Untersuchung der Sensitivität von Heizungs- / Lüftungsanlagen in Niedrigenergiehäusern

Bei Meßprojekten in denen Gebäude mit installierter Lüftungsanlage untersucht wurden, stellte man immer wieder ein breite Streuung der Meßwerte, als auch eine oftmals deutliche Abweichung vom vorher ermittelten Heizwärmebedarf der Gebäude fest. Es wird vermutet, daß diese Unterschiede systemspezifische Ursachen haben, ein Nachweis kann aufgrund der geringen Anzahl vorhandener Meßpunkte jedoch nicht geführt werden. Um die Sensitivität verschiedener Randbedingungen auf den Energieverbrauch zu ermitteln, wird im vorliegenden Forschungsprojekt ein Simulationsmodell erstellt. Das thermische Verhalten und die Durchströmung des Gebäudes werden durch ein gekoppeltes Modell abgebildet. Unterschiedliche Lüftungsanlagensysteme werden miteinander verglichen. Auf Basis vorhandener Meßdaten wird ein klimaabhängiges Modell zur Fensterlüftung entwickelt, welches in die Modellbildung der Gebäudedurchströmung mit einfließt. Feuchtegeregelte Abluftanlagen sind in der Lage den mittleren Luftwechsel auf ein hygienisch sinnvollen Wert zu begrenzen. Sie erweisen sich im Hinblick auf die Sensitivität verschiedener Randbedingungen als robuste Systeme. Trotz Einsatz von Lüftungsanlagen kann je nach Betriebszustand insbesondere bei Abluftanlagen keine ausreichende Luftqualität sichergestellt werden. Zukünftige Systeme dürfen das "Lüftungssystem" Fenster nicht vernachlässigen, sondern müssen es in das Gesamtkonzept mit einbeziehen.

Influence of the buffer environment on the Relative Biological Effectiveness of carbon ion radiation, investigated by Scanning Force Microscopy and gel electrophoresis

This work focuses on the analysis of the influence of environment on the relative biological effectiveness (RBE) of carbon ions on molecular level. Due to the high relevance of RBE for medical applications, such as tumor therapy, and radiation protection in space, DNA damages have been investigated in order to understand the biological efficiency of heavy ion radiation. The contribution of this study to the radiobiology research consists in the analysis of plasmid DNA damages induced by carbon ion radiation in biochemical buffer environments, as well as in the calculation of the RBE of carbon ions on DNA level by mean of scanning force microscopy (SFM). In order to study the DNA damages, besides the common electrophoresis method, a new approach has been developed by using SFM. The latter method allows direct visualisation and measurement of individual DNA fragments with an accuracy of several nanometres. In addition, comparison of the results obtained by SFM and agarose gel electrophoresis methods has been performed in the present study. Sparsely ionising radiation, such as X-rays, and densely ionising radiation, such as carbon ions, have been used to irradiate plasmid DNA in trishydroxymethylaminomethane (Tris buffer) and 4-(2-hydroxyethyl)-1-piperazineethanesulfonic acid (HEPES buffer) environments. These buffer environments exhibit different scavenging capacities for hydroxyl radical (HO0), which is produced by ionisation of water and plays the major role in the indirect DNA damage processes. Fragment distributions have been measured by SFM over a large length range, and as expected, a significantly higher degree of DNA damages was observed for increasing dose. Also a higher amount of double-strand breaks (DSBs) was observed after irradiation with carbon ions compared to X-ray irradiation. The results obtained from SFM measurements show that both types of radiation induce multiple fragmentation of the plasmid DNA in the dose range from D = 250 Gy to D = 1500 Gy. Using Tris environments at two different concentrations, a decrease of the relative biological effectiveness with the rise of Tris concentration was observed. This demonstrates the radioprotective behavior of the Tris buffer solution. In contrast, a lower scavenging capacity for all other free radicals and ions, produced by the ionisation of water, was registered in the case of HEPES buffer compared to Tris solution. This is reflected in the higher RBE values deduced from SFM and gel electrophoresis measurements after irradiation of the plasmid DNA in 20 mM HEPES environment compared to 92 mM Tris solution. These results show that HEPES and Tris environments play a major role on preventing the indirect DNA damages induced by ionising radiation and on the relative biological effectiveness of heavy ion radiation. In general, the RBE calculated from the SFM measurements presents higher values compared to gel electrophoresis data, for plasmids irradiated in all environments. Using a large set of data, obtained from the SFM measurements, it was possible to calculate the survive rate over a larger range, from 88% to 98%, while for gel electrophoresis measurements the survive rates have been calculated only for values between 96% and 99%. While the gel electrophoresis measurements provide information only about the percentage of plasmids DNA that suffered a single DSB, SFM can count the small plasmid fragments produced by multiple DSBs induced in a single plasmid. Consequently, SFM generates more detailed information regarding the amount of the induced DSBs compared to gel electrophoresis, and therefore, RBE can be calculated with more accuracy. Thus, SFM has been proven to be a more precise method to characterize on molecular level the DNA damage induced by ionizing radiations.

Einfluß der Gewässerversauerung auf Hyporheos und Bryorheos: Untersuchungen an zwei Waldbächen im Westharz

