Mineral zoning and geochemistry of epithermal polymetallic Zn-Pb-Ag-Cu-Bi mineralization at Cerro de Pasco, Peru

The large Cerro de Pasco Cordilleran base metal deposit in central Peru is located on the eastern margin of a middle Miocene diatreme-dome complex and comprises two mineralization stages. The first stage consists of a large pyrite-quartz body replacing Lower Mesozoic Pucara carbonate rocks and, to a lesser extent, diatreme breccia. This body is composed of pyrite with pyrrhotite inclusions, quartz, and black and red chalcedony (containing hypogene hematite). At the contact with the pyrite-quartz body, the diatreme breccia is altered to pyrite-quartz-sericite-pyrite. This body was, in part, replaced by pipelike pyrrhotite bodies zoned outward to carbonate-replacement Zn-Pb ores hearing Fe-rich sphalerite (up to 24 mol % Fes). The second mineralization stage is partly superimposed on the first and consists of zoned east-west-trending Cu-Ag-(Au-Zn-Pb) enargite-pyrite veins hosted in the diatreme breccia in the western part of the deposit and well-zoned Zn-Pb-(Bi-Ag-Cu) carbonate-replacement orebodies; in both cases, sphalerite is Fe poor and the inner parts of the orebodies show typically advanced argillic alteration assemblages, including aluminum phosphate Sulfate (APS) minerals. The zoned enargite-pyrite veins display mineral zoning, from a core of enargite-pyrite +/- alunite with traces of Au, through an intermediate zone of tennantite, chalcopyrite, and Bi minerals to a poorly developed Outer zone hearing sphalerite-galena +/- kaolinite. The carbonate-hosted replacement ores are controlled along N 35 degrees E, N 90 degrees E, N 120 degrees E, and N 170 degrees E faults. They form well-zoned upward-flaring pipelike orebodies with a core of famatinite-pyrite and alunite, an intermediate zone with tetrahedrite-pyrite, chalcopyrite, matildite, cuprobismutite, emplectite, and other Bi minerals accompanied by APS minerals, kaolinite, and dickite, and an outer zone composed of Fe-poor sphalerite (in the range of 0.05-3.5 mol % Fes) and galena. The outermost zone consists of hematite, magnetite, and Fe-Mn-Zn-Ca-Mg carbonates. Most of the second-stage carbonate-replacement orebodies plunge between 25 degrees and 60 degrees to the west, suggesting that the hydrothermal fluids ascended from deeper levels and that no lateral feeding from the veins to the carbonate-replacement orebodies took place. In the Venencocha and Santa Rosa areas, located 2.5 km northwest of the Cerro de Pasco open pit and in the southern part of the deposit, respectively, advanced argillic altered dacitic domes and oxidized veins with advanced argillic alteration halos occur. The latter veins are possibly the oxidized equivalent of the second-stage enargite-pyrite veins located in the western part of the deposit. The alteration assemblage quartz-muscovite-pyrite associated with the pyrite-quartz body suggests that the first stage precipitated at slightly, acidic fin. The sulfide mineral assemblages define an evolutionary path close to the pyrite-pyrrhotite boundary and are characteristic of low-sulfidation states; they suggest that the oxidizing slightly