrens der Intensität-Abnahme mit dem Abstand, hat der Verf. eine Tiefe von nur 10 km erhalten. Diese grosse Verschiedenheit wird da me stesso studiato (1): di Costantinopoli del 1894 dal franceseLacoine (4) e (5); dei Colli Laziali del 1911, 1927 e 1928 dall'Oddone (2) e (34); dell'Istria del 29-VIII-1931, del Friuli del 25-XII-1931, di Belluno del 27-XII-1933, tutti studiati dalCaloi (14), (21), (23); quello Calabro-Siculo del 1938 dal rumenoDemetrescu (6) e (7).
    Notes: Riassunto Nel riesaminare i risultati cui sono pervenuti altri studiosi nella determinazione della profondità alla quale furono originati alcuni terremoti, l'A. ha dovuto riconoscere che le conclusioni dei loro calcoli non sono attendibili. Lo stesso è avvenuto recentemente per il terremoto veneto dell'8-6-1934, pel quale il prof. P. Caloi aveva trovato 37 km, basati su dati sismografici. Adoperando invece il metodo della decrescenza dell'intensità con la distanza, l'A. ha ottenuto ca. 10 km. Tale grave disaccordo lo ha indotto a riesaminare i vari metodi adottati dal Caloi — specie quello dell'angolo di emergenza delle onde sismiche — ed è giunto alla conclusione che la profondità di 37 km, in apparenza assai lusinghiera tanto da presentare un errore medio di soli 0,4 km, è ben lontana da raggiungere tanta esattezza.
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    Pure and applied geophysics 8 (1946), S. 118-128 
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    Pure and applied geophysics 9 (1946), S. 65-73 
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    Pure and applied geophysics 9 (1946), S. 114-122 
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    Pure and applied geophysics 9 (1946), S. 37-64 
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    Description / Table of Contents: Summary The A. had researched the cause and modality of the large defilement of alkalines chromates in the ground-water-flow of the zone of Spinetta Marengo (Alessandria). By means of chemical and colourimetrical methods, he examined the characteristics of the diffusion of the defilement and present a new method to determine analytically and graphically the variation of the concentration in every point of the zone. — After, the A. examined an other defilement of sodium-arseniate in a well of Muggiano (La Spezia) in reference to the geological feature of the ground.
    Notes: Riassunto Ricercate le cause e le modalità secondo le quali si è verificato un vasto inquinamento da cromati alcalini nella falda acquifera della zona di Spinetta Marengo (Alessandria), l'A., mediante il rilevamento chimico-colorimetrico della diffusione dell'inquinamento, esaminate le caratteristiche della falda, introduce un nuovo metodo per determinare analiticamente e graficamente le variazioni della concentrazione. — A proposito di altro inquinamento da arseniato sodico verificatosi in un pozzo al Muggiano (La Spezia) vengono esaminate le caratteristiche in rapporto alla natura geologica del terreno.
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    Pure and applied geophysics 9 (1946), S. 74-80 
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    Pure and applied geophysics 9 (1946), S. 95-105 
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    Description / Table of Contents: Summary To the series of the sun-spot relative-numbers (Wolf-numbers) has been applied the periodal analysis after the method ofVercelli. From this are derived component waves of 16,0-11,15-8,32-5,68-4,05-2,9-2,0 years and others with periods longer but less precise. They have almost-periodical and almost-persistent characters. Theirs amplitudes are determinated in Wolf's units. The waves found by these means are compared with the corresponding waves of the climatical cycles.
    Abstract: Zusammenfassung An der Reihe der Relativzahlen der Sonnenflecke (Wolfer-Relativzahlen) wird dieVercelli Periodalanalyse angewendet. Es folgt die ganze Zerlegung. Man erhält Komponentwellen, die Perioden von 16,0-11,15-8,32-5,68-4,05-2,9-2,0 Jahren und andere mit längeren, aber umbestimmten Perioden, haben. Sie haben fast-periodische und fast-bestehende Kennzeichen. Es wird ihre Amplitude bestimmt. Dieselben Komponenten werden mit den entsprechenden Wellen der klimatischen Zyklen verglichen.
    Notes: Riassunto Alla successione dei numeri relativi delle macchie solari (numeri di Wolf) si applica il procedimento dell'analisi periodale delVercelli e si eseguisce la scomposizione completa del diagramma. Si ottengono onde componenti di anni 16,0-11,15-8,32-5,68-4,05-2,9-2,0 e altre di periodi più lunghi ma meno precisi. Esse hanno caratteri di quasi-periodicità e di quasipersistenza. Si determinano le loro ampiezze e si confrontano con quelle corrispondenti dei cicli climatici terrestri.