Im Rahmen der Fallstudie Harz sollte an der Schnittstelle zwischen Grundlagenforschung und angewandter Forschung ein Beitrag zur Klärung der Frage geleistet werden, inwieweit zwei Zuläufe der Sösetalsperre im Westharz versauert bzw. versauerungsgefährdet sind; aus diesem Stausee wird Trinkwasser für mehrere Gemeinden in Norddeutschland gewonnen. Die Belastung des fast vollständig bewaldeten Einzugsgebiets der Sösetalsperre mit luftbürtigen Schadstoffen (Saurer Regen) zählte zu den höchsten in Mitteleuropa. An jeweils drei Untersuchungsstellen der beiden Bäche Alte Riefensbeek (R1 bis R3) und Große Söse (S1 bis S3) wurden zwischen März 1987 und November 1988 Proben aus Moospolstern und dem hyporheischen Interstitial entnommen und physikalisch, chemisch und biologisch untersucht. Ergänzend wurden Wasserproben zwischen März 1986 und Oktober 1991 sowie vom April 1998 ebenso wie qualitative Fänge von Makroinvertebraten zwischen November 1986 und Juli 1990 sowie vom April 1998 ausgewertet. Die Analyse der tierischen Besiedlung der Moos- und Interstitialproben beschränkte sich auf die taxonomischen Gruppen Turbellaria (Strudelwürmer), Mollusca (Weichtiere), Amphipoda (Flohkrebse), Ephemeroptera (Eintagsfliegen), Plecoptera (Steinfliegen), Heteroptera (Wanzen), Megaloptera (Schlammfliegen), Coleoptera (Käfer), Trichoptera (Köcherfliegen) und Diptera (Zweiflügler). Der Grundsatz, daß normalverteilte und nicht normalverteilte Daten statistisch unterschiedlich behandelt werden müssen, wurde konsequent angewandt. Am Beispiel der Choriotopstruktur wurde gezeigt, daß die Auswahl des Analyseverfahrens das Ergebnis der ökologischen Interpretation multivariater statistischer Auswertung beeinflußt. Die Daten der Korngrößen-Verteilung wurden vergleichend einer univariaten und einer multivariaten statistischen Analyse unterworfen. Mit dem univariaten Verfahren wurden die Gradienten der ökologisch relevanten Korngrößen-Parameter eher erkannt als mit dem multivariaten Verfahren. Die Auswirkungen von Gewässerversauerung sowie anderer Umweltfaktoren (insgesamt 42 Faktoren) auf die Lebensgemeinschaften wurden anhand der Parameter Artenzahl, Besiedlungsdichte, Körpergröße und Biomasse untersucht. Abundanz, Biomasse und Körpergröße sowie die Umweltfaktoren wurden auf einem horizontalen Gradienten, d.h. im Längslauf der Bäche, und auf einem vertikalen Gradienten, d.h. fließende Welle / Bryorheon / Benthon versus Hyporheon, untersucht. Es wurde ein terminologisches System für die Kompartimente in der Fließgewässer-Aue vorgeschlagen, das in sich einheitlich ist. Es wurde ein neuer Moos-Vitalitätsindex für die Moospolster vorgestellt. Es wurden Bestimmungsschlüssel für die Larven der Chloroperlidae (Steinfliegen-Familie) und der Empididae (Tanzfliegen) in den beiden Harzbächen entwickelt. Die untersuchten Bachstrecken waren frei von Abwasserbelastung. An zwei Stellen wurde Wasser für einen Forellenteich ausgeleitet. Abgesehen von zwei meterhohen Abstürzen in der Großen Söse waren wasserbauliche Veränderungen ohne große Bedeutung. Das Abfluß-Regime war insofern nicht mehr natürlich, als beide Bäche in das System der bergbaulichen Bewässerungsgräben des Oberharzes eingebunden sind. Die Söse hatte ein F-nivopluviales Abfluß-Regime, der abflußreichste Doppelmonat war der März / April, die Unregelmäßigkeit des Abfluß-Regimes war sehr hoch, die Vorhersagbarkeit sehr niedrig, die monatlichen Abfluß-Maxima wiesen eine sehr geringe Konstanz auf. Der Zeitraum der biologischen Probenahme wurde von überdurchschnittlich vielen Tagen mit mäßig erhöhten Abflüssen geprägt, sehr große Hochwasser-Wellen fehlten aber. Die Abfluß-Dynamik wurde statistisch beschrieben. Das hydraulische Regime wurde anhand der Meßgrößen Fließgeschwindigkeit, Fließkraft und FROUDE-Zahl dargestellt. Der Zusammenhang zwischen Abfluß und Fließgeschwindigkeit auf der einen Seite und der Korngrößen-Verteilung auf der anderen Seite wurde statistisch untersucht, ebenfalls zwischen dem Abfluß und dem Kohlenstoff- und Stickstoff-Gehalt der Feinstpartikel sowie dem Wasserchemismus. In den Phasen ohne Hochwasser hatte das Hyporheal die Funktion einer Senke für Feinstkörner. Das Bachbett der Alten Riefensbeek war stabiler als das der Großen Söse. Insgesamt gesehen war das hyporheische Sediment in den quellnahen Abschnitten grobkörniger und auf den quellfernen Strecken feinkörniger. Der prozentuale Anteil der Feinstkörner im Hyporheal und Benthal nahm aber im Längslauf der Bäche ab. Dies ist ungewöhnlich, konnte aber nicht plausibel mit geologischen und hydrologischen Meßgrößen erklärt werden. Beide Bäche waren sommerkalt. Der Einfluß der Wassertemperatur auf die Larvalentwicklung wurde beispielhaft an den Taxa Baetis spp. und Leuctra gr. inermis untersucht. Es gab eine Tendenz, daß der Kohlenstoff- und Stickstoff-Gehalt der Feinstpartikel vom Benthal in das Hyporheal anstieg. Dies war ein weiterer Hinweis darauf, daß das Hyporheal die Funktion einer Senke und Vorratskammer für Nährstoffe hat. Der Zusammenhang zwischen partikulärer und gelöster Kohlenstoff-Fraktion wurde diskutiert. Im Hyporheon war die Nitrifikation nicht stärker als in der fließenden Welle. Es gab Hinweise, daß die sauren pH-Werte in der Großen Söse die Nitrifikation hemmten. Die Valenzen der Moos- und Tier-Taxa bezüglich Fließgeschwindigkeit, pH-Wert, Alkalinität sowie der Gehalte von Sauerstoff, Calcium, Magnesium, Kalium und Natrium wurden zusammengestellt. Das hyporheische Sediment war sehr grob und hatte eine hohe Porosität. Der Austausch zwischen fließender Welle und hyporheischem Wasser konnte deshalb sehr schnell erfolgen, es gab keine intergranulare Sprungschicht, die physikalischen und chemischen Tiefengradienten waren in den meisten Fällen gar nicht ausgeprägt oder nur sehr flach. Die Wassertemperatur des Freiwassers unterschied sich nicht signifikant von derjenigen im hyporheischen Wasser. Es gab -- von wenigen Ausnahmen bei pH-Wert, Leitfähigkeit und Sauerstoffgehalt abgesehen -- keine signifikanten Unterschiede zwischen dem Wasserchemismus der fließenden Welle und dem des Hyporheals. Die physikalischen und chemischen Voraussetzungen für die Refugialfunktion des Hyporheons waren deshalb für