acidic hydrothermal fluid was buffered by phyllite, shale, and carbonate host rock. However, the presence in the pyrite-quartz body of hematite within quartz suggests that, locally, the fluids were less buffered by the host rock. The mineral assemblages of the second mineralization stage are characteristic of high- to intermediate-sulfidation states. High-sulfidation states and oxidizing conditions were achieved and maintained in the cores of the second-stage orebodies, even in those replacing carbonate rocks. The observation that, in places, second-stage mineral assemblages are found in the inner and outer zones is explained in terms of the hydrothermal fluid advancing and waning. Microthermometric data from fluid inclusions in quartz indicate that the different ores of the first mineralization stage formed at similar temperatures and moderate salinities (200 degrees-275 degrees C and 0.2-6.8 wt % NaCl equiv in the pyrite-quartz body; 192 degrees-250 degrees C and 1.1-4.3 wt % NaCl equiv in the pyrrhotite bodies; and 183 degrees-212 degrees C and 3.2-4.0 wt % NaCl equiv in the Zn-Pb ores). These values are similar to those obtained for fluid inclusions in quartz and sphalerite from the second-stage ores (187 degrees-293 degrees C and 0.2-5.2 wt % NaCl equiv in the enargite-pyrite veins: 178 degrees-265 degrees C and 0.2-7.5 wt % NaCl equiv in quartz of carbonate-replacement orebodies; 168 degrees-999 degrees C and 3-11.8 wt % NaCl equiv in sphalerite of carbonate-replacement orebodies; and 245 degrees-261 degrees C and 3.2-7.7 wt % NaCl equiv in quartz from Venencocha). Oxygen and hydrogen isotope compositions oil kaolinite from carbonate-replacement orebodies (delta(18)O = 5.3-11.5%o, delta D = -82 to -114%o) and on alunite from the Venencocha and Santa Rosa areas (delta(18)O = 1.9-6.9%o, delta D = -56 to -73%o). Oxygen isotope compositions of quartz from the first and second stages have 6180 values from 9.1 to 1.7.8 per mil. Calculated fluids in equilibrium with kaolinite have delta(18)O values of 2.0 to 8.2 and delta D values of -69 to -97 per mil; values in equilibrium with alunite are -1.4 to -6.4 and -62 to -79 per mil. Sulfur isotope compositions of sulfides from both stages have a narrow range of delta(34)S values, between -3.7 and +4.2 per mil; values for sulfates from the second stage are between 4.2 and 31.2 per mil. These results define two mixing trends for the ore-forming fluids. The first trend reflects mixing between a moderately saline (similar to 10 wt % NaCl equiv) magmatic end member that had degassed (as indicated by the low delta D values) and meteoric water. The second mixing indicates condensation of magmatic vapor with HCl and SO(2) into meteoric water, which formed alunite. The hydrothermal system at Cerro de Pasco was emplaced at a shallow depth (similar to 500 m) in the epithermal and upper part of a porphyry environment. The similar temperatures and salinities obtained for the first stage and second stages, together with the stable isotope data, indicate that both stages are linked and represent successive stages of epithermal polymetallic mineralization in the upper part of a porphyry system.