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    Synthese 〈Dordrecht〉 5 (1946), S. 61-61 
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    Synthese 〈Dordrecht〉 5 (1946), S. 56-56 
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    Synthese 〈Dordrecht〉 5 (1946), S. 108-115 
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    Synthese 〈Dordrecht〉 5 (1946), S. 156-161 
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    Synthese 〈Dordrecht〉 5 (1946), S. 117-129 
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    Synthese 〈Dordrecht〉 5 (1946), S. 183-186 
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    Cellular and molecular life sciences 2 (1946), S. 33-36 
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    Cellular and molecular life sciences 2 (1946), S. 24-24 
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    Notes: Summary Synthetic Na-propioguajacon-α-sulfonate looses its sulfo-group when treated with an excess of bromine. Ligninsulfonic acid looses only 50% of its sulphur, a brominated ligninsulfonic acid being probably formed as a by-product.
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    Cellular and molecular life sciences 2 (1946), S. 405-406 
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    Notes: Summary With the intention to clarify the mechanism of action of the antibiotic effect of some quinones the inhibition of the activity of papain by various quinones was measured. The results let it appear improbable that there is any relation between the antibacterial effect of the quinones and their inhibition power on papain. On the other hand a close parallelism was found in the strength of inhibition of the same quinones on papain, urease and catalase. The mechanism of action of the quinone inhibition of these three enzymes must be regarded as a very similar one.
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    Cellular and molecular life sciences 2 (1946), S. 404-405 
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    Notes: Zusammenfassung Euler hatte in seiner Originalabhandlung über die lateinischen Quadrate vermutet, daß kein Paar wechselseitig orthogonaler 6×6 Quadrate existiert, was einige Jahre später bewiesen wurde. Man fand dann aber, daß diese 6×6 lateinischen Quadrate einige interessante orthogonale Verteilungen in einem schwächeren als demEulerschen Sinne besitzen, die zum Teil klassifiziert und aufgezählt werden konnten. Die vorliegende Note charakterisiert die erhaltenen Resultate und gibt einige interessante Symmetrieeigenschaften dieser Verteilungen an.
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    Cellular and molecular life sciences 2 (1946), S. 493-493 
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    Notes: Summary The paper deals with a new method to determine the temperature of the solar corona. The method starts from the observational result that the elements found in the corona are distributed over a multitude of consecutive ionisation-stages and leads to the value of 630000° C. Although this method is not an exact one, the result is in good agreement with other methods, leading to a temperature of about 106 ° C.
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    Cellular and molecular life sciences 2 (1946), S. 498-500 
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    Notes: Summary The body temperature of thyroidectomized guinea pigs rises in a thermostat at 34–35° C higher and for a longer period than that of normal controls. Administration of thyroxine does not only not eliminate the observed effect of thyroidectomy, but the hight and duration of the rise of body temperature increases still further. It is concluded therefore that the observed effect is not due to thyroxine deficiency, but to lack of thermothyrine A, the antagonistic hormone of the thyroid described byMansfeld. Experiments during administration of methylthiouracil gave similar—though less marked, nevertheless significant—results and demonstrate that thiouracil inhibits not only thyroxine production but the formation of thermothyrine A as well. The fact—found byMansfeld—that in case of lack of thyroid-colloid both thermothyrines increase instead of decreasing O2 consumption and accelerate the heartbeat suggests the possibility that thermothyrine may play a role in the symptomatology of Grave's disease, and so the present experiments may have a bearing on the therapeutic action of thiouracil.
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    Cellular and molecular life sciences 2 (1946), S. 506-507 
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    Cellular and molecular life sciences 2 (1946), S. 497-498 
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    Notes: Summary The chromosomal sets of five species ofPerlodidæ (Plecoptera) are given in the present paper. The sexual chromosomes belong to three distinct types:X-O,X 1-X 2,X 1-X 2-X 3. The author shows that these three types are likely derived from the most primitive patternX-Y, by translocation and inversion.