versauerungsempfindliche Taxa nicht gegeben. In der Tiefenverteilung der untersuchten Tiergruppen im Hyporheal lag das Maximum der Abundanz bzw. Biomasse häufiger in 10 cm als in 30 cm Tiefe. Daraus läßt sich aber keine allgemeine Gesetzmäßigkeit ableiten. Es wurde durchgehend die Definition angewendet, daß die Gewässerversauerung durch den Verlust an Pufferkapazität charakterisiert ist. Saure Gewässer können, müssen aber nicht versauert sein; versauerte Gewässer können, müssen aber nicht saures Wasser haben. Maßstab für das Pufferungsvermögen eines Gewässers ist nicht der pH-Wert, sondern sind die Alkalinität und andere chemische Versauerungsparameter. Der pH-Wert war auch operativ nicht als Indikator für Gewässerversauerung anwendbar. Die chemische Qualität des Bachwassers der Großen Söse entsprach aufgrund der Versauerung nicht den umweltrechtlichen Vorgaben bezüglich der Parameter pH-Wert, Aluminium, Eisen und Mangan, bzgl. Zink galt dies nur an S1. In der Alten Riefensbeek genügte das Hyporheal-Wasser in 30 cm Tiefe an R2 bzgl. des Sauerstoff-Gehalts nicht den umweltrechtlichen Anforderungen. Nur im Freiwasser an R1 genügten die Ammonium-Werte den Vorgaben der EG-Fischgewässer-Richtlinie, der Grenzwert wurde an allen anderen Meßstellen und Entnahmetiefen überschritten. Das BSB-Regime in allen Entnahmetiefen an R2, im Freiwasser an R3 und S1, im Hyporheal an R1 sowie in 30 cm Tiefe an R3 genügte nicht den Anforderungen der Fischgewässer-Richtlinie. Der Grenzwert für Gesamt-Phosphor wurde an S3 überschritten. In der Großen Söse war der Aluminium-Gehalt so hoch, daß anorganisches und organisches Aluminium unterschieden werden konnten. Besonders hohe Gehalte an toxischem anorganischen Aluminium wurden an Tagen mit Spitzen-Abflüssen und Versauerungsschüben gemessen. Erst die Ermittlung verschiedener chemischer Versauerungsparameter zeigte, daß auch die alkalischen Probestellen R2 und R3 mindestens versauerungsempfindlich waren. Die Messung bzw. Berechnung von chemischen Versauerungsparametern sollte deshalb zum Routineprogramm bei der Untersuchung von Gewässerversauerung gehören. Zu Beginn des Untersuchungsprogramms war angenommen worden, daß die mittleren und unteren Abschnitte der Alten Riefensbeek unversauert sind. Dieser Ansatz des Untersuchungsprogramms, einen unversauerten Referenzbach (Alte Riefensbeek) mit einem versauerten Bach (Große Söse) zu vergleichen, mußte nach der Berechnung von chemischen Versauerungsindikatoren sowie der Analyse der Abundanz- und Biomasse-Werte modifiziert werden. Es gab einen Versauerungsgradienten entlang der Probestellen: R1 (unversauert) R2 und R3 (versauerungsempfindlich bis episodisch leicht versauert) S2 und S3 (dauerhaft versauert) S1 (dauerhaft stark versauert). An S1 war das Hydrogencarbonat-Puffersystem vollständig, an S2 und S3 zeitweise ausgefallen. Die Versauerungslage an R2 und R3 war also schlechter als vorausgesehen. Unterschiede im Versauerungsgrad zwischen den Meßstellen waren nicht so sehr in unterschiedlichen Eintragsraten von versauernden Stoffen aus der Luft begründet, sondern in unterschiedlichen Grundgesteinen mit unterschiedlichem Puffervermögen. Der Anteil der verschiedenen sauren Anionen an der Versauerung wurde untersucht, die chemischen Versauerungsmechanismen wurden mit Hilfe von Ionenbilanzen und verschiedenen Versauerungsquotienten analysiert. Die beiden untersuchten Bäche waren von anthropogener Versauerung betroffen. Dabei spielte die Schwefel-Deposition (Sulfat) eine größere Rolle als die Stickstoff-Deposition (Nitrat). Die Probestelle S1 war immer schon in unbekanntem Maß natürlich sauer. Dieser natürlich saure Zustand wurde von der hinzugekommenen anthropogenen Versauerung bei weitem überragt. Die wenigen gewässerökologischen Daten, die im Wassereinzugsgebiet der Söse vor 1986 gewonnen wurden, deuten darauf hin, daß die Versauerung in den 70er und in der ersten Hälfte der 80er Jahre vom Boden und Gestein in die Bäche durchgeschlagen war. Dieser Versauerungsprozeß begann vermutlich vor 1973 in den Quellen auf dem Acker-Bruchberg und bewegte sich im Laufe der Jahre immer weiter talwärts in Richtung Trinkwasser-Talsperre. Der Mangel an (historischen) freilandökologischen Grundlagendaten war nicht nur im Untersuchungsgebiet, sondern ist allgemein in der Versauerungsforschung ein Problem. Wenn sich das Vorkommen von nah verwandten Arten (weitgehend) ausschließt, kann dies an der Versauerung liegen, z.B. war die Alte Riefensbeek ein Gammarus-Bach, die Große Söse ein Niphargus-Bach; dieses muß aber nicht an der Versauerung liegen, z.B. fehlte Habroleptoides confusa im Hyporheos an R3, Habrophlebia lauta hatte dagegen ihr Abundanz- und Biomasse-Maximum an R3. Zugleich lag das Maximum des prozentualen Anteils von Grobsand an R3, eine mögliche Ursache für diese interspezifische Konkurrenz. Die biologische Indikation von Gewässerversauerung mit Hilfe der Säurezustandsklassen funktionierte nicht in den beiden Harzbächen. Es wurde deshalb ein biologischer Versauerungsindex vorgeschlagen; dieser wurde nicht am pH-Wert kalibriert, sondern an der chemischen Versauerungslage, gekennzeichnet durch die Alkalinität und andere chemische Meßgrößen der Versauerung. Dafür wurden aufgrund der qualitativen und quantitativen Daten die häufigeren Taxa in die vier Klassen deutlich versauerungsempfindlich, mäßig versauerungsempfindlich, mäßig versauerungstolerant und deutlich versauerungstolerant eingeteilt. Es reicht nicht aus, die biologischen Folgen von Gewässerversauerung sowie Veränderungen in der Nährstoff-Verfügbarkeit und im sonstigen Wasserchemismus nur anhand der Artenzahl oder des Artenspektrums abzuschätzen. Vielmehr müssen quantitative Methoden wie die Ermittlung der Abundanzen angewandt werden, um anthropogene und natürliche Störungen des Ökosystems zu erfassen. Es wurde eine Strategie für die behördliche Gewässergüteüberwachung von Bachoberläufen vorgeschlagen, die flächendeckend die Versauerungsgefährdung erfassen kann. Die Auswirkungen der zeitlichen Dynamik des Versauerungschemismus wurden am Beispiel des versauerungsempfindlichen Taxons Baetis spp. (Eintagsfliegen) dargestellt. An S2 und S3 kam es zu starken Versauerungsschüben. Baetis