'Royal Gala' apple quality stored under ultralow oxygen concentration and low temperature conditions

The objective of this work was to evaluate the interaction of ultralow oxygen concentrations (ULO) with storage temperatures and carbon dioxide partial pressures and its influence on fruit quality preservation and on the occurrence of physiological disorders in 'Royal Gala' apples. The experiment was carried out in a completely randomized design, with four replicates 25-fruit. ULO conditions (1.0 kPa O2 + 2.0 kPa CO2; 0.8 kPa O2 + 1.5 kPa CO2; 0.8 kPa O2 + 1.0 kPa CO2; 0.6 kPa O2 + 1.5 kPa CO2; and 0.6 kPa O2 + 1.0 kPa CO2) were tested at 0, 0.5 and 1.0°C, in a 5x3 factorial arrangement. Fruit quality and ripening analyses were performed after eight-month storage plus seven days of shelf-life at 20°C. Oxygen partial pressures below 0.8 kPa increased the occurrence of internal breakdown and mealiness. The best ULO condition was 1.0 kPa O2 + plus 2.0 kPa CO2 at 1.0°C. The interaction of ULO conditions and storage temperatures shows the need of increasing O2 partial pressure at higher storage temperatures.

Forecasting the Earth"s radiation belts and modeling solar energetic particle events: Recent results from SPACECAST

High-energy charged particles in the van Allen radiation belts and in solar energetic particle events can damage satellites on orbit leading to malfunctions and loss of satellite service. Here we describe some recent results from the SPACECAST project on modelling and forecasting the radiation belts, and modelling solar energetic particle events. We describe the SPACECAST forecasting system that uses physical models that include wave-particle interactions to forecast the electron radiation belts up to 3 h ahead. We show that the forecasts were able to reproduce the >2 MeV electron flux at GOES 13 during the moderate storm of 7-8 October 2012, and the period following a fast solar wind stream on 25-26 October 2012 to within a factor of 5 or so. At lower energies of 10- a few 100 keV we show that the electron flux at geostationary orbit depends sensitively on the high-energy tail of the source distribution near 10 RE on the nightside of the Earth, and that the source is best represented by a kappa distribution. We present a new model of whistler mode chorus determined from multiple satellite measurements which shows that the effects of wave-particle interactions beyond geostationary orbit are likely to be very significant. We also present radial diffusion coefficients calculated from satellite data at geostationary orbit which vary with Kp by over four orders of magnitude. We describe a new automated method to determine the position at the shock that is magnetically connected to the Earth for modelling solar energetic particle events and which takes into account entropy, and predict the form of the mean free path in the foreshock, and particle injection efficiency at the shock from analytical theory which can be tested in simulations.

Soil diffuse degassing and thermal energy fluxes from the southern Lakki plain, Nisyros (Greece)

Two diffuse soil CO2 flux surveys from the southern Lakki plain show that CO2 is mainly released from the hydrothermal explosion craters. The correspondence between high CO2 fluxes and elevated soil temperatures suggests that a flux of hot hydrothermal fluids ascends towards the surface. Steam mostly condenses near the surface and the heat given off is conductively transferred to the atmosphere through the soil, accompanied by a large CO2 flux. Tt was calculated, that 68 t d(-1) of hydrothermal CO2 are released through the total surveyed area of similar to1.3 km(2) Admitting that a steam flux of 2200 t d(-1) accompanies this CO2 flux, the thermal energy released through steam condensation amounts to 58 MW.

Intracellular thiol-mediated modulation of epithelial sodium channel activity.

The epithelial sodium channel ENaC is physiologically important in the kidney for the regulation of the extracellular fluid volume, and in the lungs for the maintenance of the appropriate airway surface liquid volume that lines the pulmonary epithelium. Besides the regulation of ENaC by hormones, intracellular factors such as Na(+) ions, pH, or Ca(2+) are responsible for fast adaptive responses of ENaC activity to changes in the intracellular milieu. In this study, we show that ENaC is rapidly and reversibly inhibited by internal sulfhydryl-reactive molecules such as methanethiosulfonate derivatives of different sizes, the metal cations Cd(2+) and Zn(2+), or copper(II) phenanthroline, a mild oxidizing agent that promotes the formation of disulfide bonds. At the single channel level, these agents applied intracellularly induce the appearance of long channel closures, suggesting an effect on ENaC gating. The intracellular reducing agent dithiothreitol fully reverses the rundown of ENaC activity in inside-out patches. Our observations suggest that changes in intracellular redox potential modulate ENaC activity and may regulate ENaC-mediated Na(+) transport in epithelia. Finally, substitution experiments reveal that multiple cysteine residues in the amino and carboxyl termini of ENaC subunits are responsible for this thiol-mediated inhibition of ENaC.

Sea state effect on the sea surface emissivity at L-band

In May 1999, the European Space Agency (ESA) selected the Earth Explorer Opportunity Soil Moisture and Ocean Salinity (SMOS) mission to obtain global and frequent soil moisture and ocean salinity maps. SMOS' single payload is the Microwave Imaging Radiometer by Aperture Synthesis (MIRAS), an L-band two-dimensional aperture synthesis radiometer with multiangular observation capabilities. At L-band, the brightness temperature sensitivity to the sea surface salinity (SSS) is low, approximately 0.5 K/psu at 20/spl deg/C, decreasing to 0.25 K/psu at 0/spl deg/C, comparable to that to the wind speed /spl sim/0.2 K/(m/s) at nadir. However, at a given time, the sea state does not depend only on local winds, but on the local wind history and the presence of waves traveling from far distances. The Wind and Salinity Experiment (WISE) 2000 and 2001 campaigns were sponsored by ESA to determine the impact of oceanographic and atmospheric variables on the L-band brightness temperature at vertical and horizontal polarizations. This paper presents the results of the analysis of three nonstationary sea state conditions: growing and decreasing sea, and the presence of swell. Measured sea surface spectra are compared with the theoretical ones, computed using the instantaneous wind speed. Differences can be minimized using an "effective wind speed" that makes the theoretical spectrum best match the measured one. The impact on the predicted brightness temperatures is then assessed using the small slope approximation/small perturbation method (SSA/SPM).