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    Cellular and molecular life sciences 2 (1946), S. 495-497 
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    Notes: Zusammenfassung 0,5prozentige Lösungen von 2,4-dichlorophenoxyessigsaurem Natrium verhindern das Keimen vonAgrostemma Githago, Hordeum vulgare undTriticum vulgare. Das Wachstum junger Pflanzen der drei Arten wird durch Verpflanzen auf mit 0,5prozentigen Lösungen dieses Stoffes getränktem Sand gehemmt. Schwächere Lösungen gestatten das Wachstum, es ist aber verlangsamt und die Pflanzen tragen Mißbildungen verschiedener Art, die an die nach Einwirkung von Colchicin und Heteroauxin beschriebenen erinnern. Stark verdünnte Lösungen (5·10−6) beschleunigen das Wachstum und regen die Wurzelbildung an; diese Wirkung ist beiHordeum vulgare besonders deutlich.
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    Cellular and molecular life sciences 2 (1946), S. 507-509 
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    Cellular and molecular life sciences 2 (1946), S. 41-48 
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    Notes: Summary A survey of the biochemistry of regenerating animals has been made: after a critical discussion ofChild's metabolic gradients theory, the relative importance of respiration rate, carbohydrates, proteins and nucleic acids metabolism are stressed. The similarities between biochemical processes in the embryo and the regenerating organism are pointed out.
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    Cellular and molecular life sciences 2 (1946), S. 111-111 
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    Cellular and molecular life sciences 2 (1946), S. 463-465 
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    Cellular and molecular life sciences 2 (1946), S. 465-467 
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    Cellular and molecular life sciences 2 (1946), S. 492-493 
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    Notes: Summary The principal results of the present inquiries are: If a plane quantity of points “M” has a finite number of symmetrals “n”, which intersect in a point “S”, these symmetrals form a regular fascicle of straight lines, with an angleπ/n of two subsequent symmetrals. If “α” is the angle between two straight lines with the intersection point “S”, you may or may not supplement them to a regular fascicle of symmetrals of a quantity of points “M”, by adding a finite number of straight lines, according as “α” represents a rational or irrational multiple of 2π. If the angle “α” of two symmetrals of “M” with the intersection point “S” is an irrational multiple of 2π, there will be to every straight line “g” through “S” a symmetral of “M”, which comprises with “g”, a small angle of the size you may choose. If “M” is closed, then in this case every straight line “g” through “S” will be a symmetral of “M”. The symmetrals of a limited quantity of points will intersect in an exact point.
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    Cellular and molecular life sciences 2 (1946), S. 86-99 
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    Notes: Summary After a short reference to the fundamental principles of the oxidation-reduction potential and the meaning of the symbolr H introduced byClark, the author proceeds to set out, among the numerous applications which this important notion has found in various scientific fields, those found in Bacteriology and Hygiene. As regards Bacteriology, the oxidation-reduction potential of the sterile culture media and of various aerobic and anaerobic micro-organisms has been investigated in connection with their growth. The oxidation-reduction potential has proved to be a very good means of classification and identification of the various bacterial strains. Moreover, although the studies performed are not numerous the said oxidation-reduction potential has also been shown to have a great importance in the determination of the immunisation processes of the organism and in its serological behaviour. The oxidation-reduction potential, furthermore, has found very large applications in the field of alimentation, from the problem of fermentations, such as the alcoholic fermentation and the bread fermentation, to the distinction between raw and boiled milk by means ofSchardinger's reaction. In the future, the possibilities for application and development of the oxidation-reduction potential appear to be even more considerable.
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    Cellular and molecular life sciences 2 (1946), S. 108-109 
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    Notes: Summary The measurement of meson masses in the cosmic radiation with a slowly expanding wilson chambre indicates mesons of different masses. There are at least two different masses, one between 100m 0 and 200m 0, and the other exceeding 200m 0.
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    Cellular and molecular life sciences 2 (1946), S. 512-512 
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    Cellular and molecular life sciences 2 (1946), S. 60-62 
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    Cellular and molecular life sciences 2 (1946), S. 70-71 
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    Notes: Summary A series of derivatives of triphenylethylene have been tested and some of them found to possess interesting oestrogenic properties; the relations between chemical constitution and oestrogenic activity have been discussed.
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    Cellular and molecular life sciences 2 (1946), S. 188-189 
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    Notes: Summary The ribonucleic and thymonucleic acids are antisulphamide forEremothecium Ashbyii and for aSaccharomyces. This effect is due partly to purines, first of all to adenine, but not to any pyrimidines. ForSaccharomyces, the action of adenine is 1/10 of that of PAB acid. The suggestion is made that the bacteriostatic effect of the sulphamide is connected with the nucleic acids of the cytoplasma and the nucleus. Those are studied cytologically with help of the ribonuclease-method ofBrachet. Strong differences appear between the normal cells and the intoxicated ones.