konnte sich nicht ganzjährig halten, sondern nur in versauerungsarmen Phasen im Sommer und im Herbst; es gab einen Besiedlungskreislauf aus Ausrottungs- und Wiederbesiedlungsphasen. Die temporäre Population von Baetis an S2 und S3 bestand nur aus ersten Larvenstadien. Die Probestellen wurden auf horizontalen Gradienten der Umweltfaktoren angeordnet. Bei einigen Parametern gab es keinen Gradienten (z.B. Sauerstoff-Gehalt), bei anderen Parametern waren die Meßstellen auf sehr flachen Gradienten angeordnet (z.B. C:N-Quotient der Feinstkörner), bei den restlichen Meßgrößen waren die Gradienten sehr deutlich (z.B. Alkalinität). Bei den Längsgradienten von Abundanz und Biomasse waren alle Möglichkeiten vertreten: Zunahme (z.B. Leuctra pseudosignifera), Abnahme (z.B. Gammarus pulex), Maximum an der mittleren Probestelle (z.B. Leuctra pseudocingulata) und kein signifikanter Trend (z.B. Nemoura spp.). Abundanz und Biomasse zahlreicher taxonomischer Einheiten hatten ihr Maximum im Längslauf an den quellnächsten Probestellen R1 und S1, z.B. Protonemura spp. und Plectrocnemia spp. Die Lebensgemeinschaften an R1 und S1 waren allerdings völlig unterschiedlich zusammengesetzt. Die häufig vertretene Annahme, versauerte Gewässer seien biologisch tot, ist falsch. Unter Anwendung des 3. biozönotischen Grundprinzips wurde das Maximum von Abundanz und Biomasse in den quellnahen Abschnitten mit dem eustatistischen (stabilen) Regime von Wassertemperatur, Abfluß und Protonen-Gehalt, in der Alten Riefensbeek auch von Alkalinität und ALMER-Relation erklärt. Aufgrund der natürlichen und anthropogenen Störungen war im Längslauf der untersuchten Bäche keine natürliche biozönotische Gliederung des Artenbestands erkennbar. Die Korrelationsberechnungen zwischen den Umweltfaktoren und der Taxazahl ergaben, daß in erster Linie versauerungsrelevante Parameter -- Gehalte saurer Anionen, basischer Kationen und von Metallen, Alkalinität usw. -- die höchsten Korrelationskoeffizienten mit der Taxa-Zahl hatten; unter den natürlichen Meßgrößen zählten nur die Gehalte von DOC und TIC sowie der Anteil der Sande zu der Gruppe mit den höchsten Korrelationskoeffizienten. Die Korrelationsberechnungen zwischen den Umweltfaktoren und den Abundanzen ergab dagegen, daß die quantitative Zusammensetzung der Lebensgemeinschaft nicht nur durch die anthropogene Gewässerversauerung, sondern mindestens genauso durch einige natürliche Meßgrößen beeinflußt wurde. Es gab in den Harzbächen keinen ökologischen Superfaktor, der die quantitative Zusammensetzung der Lebensgemeinschaft überwiegend bestimmte. Auch die Meßgrößen der anthropogenen Gewässerversauerung waren nicht solch ein Superfaktor. Einen ähnlich hohen Einfluß auf die quantitative Zusammensetzung der Lebensgemeinschaft hatten die geologisch bestimmten Umweltfaktoren Leitfähigkeit und TIC-Gehalt, der von der Landnutzung bestimmte DOC-Gehalt sowie der Chlorid-Gehalt, der geologisch, möglicherweise aber auch durch den Eintrag von Straßensalz bestimmt wird. Die Mischung von anthropogenen und natürlichen Faktoren wurde in einem Modell der Wirkung von abiotischen Faktoren auf Bryorheos und Hyporheos dargestellt. Als Beispiel für die zeitliche Nutzung ökologischer Nischen wurde die Verteilung der Larven und Adulten der Dryopidae (Hakenkäfer) im Hyporheos und Bryorheos untersucht. Die Larven wurden vorzugsweise im Hyporheon, die Adulten im Bryorheon angetroffen. Die untersuchten Taxa wurden in die Varianten bryorheobiont, bryorheophil, bryorheotolerant, bryorheoxen und bryorheophob bzw. hyporheobiont, hyporheophil, hyporheotolerant, hyporheoxen und hyporheophob eingeteilt, um ihre räumliche Nutzung ökologischer Nischen zu beschreiben. Die gängige Lehrmeinung, daß das Hyporheon die Kinderstube benthaler Makroinvertebraten ist, konnte für zahlreiche Taxa bestätigt werden (z.B. Habrophlebia lauta). Für die bryorheophilen Taxa (z.B. Gammarus pulex und Baetis spp.) trifft diese Lehrmeinung in den beiden Harzbächen nicht zu. Vielmehr übernimmt das Bryorheon die Funktion einer Kinderstube. Die Larven von Plectrocnemia conspersa / geniculata sowie von Baetis spp. und Amphinemura spp. / Protonemura spp. neben Gammarus pulex zeigten eine Habitatbindung, die erstgenannte Gattung an das Hyporheal, die letztgenannten 3 Taxa an untergetauchte Moospolster (Bryorheal). Die Idee von der Funktion des Hyporheals als Kinderstube der Larven und Jungtiere, als Schutzraum gegen die Verdriftung durch Strömung und vor Fraßdruck durch Räuber sowie als Ort hohen Nahrungsangebots mußte für die letztgenannten 3 Taxa abgelehnt werden. Für sie übernahm das Bryorheal diese Aufgaben. Zwar waren die beiden Bäche oligotroph und die Nahrungsqualität der Feinstkörner im Hyporheal war niedrig. Die Abundanz- und Biomasse-Werte im Bryorheos und Hyporheos gehörten aber zu den weltweit höchsten. Es wurde das Paradoxon diskutiert, daß im Hyporheon der beiden Bäche Diatomeen-Rasen gefunden wurden, obwohl das Hyporheon lichtlos sein soll. Das Hyporheon wurde als ein Ökoton zwischen Benthon / Rheon und Stygon angesehen. Es wurden vier Haupttypen des Hyporheons beschrieben. Wegen des sehr unterschiedlichen Charakters des Hyporheons in verschiedenen Fließgewässern gibt es keinen einheitlichen Satz von abiotischen und biotischen Faktoren, mit denen das Hyporheon vom Benthon und Stygon abgegrenzt werden kann. In den beiden Harzbächen ähnelte das Hyporheon mehr dem Benthon als dem Stygon. Es konnte nicht anhand der chemischen Meßgrößen vom Benthon abgegrenzt werden, sondern anhand der physikalischen Meßgrößen Trübung und der Anteile von Feinsand und Schluffe/Tone sowie anhand der biologischen Parameter Summen-Abundanz und Summen-Biomasse. Aus der Typologie des Hyporheons folgt, daß ein bestimmtes Hyporheon nicht alle in der Literatur beschriebenen Funktionen innerhalb der Fließgewässer-Aue übernehmen kann. Es wurde ein Schema entwickelt, mit dem sich die optimale Liste der Parameter für die Untersuchung eines bestimmten Hyporheons auswählen läßt. Der Tendenz in der Fließgewässer-Ökologie, immer neue Konzepte zu entwickeln, die allgemeingültig sein sollen, wurde das Konzept vom individuellen Charakter von Fließgewässer-Ökosystemen entgegengestellt.