A model of the wind direction signature in the Stokes emission vector from the ocean surface at microwave frequencies

This paper presents a model of the Stokes emission vector from the ocean surface. The ocean surface is described as an ensemble of facets with Cox and Munk's (1954) Gram-Charlier slope distribution. The study discusses the impact of different up-wind and cross-wind rms slopes, skewness, peakedness, foam cover models and atmospheric effects on the azimuthal variation of the Stokes vector, as well as the limitations of the model. Simulation results compare favorably, both in mean value and azimuthal dependence, with SSM/I data at 53° incidence angle and with JPL's WINDRAD measurements at incidence angles from 30° to 65°, and at wind speeds from 2.5 to 11 m/s.

Esityksen valmistaminen muistojen pohjalta

Opinnäytteeni pohtii esitystä ja työtapaa, jossa lähtökohtana ovat työryhmän muistot. Työryhmän jäsenten yksityisistä muistoista muokataan julkinen esitys. Tutkin esityksen valmistamista muistoja hyväksikäyttäen sekä tuon esille omia kokemuksia tällaisesta työskentelystä. Käytän muistoja lähtökohtana taiteelliseen lopputulokseen, joka tässä tapauksessa on teatteriesitys. Koen muistot luonnonvarana, joita hyödyntämällä saadaan ainutkertainen, mielenkiintoinen esitys. Esitys valmistetaan ryhmätyönä, yhden työryhmän jäsenen kuitenkin toimiessa projektissa ohjaajana. Pidän esitysprosessia tärkeänä kaikille asianosaisille, sillä sen aikana kohdataan kunkin jäsenen muisto uudelleen ja siitä muokkautuu uusi, julkinen tulkinta, joka voi taas synnyttää samaistumista katsojan omassa muistomaailmassa. Teatterin tekeminen on muodon antamista jollekin asialle. Tässä prosessissa annetaan muoto ennalta valitulle teemalle työryhmän muistoja rakennusmateriaaleina käyttäen. Prosessi on avoin ja siinä ohjaajalla ei ole etukäteissuunnitelmaa esityksen kulusta muutoin kuin teeman suhteen. Ohjaaja ei ole suunnitellut projektia valmiiksi, vaan yhdessä työryhmän kanssa hän työskentelee prosessoiden sitä materiaalia, mikä nousee työryhmän jäsenten omista muistoista.

Tracing of the Rhône River, wastewater, and mixing within Lake Geneva : stable isotope compositions of water and dissolved inorganic carbon