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    Cellular and molecular life sciences 2 (1946), S. 186-188 
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    Notes: Zusammenfassung In der Berührungsfläche einer an verschiedenen Metallen geriebenen polierten Glas- oder Quarzplatte werden helle, punktförmige Lichtblitze schon bei verhältnismäßig schwachen Reibungseffekten beobachtet. Die lokale Temperatur muß mindestens 550°C betragen. Die Beobachtung deutet auf kleinste Kontaktflächen und ist von Bedeutung für die Kenntnis der Reibungsvorgänge.
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    Cellular and molecular life sciences 2 (1946), S. 110-111 
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    Notes: Summary Saline extracts from rabbit's skeletal muscles obtained and dialyzed at the ionic strength 0.15 contain at least 11 electrophoretically distinct components. Five of these components (n, m, t, l, s) have properties which are comparable with some characteristics of the myogens ofWeber, another component (h) is probably myoalbumin. Muscular proteins which are more soluble at higher ionic strength are not homogenous: there must be not one but two or more electrophoretically different myosins. Much work is needed to establish accurate relations between electrophoretic and classical muscular proteins.
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    Cellular and molecular life sciences 2 (1946), S. 112-114 
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    Cellular and molecular life sciences 2 (1946), S. 115-115 
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    Cellular and molecular life sciences 2 (1946), S. 115-115 
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    Cellular and molecular life sciences 2 (1946), S. 116-116 
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    Cellular and molecular life sciences 2 (1946), S. 132-137 
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    Notes: Summary The permeability of cells to dissolved molecules is given by the permeation constant ofCollander (cm·h−1), whilst the permeability to water is measured by a filter constant (cm·Atm.−1·h−1). Therefore these constants are not comparable, and it is impossible to calculate quantitative data on the semipermeability of a cell. In this paper the permeation process is considered as a counterdiffusion of dissolved molecules into the cell and water out of the cell. From the two resulting diffusion equations formulae and a graphic method are derived, which permit to calculate the permeation constant of water, when the permeation constant of a given substance entering the cell is known. These constants are comparable and their ratio is a conclusive measure of the semipermeability.
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    Cellular and molecular life sciences 2 (1946), S. 232-232 
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    Cellular and molecular life sciences 2 (1946), S. 250-256 
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    Cellular and molecular life sciences 2 (1946), S. 261-262 
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    Cellular and molecular life sciences 2 (1946), S. 297-302 
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    Notes: Summary In this article we hope to have proved that there are as arace no pygmies in Melanesia but only peoples of small stature, resembling very much the peoples of normal stature. This makes it very probable that the so-called pygmies in other parts of the world arenot real pygmies but merely modifications of the people of normal stature caused by the influence of the mode of life and of nutrition. This theory is by the fact, that the “Pygmies” have nowhere their own language and that in their culture there is nothing separating them from other “parasitic-living” peoples of normal stature.
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    Cellular and molecular life sciences 2 (1946), S. 160-171 
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    Cellular and molecular life sciences 2 (1946), S. 295-297 
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    Notes: Summary Mr.Breuil reports on his last inspection of the finding places of anthropoids with human features on the high plateau of South Africa. He suggests an international exploitation and evaluation of the findings of anthropoids.
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    Cellular and molecular life sciences 2 (1946), S. 324-324 
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    Cellular and molecular life sciences 2 (1946), S. 323-324 
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    Cellular and molecular life sciences 2 (1946), S. 325-336 
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    Notes: Summary A general survey of the actual knowledges on the bone phosphatase is given. The enzyme plays an important rôle in the calcification of bone and teeth, this process being unable to proceed at a physiological speed without the participation of a phosphatase. The biological function of the enzyme is thus to accelerate and not to promote the calcification. The knowledge of the mechanism of phosphatase activity in the skeletal organs and of the chemical composition of the bone salt cannot lead to a full understanding of the physiology of ossification. A prominent function in this field is devoted to the proteins of the ground substance of bone and to their evolution. The study of the protein matrix of bone is now the most important subject of work for the biochemistry of ossification.
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    Cellular and molecular life sciences 2 (1946), S. 368-369 
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    Notes: Summary When electrophoretic studies are made on protein solutions of high viscosity, the beam of light used in the « Schieren » scanning method is partially reflected by the very sharp boundaries which leads to very asymmetric pictures taken by theTiselius-Longsworth method.
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    Cellular and molecular life sciences 2 (1946), S. 374-376 
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