Approximate solutions and error estimates for a Stokes boundary value problem

The aim of this paper is the numerical treatment of a boundary value problem for the system of Stokes' equations. For this we extend the method of approximate approximations to boundary value problems. This method was introduced by V. Maz'ya in 1991 and has been used until now for the approximation of smooth functions defined on the whole space and for the approximation of volume potentials. In the present paper we develop an approximation procedure for the solution of the interior Dirichlet problem for the system of Stokes' equations in two dimensions. The procedure is based on potential theoretical considerations in connection with a boundary integral equations method and consists of three approximation steps as follows. In a first step the unknown source density in the potential representation of the solution is replaced by approximate approximations. In a second step the decay behavior of the generating functions is used to gain a suitable approximation for the potential kernel, and in a third step Nyström's method leads to a linear algebraic system for the approximate source density. For every step a convergence analysis is established and corresponding error estimates are given.

Hyperspectral field measurements to determine dry matter yield and nutritive value of legume-grass swards

Summary: Productivity, botanical composition and forage quality of legume-grass swards are important factors for successful arable farming in both organic and conventional farming systems. As these attributes can vary considerably within a field, a non-destructive method of detection while doing other tasks would facilitate a more targeted management of crops, forage and nutrients in the soil-plant-animal system. This study was undertaken to explore the potential of field spectral measurements for a non destructive prediction of dry matter (DM) yield, legume proportion in the sward, metabolizable energy (ME), ash content, crude protein (CP) and acid detergent fiber (ADF) of legume-grass mixtures. Two experiments were conducted in a greenhouse under controlled conditions which allowed collecting spectral measurements which were free from interferences such as wind, passing clouds and changing angles of solar irradiation. In a second step this initial investigation was evaluated in the field by a two year experiment with the same legume-grass swards. Several techniques for analysis of the hyperspectral data set were examined in this study: four vegetation indices (VIs): simple ratio (SR), normalized difference vegetation index (NDVI), enhanced vegetation index (EVI) and red edge position (REP), two-waveband reflectance ratios, modified partial least squares (MPLS) regression and stepwise multiple linear regression (SMLR). The results showed the potential of field spectroscopy and proved its usefulness for the prediction of DM yield, ash content and CP across a wide range of legume proportion and growth stage. In all investigations prediction accuracy of DM yield, ash content and CP could be improved by legume-specific calibrations which included mixtures and pure swards of perennial ryegrass and of the respective legume species. The comparison between the greenhouse and the field experiments showed that the interaction between spectral reflectance and weather conditions as well as incidence angle of light interfered with an accurate determination of DM yield. Further research is hence needed to improve the validity of spectral measurements in the field. Furthermore, the developed models should be tested on varying sites and vegetation periods to enhance the robustness and portability of the models to other environmental conditions.

Patent DE10 2004 037 519 B4 “Sensor Process and Device for Determining a Physical Value“. A Proof of Concept

At present, a fraction of 0.1 - 0.2% of the patients undergoing surgery become aware during the process. The situation is referred to as anesthesia awareness and is obviously very traumatic for the person experiencing it. The reason for its occurrence is mostly an insufficient dosage of the narcotic Propofol combined with the incapability of the technology monitoring the depth of the patient’s anesthetic state to notice the patient becoming aware. A solution can be a highly sensitive and selective real time monitoring device for Propofol based on optical absorption spectroscopy. Its working principle has been postulated by Prof. Dr. habil. H. Hillmer and formulated in DE10 2004 037 519 B4, filed on Aug 30th, 2004. It consists of the exploitation of Intra Cavity Absorption effects in a two mode laser system. In this Dissertation, a two mode external cavity semiconductor laser, which has been developed previously to this work is enhanced and optimized to a functional sensor. Enhancements include the implementation of variable couplers into the system and the implementation of a collimator arrangement into which samples can be introduced. A sample holder and cells are developed and characterized with a focus on compatibility with the measurement approach. Further optimization concerns the overall performance of the system: scattering sources are reduced by re-splicing all fiber-to-fiber connections, parasitic cavities are eliminated by suppressing the Fresnel reflexes of all one fiber ends by means of optical isolators and wavelength stability of the system is improved by the implementation of thermal insulation to the Fiber Bragg Gratings (FBG). The final laser sensor is characterized in detail thermally and optically. Two separate modes are obtained at 1542.0 and 1542.5 nm, tunable in a range of 1nm each. Mode Full Width at Half Maximum (FWHM) is 0.06nm and Signal to Noise Ratio (SNR) is as high as 55 dB. Independent of tuning the two modes of the system can always be equalized in intensity, which is important as the delicacy of the intensity equilibrium is one of the main sensitivity enhancing effects formulated in DE10 2004 037 519 B4. For the proof of concept (POC) measurements the target substance Propofol is diluted in the solvents Acetone and DiChloroMethane (DCM), which have been investigated for compatibility with Propofol beforehand. Eight measurement series (two solvents, two cell lengths and two different mode spacings) are taken, which draw a uniform picture: mode intensity ratio responds linearly to an increase of Propofol in all cases. The slope of the linear response indicates the sensitivity of the system. The eight series are split up into two groups: measurements taken in long cells and measurements taken in short cells.

Value Added by Quality Management

Abstract: Quality Management is an essential part of successful organisations. But the effect of it is mostly not directly visible. The effects are more indirect, and have a time lag till results appear. In today’s challenging times, all activities of an organisation have to proof their ability to add value. While Value Based Management is more focussed on financial value, other concepts and models like EFQM Excellence Model and Kaplan and Norton’s Balanced Score Card also point on values that are the basis and driver for financial success. Quality Management has to proof its effects on company values, and therefore the transacting mechanisms have to be identified and procedure to manage the process of Value Adding Quality Management has to be developed.