This study presents an evaluation of the stable isotopic composition of water (hydrogen and oxygen) and dissolved inorganic carbon (DIC) of Lake Geneva, a deep, peri-alpine lake situated at the border between Switzerland and France. The research goal is to apply vertical and seasonal variations of the isotope compositions to evaluate mixing processes of pollutants, nutrients and oxygen. Depth profiles were sampled at different locations throughout Lake Geneva on a monthly and seasonal basis over the course of three years (2009-2011). The results of the oxygen isotopic composition indicate a Rhône River interflow, which can be traced for about 55 km throughout the lake during summer. The Rhône River interflow is 7 to 15 m thick and the molar fraction of Rhône water is estimated to amount up to 37 %. Calculated density of the water and measured isotopic compositions demonstrate that the interflow depth changes in conjunction with the density gradient in the water column during fall. Partial pressure of CO2 indicates that the epilimnion is taking up CO2 from the atmosphere between spring and fall. The epilimnion is most enriched in 13CDIC in September and a progressive depletion of 13CDIC can be observed in the metalimnion from spring to late fall. This stratification is dependent on the local density stratification and the results demonstrate that parameters, which are indicating photosynthesis, are not necessarily linked to δ13CDIC values. In addition, the amount of primary production shows a strong discrepancy between summer 2009 and 2010, but δ13CDIC values of the epilimnion and metalimnion do not indicate variations. In the hypolimnion of the deep lake δ13CDIC values are constant and the progressive depletion allows tracing remineralization processes. The combination of stable carbon and oxygen isotopic compositions allows furthermore tracing Rhône River water fractions, as well as wastewater, stormwater and anthropogenic induced carbon in the water column of the shallow Bay of Vidy. In combination with the results of measured micropollutants, the study underlines that concentrations of certain substances may be related to the Rhône River interflow and/or remineralization of particulate organic carbon. Water quality monitoring and research should therefore be extended to the metalimnion as well as sediment water interface.

Carbon-isotope stratigraphy of the Liesberg Beds Member (Oxfordian, Swiss Jura) using echinoids and crinoids

The Liesberg Beds form the transition between the lower Oxfordian dark coloured marls (Renggeri Member and the Terrain a Chailles Member) and the middle Oxfordian reefal limestones (St-Ursanne Formation). Both lithofacies and biofacies are diverse and evolve rapidly up-section. Stable isotope studies of whole-rock samples are therefore excluded. In search for a convenient isotopic marker, we measured carbon isotope compositions of several fossil groups and chose crinoid stems of Millericrinus spp and echinoid spines of Paracidaris spp because of their abundance throughout the section and the small variations of delta(13)C within one fossil and between fossils from the same stratigraphic level. The delta(13)C values of echinoderms largely reflect earliest diagenetic conditions at the seawatersediment interface. The porous stereome structure secreted of high Mg-calcite by echinoderms has a high reactive surface/volume ratio, which triggers the precipitation of very early syntaxial cements. In the four studied sections reproducible carbon isotope shifts were observed both for Millericrinus spp stems and Paracidaris spp spines. A negative delta(13)C shift of 1-1.5 parts per thousand was observed near the base of the section, just above the transition from Terrain a Chailles Member, where the first corals occur. In the middle and upper part of the four sections, characterised by a stepwise increase of corals and the macrofossils, a positive delta(13)C Shift of about 2 parts per thousand was observed. Despite the highly variable lithologic composition of the Liesberg Beds;Member, carbon isotope shifts seem to be consistent and warrant an interpretation as an original signal, controlled by the isotopic composition of dissolved carbonic acid in seawater. We explain the heavy delta(13)C values (approximate to 2-2.3 parts per thousand) in the lower Liesberg Beds as a transition from an oxygen-limited environment (Terrain a Chailles Member) to the Liesberg Beds Member. The lowest delta(13)C values (approximate to 1-1.5 parts per thousand) correspond to a large input of dissolved nutrients to the platform under oxidizing conditions. The ensuing positive shift (between 2.5 and 3.5 parts per thousand), however, seems to correspond to a general trend of opening up of the platform and connection to open marine waters. Positive delta(13)C values in the upper Liesberg Beds is interpreted as a result of important accelareted extraction of organic carbon from the ocean reservoir, that occurred possibly during periods of warm and humid climate.

Deposition rates of sidestream tobacco smoke particles in an experimental chamber

The natural dissipation rates of sidestream smoke (SS) particles dispersed in a chamber were studied from the standpoint of a static atmosphere and were expressed as half-lives of residence in the air. The half-lives for particles less than 0.3 micron, 0.3-0.5 micron and 0.5-1 micron were found to be 25.5, 12.8 and 4.9 h, respectively. Total particulate matter (TPM) decreases by half after 6.2 h. Other data on diluted SS in the indoor air were also reported.