Application of biogas slurries from energy crops to arable soils and their impact on carbon and nitrogen dynamics

The use of renewable primary products as co-substrate or single substrate for biogas production has increased consistently over the last few years. Maize silage is the preferential energy crop used for fermentation due to its high methane (CH4) yield per hectare. Equally, the by-product, namely biogas slurry (BS), is used with increasing frequency as organic fertilizer to return nutrients to the soil and to maintain or increase the organic matter stocks and soil fertility. Studies concerning the application of energy crop-derived BS on the carbon (C) and nitrogen (N) mineralization dynamics are scarce. Thus, this thesis focused on the following objectives: I) The determination of the effects caused by rainfall patterns on the C and N dynamics from two contrasting organic fertilizers, namely BS from maize silage and composted cattle manure (CM), by monitoring emissions of nitrous oxide (N2O), carbon dioxide (CO2) and CH4 as well as leaching losses of C and N. II) The investigation of the impact of differences in soil moisture content after the application of BS and temperature on gaseous emissions (CO2, N2O and CH4) and leaching of C and N compounds. III) A comparison of BS properties obtained from biogas plants with different substrate inputs and operating parameters and their effect on C and N dynamics after application to differently textured soils with varying application rates and water contents. For the objectives I) and II) two experiments (experiment I and II) using undisturbed soil cores of a Haplic Luvisol were carried out. Objective III) was studied on a third experiment (experiment III) with disturbed soil samples. During experiment I three rainfall patterns were implemented including constant irrigation, continuous irrigation with periodic heavy rainfall events, and partial drying with rewetting periods. Biogas slurry and CM were applied at a rate of 100 kg N ha-1. During experiment II constant irrigation and an irrigation pattern with partial drying with rewetting periods were carried out at 13.5°C and 23.5°C. The application of BS took place either directly before a rewetting period or one week after the rewetting period stopped. Experiment III included two soils of different texture which were mixed with ten BS’s originating from ten different biogas plants. Treatments included low, medium and high BS-N application rates and water contents ranging from 50% to 100% of water holding capacity (WHC). Experiment I and II showed that after the application of BS cumulative N2O emissions were 4 times (162 mg N2O-N m-2) higher compared to the application of CM caused by a higher content of mineral N (Nmin) in the form of ammonium (NH4+) in the BS. The cumulative emissions of CO2, however, were on the same level for both fertilizers indicating similar amounts of readily available C after composting and fermentation of organic material. Leaching losses occurred predominantly in the mineral form of nitrate (NO3-) and were higher in BS amended soils (9 mg NO3--N m-2) compared to CM amended soils (5 mg NO3--N m-2). The rainfall pattern in experiment I and II merely affected the temporal production of C and N emissions resulting in reduced CO2 and enhanced N2O emissions during stronger irrigation events, but showed no effect on the cumulative emissions. Overall, a significant increase of CH4 consumption under inconstant irrigation was found. The time of fertilization had no effect on the overall C and N dynamics. Increasing temperature from 13.5°C to 23.5°C enhanced the CO2 and N2O emissions by a factor of 1.7 and 3.7, respectively. Due to the increased microbial activity with increasing temperature soil respiration was enhanced. This led to decreasing oxygen (O2) contents which in turn promoted denitrification in soil due to the extension of anaerobic microsites. Leaching losses of NO3- were also significantly affected by increasing temperature whereas the consumption of CH4 was not affected. The third experiment showed that the input materials of biogas plants affected the properties of the resulting BS. In particular the contents of DM and NH4+ were determined by the amount of added plant biomass and excrement-based biomass, respectively. Correlations between BS properties and CO2 or N2O emissions were not detected. Solely the ammonia (NH3) emissions showed a positive correlation with NH4+ content in BS as well as a negative correlation with the total C (Ct) content. The BS-N application rates affected the relative CO2 emissions (% of C supplied with BS) when applied to silty soil as well as the relative N2O emissions (% of N supplied with BS) when applied to sandy soil. The impacts on the C and N dynamics induced by BS application were exceeded by the differences induced by soil texture. Presumably, due to the higher clay content in silty soils, organic matter was stabilized by organo-mineral interactions and NH4+ was adsorbed at the cation exchange sites. Different water contents induced highest CO2 emissions and therefore optimal conditions for microbial activity at 75% of WHC in both soils. Cumulative nitrification was also highest at 75% and 50% of WHC whereas the relative N2O emissions increased with water content and showed higher N2O losses in sandy soils. In summary it can be stated that the findings of the present thesis confirmed the high fertilizer value of BS’s, caused by high concentrations of NH4+ and labile organic compounds such as readily available carbon. These attributes of BS’s are to a great extent independent of the input materials of biogas plants. However, considerably gaseous and leaching losses of N may occur especially at high moisture contents. The emissions of N2O after field application corresponded with those of animal slurries.

Status and Potential of Smallholder Livestock Production Systems in Xishuangbanna, southern P.R. China

With Chinas rapid economic development during the last decades, the national demand for livestock products has quadrupled within the last 20 years. Most of that increase in demand has been answered by subsidized industrialized production systems, while million of smallholders, which still provide the larger share of livestock products in the country, have been neglected. Fostering those systems would help China to lower its strong urban migration streams, enhance the livelihood of poorer rural population and provide environmentally save livestock products which have a good chance to satisfy customers demand for ecological food. Despite their importance, China’s smallholder livestock keepers have not yet gained appropriate attention from governmental authorities and researchers. However, profound analysis of those systems is required so that adequate support can lead to a better resource utilization and productivity in the sector. To this aim, this pilot study analyzes smallholder livestock production systems in Xishuangbanna, located in southern China. The area is bordered by Lao and Myanmar and geographically counts as tropical region. Its climate is characterized by dry and temperate winters and hot summers with monsoon rains from May to October. While the regionis plain, at about 500 m asl above sea level in the south, outliers of the Himalaya mountains reach out into the north of Xishuangbanna, where the highest peak reaches 2400 m asl. Except of one larger city, Jinghong, Xishuangbanna mainly is covered by tropical rainforest, areas under agricultural cultivation and villages. The major income is generated through inner-Chinese tourism and agricultural production. Intensive rubber plantations are distinctive for the lowland plains while small-scaled traditional farms are scattered in the mountane regions. In order to determine the current state and possible future chances of smallholder livestock production in that region, this study analyzed the current status of the smallholder livestock sector in the Naban River National Nature Reserve (NRNNR), an area which is largely representative for the whole prefecture. It covers an area of about 50square kilometer and reaches from 470 up to 2400 m asl. About 5500 habitants of different ethnic origin are situated in 24 villages. All data have been collected between October 2007 and May 2010. Three major objectives have been addressed in the study: 1. Classifying existing pig production systems and exploring respective pathways for development 2. Quantifying the performance of pig breeding systemsto identify bottlenecks for production 3. Analyzing past and current buffalo utilization to determine the chances and opportunities of buffalo keeping in the future In order to classify the different pig production s ystems, a baseline survey (n=204, stratified cluster sampling) was carried out to gain data about livestock species, numbers, management practices, cultivated plant species and field sizes as well associo-economic characteristics. Sampling included two clusters at village level (altitude, ethnic affiliation), resulting in 13 clusters of which 13-17 farms were interviewed respectively. Categorical Principal Component Analysis (CatPCA) and a two-step clustering algorithm have been applied to identify determining farm characteristics and assort recorded households into classes of livestock production types. The variables keep_sow_yes/no, TLU_pig, TLU_buffalo, size_of_corn_fields, altitude_class, size_of_tea_plantationand size_of_rubber_fieldhave been found to be major determinants for the characterization of the recorded farms. All farms have extensive or semi-intensive livestock production, pigs and buffaloes are predominant livestock species while chicken and aquaculture are available but play subordinate roles for livelihoods. All pig raisers rely on a single local breed, which is known as Small Ear Pig (SMEP) in the region. Three major production systemshave been identified: Livestock-corn based LB; 41%), rubber based (RB; 39%) and pig based (PB;20%) systems. RB farms earn high income from rubber and fatten 1.9 ±1.80 pigs per household (HH), often using purchased pig feed at markets. PB farms own similar sized rubber plantations and raise 4.7 ±2.77 pigs per HH, with fodder mainly being cultivated and collected in theforest. LB farms grow corn, rice and tea and keep 4.6 ±3.32 pigs per HH, also fed with collected and cultivated fodder. Only 29% of all pigs were marketed (LB: 20%; RB: 42%; PB: 25%), average annual mortality was 4.0 ±4.52 pigs per farm (LB: 4.6 ±3.68; RB: 1.9 ±2.14; PB: 7.1 ±10.82). Pig feed mainly consists of banana pseudo stem, corn and rice hives and is prepared in batches about two to three times per week. Such fodder might be sufficient in energy content but lacks appropriate content of protein. Pigs therefore suffer from malnutrition, which becomes most critical in the time before harvest season around October. Farmers reported high occurrences of gastrointestinal parasites in carcasses and often pig stables were wet and filled with manure. Deficits in nutritional and hygienic management are major limits for development and should be the first issues addressed to improve productivity. SME pork was found to be known and referred by local customers in town and by richer lowland farmers. However, high prices and lacking availability of SME pork at local wet-markets were the reasons which limited purchase. If major management constraints are overcome, pig breeders (PB and LB farms) could increase the share of marketed pigs for town markets and provide fatteners to richer RB farmers. RB farmers are interested in fattening pigs for home consumption but do not show any motivation for commercial pig raising. To determine the productivity of input factors in pig production, eproductive performance, feed quality and quantity as well as weight development of pigs under current management were recorded. The data collection included a progeny history survey covering 184 sows and 437 farrows, bi-weekly weighing of 114 pigs during a 16-months time-span on 21 farms (10 LB and 11 PB) as well as the daily recording of feed quality and quantity given to a defined number of pigs on the same 21 farms. Feed samples of all recorded ingredients were analyzed for their respective nutrient content. Since no literature values on thedigestibility of banana pseudo stem – which is a major ingredient of traditional pig feed in NRNNR – were found, a cross-sectional digestibility trial with 2x4 pigs has been conducted on a station in the research area. With the aid of PRY Herd Life Model, all data have been utilized to determine thesystems’ current (Status Quo = SQ) output and the productivity of the input factor “feed” in terms of saleable life weight per kg DM feed intake and monetary value of output per kg DM feed intake.Two improvement scenarios were simulated, assuming 1) that farmers adopt a culling managementthat generates the highest output per unit input (Scenario 1; SC I) and 2) that through improved feeding, selected parameters of reproduction are improved by 30% (SC II). Daily weight gain averaged 55 ± 56 g per day between day 200 and 600. The average feed energy content of traditional feed mix was 14.92 MJ ME. Age at first farrowing averaged 14.5 ± 4.34 months, subsequent inter-farrowing interval was 11.4 ± 2.73 months. Littersize was 5.8 piglets and weaning age was 4.3 ± 0.99 months. 18% of piglets died before weaning. Simulating pig production at actualstatus, it has been show that monetary returns on inputs (ROI) is negative (1:0.67), but improved (1:1.2) when culling management was optimized so that highest output is gained per unit feed input. If in addition better feeding, controlled mating and better resale prices at fixed dates were simulated, ROI further increased to 1:2.45, 1:2.69, 1:2.7 and 1:3.15 for four respective grower groups. Those findings show the potential of pork production, if basic measures of improvement are applied. Futureexploration of the environment, including climate, market-season and culture is required before implementing the recommended measures to ensure a sustainable development of a more effective and resource conserving pork production in the future. The two studies have shown that the production of local SME pigs plays an important role in traditional farms in NRNNR but basic constraints are limiting their productivity. However, relatively easy approaches are sufficient for reaching a notable improvement. Also there is a demand for more SME pork on local markets and, if basic constraints have been overcome, pig farmers could turn into more commercial producers and provide pork to local markets. By that, environmentally safe meat can be offered to sensitive consumers while farmers increase their income and lower the risk of external shocks through a more diverse income generating strategy. Buffaloes have been found to be the second important livestock species on NRNNR farms. While they have been a core resource of mixed smallholderfarms in the past, the expansion of rubber tree plantations and agricultural mechanization are reasons for decreased swamp buffalo numbers today. The third study seeks to predict future utilization of buffaloes on different farm types in NRNNR by analyzing the dynamics of its buffalo population and land use changes over time and calculating labor which is required for keeping buffaloes in view of the traction power which can be utilized for field preparation. The use of buffaloes for field work and the recent development of the egional buffalo population were analyzed through interviews with 184 farmers in 2007/2008 and discussions with 62 buffalo keepers in 2009. While pig based farms (PB; n=37) have abandoned buffalo keeping, 11% of the rubber based farms (RB; n=71) and 100% of the livestock-corn based farms (LB; n=76) kept buffaloes in 2008. Herd size was 2.5 ±1.80 (n=84) buffaloes in early 2008 and 2.2 ±1.69 (n=62) in 2009. Field work on own land was the main reason forkeeping buffaloes (87.3%), but lending work buffaloes to neighbors (79.0%) was also important. Other purposes were transport of goods (16.1%), buffalo trade (11.3%) and meat consumption(6.4%). Buffalo care required 6.2 ±3.00 working hours daily, while annual working time of abuffalo was 294 ±216.6 hours. The area ploughed with buffaloes remained constant during the past 10 years despite an expansion of land cropped per farm. Further rapid replacement of buffaloes by tractors is expected in the near future. While the work economy is drastically improved by the use of tractors, buffaloes still can provide cheap work force and serve as buffer for economic shocks on poorer farms. Especially poor farms, which lack alternative assets that could quickly be liquidizedin times of urgent need for cash, should not abandon buffalo keeping. Livestock has been found to be a major part of small mixed farms in NRNNR. The general productivity was low in both analyzed species, buffaloes and pigs. Productivity of pigs can be improved through basic adjustments in feeding, reproductive and hygienic management, and with external support pig production could further be commercialized to provide pork and weaners to local markets and fattening farms. Buffalo production is relatively time intensive, and only will be of importance in the future to very poor farms and such farms that cultivate very small terraces on steep slopes. These should be encouraged to further keep buffaloes. With such measures, livestock production in NRNNR has good chances to stay competitive in the future.