Up-conversion effect of Er- and Yb-doped ZnO thin films

Visible up-conversion in ZnO:Er and ZnO:Er:Yb thin films deposited by RF magnetron sputtering under different O2-rich atmospheres has been studied. Conventional photoluminescence (325 nm laser source) and up-conversion (980 nm laser source) have been performed in the films before and after an annealing process at 800 °C. The resulting spectra demonstrate that the thermal treatment, either during or post-deposition, activates optically the Er3+ ions, being the latter process much more efficient. Moreover, the atmosphere during deposition was also found to be an important parameter, as the deposition under O2 flow increases the optical activity of Er+3 ions. In addition, the inclusion of Yb3+ ions into the films has shown an enhancement of the visible up-conversion emission at 660 nm by a factor of 4, which could be associated to either a better energy transfer from the 2F5/2 Yb level to the 4I11/2 Er one, or to the prevention of having Er2O3 clustering in the films.

Vaihtoehtoalkalit mekaanisen massan peroksidivalkaisussa

Tehokkain tapavalkaista mekaanisesti kuidutettua puumassaa on suorittaa se hapettavasti peroksidikemikaalilla vahvasti alkalisissa oloissa. Perinteisesti alkalisuus on aikaansaatu natriumhydroksidin ja -silikaatin avulla. Se kuitenkin liuottaa massasta merkittävästi ligniiniä, mikä huonontaa saantoa ja suurentaa valkaisun jätevesien orgaanisen hiilen määrää sekä kemiallista hapenkulutusta. Yhä kovenevien vaaleustavoitteiden ja tiukentuneen vedenkäytön seurauksena on syntynyt tarve etsiä parempia valkaisun alkaleja. Kirjallisuuden pohjalta valittiinkokeellisesti tutkittaviksi alkaleiksi magnesiumhydroksidi, magnesiumoksidi, kalsiumhydroksidi sekä kalsiumoksidi. Niiden toimivuutta hapettavan vetyperoksidivalkaisun alkaleina tutkittiin valkaisukokein natriumsilikaattilisäyksen kanssa sekä ilman. Näistä parhaiten toimivaksi osoittautui Mg(OH)2. Sen avulla suoritettiin jatkoksi laboratoriokoevalkaisuja korkeassa sakeudessa. Keski- ja korkeasakeusvalkaisukokeiden tulosten mukaan käytettäessä Mg(OH)2 -alkalia natriumydroksidin ja -silikaatin asemesta jää massan loppuvaaleus noin yhden ISO-prosentin verran heikommaksi. Tällöin valkaisusuodoksessa oli vain varsin vähäinen määrä massasta liuennutta orgaanista hiiliainesta, noin 45 % siitä, mitä natriumin yhdisteiden käyttö vertailukokeessa tuotti. Tulosta varmennettiin suorittamalla korkea-sakeusvalkaisukokeita hiokemassatehtaan olosuhteissa, massoilla ja kiertovesillä.Myös tehdaskokeiden mukaan valkaistun massan loppuvaaleus jää noin yhden ISO-prosentin alhaisemmaksi, mutta valkaisusuodoksen orgaanisen hiilen määrä (TOC) jääalle puoleen Na-kemikaalein suoritetusta vertailukokeesta.