Alternative plant protein sources for pigs and chickens in the tropics – nutritional value and constraints: a review

In the tropics, a large number of smallholder farms contribute significantly to food security by raising pigs and poultry for domestic consumption and for sale on local markets. The high cost and, sometimes, the lack of availability of commercial protein supplements is one of the main limitations to efficient animal production by smallholders. Locally-grown forages and grain legumes offer ecological benefits such as nitrogen fixation, soil improvement, and erosion control which contribute to improve cropping efficiency. Besides these agronomical assets, they can be used as animal feeds in mixed farming systems. In this paper we review options to include locally-grown forages and grain legumes as alternative protein sources in the diets of pigs and poultry in order to reduce farmers’ dependence on externally-purchased protein concentrates. The potential nutritive value of a wide range of forages and grain legumes is presented and discussed. The influence of dietary fibre and plant secondary metabolites contents and their antinutritive consequences on feed intake, digestive processes and animal performances are considered according to the varying composition in those compounds of the different plant species and cultivars covered in this review. Finally, methods to overcome the antinutritive attributes of the plant secondary metabolites using heat, chemical or biological treatment are reviewed regarding their efficiency and their suitability in low input farming systems.

Optimization of Processing Technology for Commercial Drying of Bananas (Matooke)

Summary - Cooking banana is one of the most important crops in Uganda; it is a staple food and source of household income in rural areas. The most common cooking banana is locally called matooke, a Musa sp triploid acuminate genome group (AAA-EAHB). It is perishable and traded in fresh form leading to very high postharvest losses (22-45%). This is attributed to: non-uniform level of harvest maturity, poor handling, bulk transportation and lack of value addition/processing technologies, which are currently the main challenges for trade and export, and diversified utilization of matooke. Drying is one of the oldest technologies employed in processing of agricultural produce. A lot of research has been carried out on drying of fruits and vegetables, but little information is available on matooke. Drying of matooke and milling it to flour extends its shelf-life is an important means to overcome the above challenges. Raw matooke flour is a generic flour developed to improve shelf stability of the fruit and to find alternative uses. It is rich in starch (80 - 85%db) and subsequently has a high potential as a calorie resource base. It possesses good properties for both food and non-food industrial use. Some effort has been done to commercialize the processing of matooke but there is still limited information on its processing into flour. It was imperative to carry out an in-depth study to bridge the following gaps: lack of accurate information on the maturity window within which matooke for processing into flour can be harvested leading to non-uniform quality of matooke flour; there is no information on moisture sorption isotherm for matooke from which the minimum equilibrium moisture content in relation to temperature and relative humidity is obtainable, below which the dry matooke would be microbiologically shelf-stable; and lack of information on drying behavior of matooke and standardized processing parameters for matooke in relation to physicochemical properties of the flour. The main objective of the study was to establish the optimum harvest maturity window and optimize the processing parameters for obtaining standardized microbiologically shelf-stable matooke flour with good starch quality attributes. This research was designed to: i) establish the optimum maturity harvest window within which matooke can be harvested to produce a consistent quality of matooke flour, ii) establish the sorption isotherms for matooke, iii) establish the effect of process parameters on drying characteristics of matooke, iv) optimize the drying process parameters for matooke, v) validate the models of maturity and optimum process parameters and vi) standardize process parameters for commercial processing of matooke. Samples were obtained from a banana plantation at Presidential Initiative on Banana Industrial Development (PIBID), Technology Business Incubation Center (TBI) at Nyaruzunga – Bushenyi in Western Uganda. A completely randomized design (CRD) was employed in selecting the banana stools from which samples for the experiments were picked. The cultivar Mbwazirume which is soft cooking and commonly grown in Bushenyi was selected for the study. The static gravitation method recommended by COST 90 Project (Wolf et al., 1985), was used for determination of moisture sorption isotherms. A research dryer developed for this research. All experiments were carried out in laboratories at TBI. The physiological maturity of matooke cv. mbwazirume at Bushenyi is 21 weeks. The optimum harvest maturity window for commercial processing of matooke flour (Raw Tooke Flour - RTF) at Bushenyi is between 15-21 weeks. The finger weight model is recommended for farmers to estimate harvest maturity for matooke and the combined model of finger weight and pulp peel ratio is recommended for commercial processors. Matooke isotherms exhibited type II curve behavior which is characteristic of foodstuffs. The GAB model best described all the adsorption and desorption moisture isotherms. For commercial processing of matooke, in order to obtain a microbiologically shelf-stable dry product. It is recommended to dry it to moisture content below or equal to 10% (wb). The hysteresis phenomenon was exhibited by the moisture sorption isotherms for matooke. The isoteric heat of sorption for both adsorptions and desorption isotherms increased with decreased moisture content. The total isosteric heat of sorption for matooke: adsorption isotherm ranged from 4,586 – 2,386 kJ/kg and desorption isotherm from 18,194– 2,391 kJ/kg for equilibrium moisture content from 0.3 – 0.01 (db) respectively. The minimum energy required for drying matooke from 80 – 10% (wb) is 8,124 kJ/kg of water removed. Implying that the minimum energy required for drying of 1 kg of fresh matooke from 80 - 10% (wb) is 5,793 kJ. The drying of matooke takes place in three steps: the warm-up and the two falling rate periods. The drying rate constant for all processing parameters ranged from 5,793 kJ and effective diffusivity ranged from 1.5E-10 - 8.27E-10 m2/s. The activation energy (Ea) for matooke was 16.3kJ/mol (1,605 kJ/kg). Comparing the activation energy (Ea) with the net isosteric heat of sorption for desorption isotherm (qst) (1,297.62) at 0.1 (kg water/kg dry matter), indicated that Ea was higher than qst suggesting that moisture molecules travel in liquid form in matooke slices. The total color difference (ΔE*) between the fresh and dry samples, was lowest for effect of thickness of 7 mm, followed by air velocity of 6 m/s, and then drying air temperature at 70˚C. The drying system controlled by set surface product temperature, reduced the drying time by 50% compared to that of a drying system controlled by set air drying temperature. The processing parameters did not have a significant effect on physicochemical and quality attributes, suggesting that any drying air temperature can be used in the initial stages of drying as long as the product temperature does not exceed gelatinization temperature of matooke (72˚C). The optimum processing parameters for single-layer drying of matooke are: thickness = 3 mm, air temperatures 70˚C, dew point temperature 18˚C and air velocity 6 m/s overflow mode. From practical point of view it is recommended that for commercial processing of matooke, to employ multi-layer drying of loading capacity equal or less than 7 kg/m², thickness 3 mm, air temperatures 70˚C, dew point temperature 18˚C and air velocity 6 m/s overflow mode.