Metsäteollisuuden prosessien suunnittelu simulointiympäristössä

Prosessisimulointiohjelmistojen käyttö on yleistynyt paperiteollisuuden prosessien kartoituksessa ja kyseiset ohjelmistot ovat jo pitkään olleet myös Pöyry Engineering Oy:n työkaluja prosessisuunnittelussa. Tämän työn tavoitteeksi määritettiin prosessisimulointiohjelmistojen käytön selvittäminen suomalaisissa paperitehtaissa sekä prosessisimuloinnin tulevaisuuden näkymien arviointi metsäteollisuuden suunnittelupalveluissa liiketoiminnan kehittämiseksi. Työn teoriaosassa selvitetään mm. seuraavia asioita: mitä prosessisimulointi on, miksi simuloidaan ja mitkä ovat simuloinnin hyödyt ja haasteet. Teoriaosassa esitellään yleisimmät käytössä olevat prosessisimulointiohjelmistot, simulointiprosessin eteneminen sekä prosessisimuloinnin tuotteistamisen vaatimuksia. Työn kokeellisessa osassa selvitettiin kyselyn avulla prosessisimulointiohjelmistojen käyttöä Suomen paperitehtaissa. Kysely lähetettiin kaikille Suomen tärkeimmille paperitehtaille. Kyselyn avulla selvitettiin mm, mitä ohjelmia käytetään, mitä on simuloitu, mitä pitää vielä simuloida ja kuinka tarpeellisena prosessisimulointia pidetään. Työntulokset osoittavat, että kaikilla kyselyyn vastanneilla suomalaisilla paperitehtailla on käytetty prosessisimulointia. Suurin osa simuloinneista on tehty konelinjoihin sekä massa- ja vesijärjestelmiin. Tulevaisuuden tärkeimpänä kohteena pidetään energiavirtojen simulointia. Simulointimallien pitkäjänteisessä hyödyntämisessä ja ylläpidossa on kehitettävää, jossa simulointipalvelujen hankkiminen palveluna on tehtaille todennäköisin vaihtoehto. Johtopäätöksenä on se, että tehtailla on tarvetta prosessisimuloinnille. Ilmapiiri on kyselytuloksien mukaan suotuisa ja simulointi nähdään tarpeellisena työkaluna. Prosessisimuloinnin markkinointia, erillispalvelutuotteen lisäksi, kannattaisi kehittää siten, että simulointimallin ylläpito jatkuisi projektin jälkeen lähipalveluna. Markkinointi pitäisi tehdä jo projektin alkuvaiheessa tai projektin aikana. Simulointiohjelmien kirjosta suunnittelutoimiston kannattaa valita simulointiohjelmistoja, jotka sopivat sille parhaiten. Erityistapauksissa muiden ohjelmien hankintaa kannattaa harkita asiakkaan toivomusten mukaisesti.

Kriittiset menestystekijät suorituskyvyn mittaamisen tukena

Suorituskyvyn mittaamiseen on alettu kiinnittää entistä enemmän huomiota, kun julkinen sektori on siirtynyt uusiin palkkausjärjestelmiin. Onnistuneen suorituskyvyn mittauksen taustalla on onnistuminen kriittisten menestystekijöiden määrittämisessä. Kriittisten menestystekijöiden yhdistämistä suorituskyvyn mittaamiseen ei ole kuitenkaan tutkittu kovinkaan paljon. Työssä selvitetään puolustusvoimien materiaalihankkeiden kriittiset menestystekijät. Työssä tarkastellaan kriittisten menestystekijöiden ja suorituskyvyn mittaamisen aikaisempaa tutkimusta ja teoriaa, jota on sovellettu työn empiirisessä osassa. Empiirisen aineiston muodostaa hankehenkilöstölle ja - johdolle suunnattu kysely. Kriittisten menestystekijöidenmäärittämisessä ja suorituskyvyn mittaamisen välistä yhteyttä tutkittaessa on käytetty hyväksi teoriaa, SWOT-analyysia, kyselyn tuloksia ja asiakkaan asiakirjoja. Valitut kriittiset menestystekijät ovat henkilöstö, avoin ympäristö sekä henki, riittävät resurssit, resurssien kustannustehokas käyttö,realistinen ja selkeä tavoite, vaatimustenmäärittelyn onnistuminen, yksityiskohtaiset ja päivitettävät suunnitelmat. Työssä pohditaan myös suorituskyvyn mittaamista hankkeissa ja tuloksena ehdotetaan SAKE- järjestelmän käyttöönottoa. Näkökulmiksi SAKE- järjestelmään ehdotetaan henkilöstöä, laatua, johtoa ja resursseja. Työn pohjalta tulisi käynnistää jatkotyö, jossa materiaalihankkeille luotaisiin varsinainen suorituskyvyn mittaristo.