712 resultados para Deep leadership


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Tutkielman tavoitteena on selvittää, minkälainen kuva kadettikurssilaisten puheessa rakentuu hyvästä johtajuudesta, keitä he mainitsevat ihanteellisina johtajina ja mitä sankaruus heille merkitsee. Kadettien näkemyksiä tarkastellaan puolustusvoimien ”perinteisen” ja uuden syväjohtamisen mukaisen johtajakoulutuksen valossa. Tutkimus on kvalitatiivinen ja menetelmänä käytetään diskurssianalyysiä. Ympäröivä kulttuuri muokkaa, mallintaa ja uusintaa ihmisten sosiaalista todellisuutta. Puolustusvoimien johtajakoulutuksella, sotilasorganisaation kulttuurilla ja historian esikuvallisilla sotilasjohtajilla on keskeinen merkitys kadettikurssilaisten hyvä johtaja –kuvan muodostumisessa. Diskursseissa käsitys hyvästä johtajuudesta rakentuu sekä perinteisesti maskuliinisina pidettyjen että ”uusien” pehmeämpien johtamisarvojen kautta. Kadettien mukaan sotilasjohtaja voi olla niin käskijä ja valvoja kuin alaiset huomioiva, osallistuva johtaja. Suomalaisista sotilasjohtajista esille nostetaan Carl Gustav Mannerheim, Lauri Törni ja Adolf Ehrnrooth. Kadettikurssilaiset säilyttävät puheessaan sekä perinteiseen sotilasjohtamiseen liittyviä myyttejä että rakentavat syväjohtamisen mallia mukailevia johtamisarvoja.

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Tämän tutkielman tarkoituksena on osallistua keskusteluun S-ryhmän johtamiskulttuurista, jossa on viime vuosina alettu korostaa esimiehen ihmisten johtamisen valmiuksia yhtenä tämän päivän ja tulevaisuuden keskeisenä menestyksen tekijänä. Tässä tutkielmassa perehdytään syvä-johtamisen esimiesvalmennukseen. Kohdeorganisaatio on Hankkija-Maatalous Oy. Tutkielman tavoitteena on selvittää, mitä Syväjohtaminen DL Oy:n esimiesvalmennus syväjohtamisen keinoin on ja kuinka syvä-johtamisen mukainen esimiesvalmennusprosessi on koettu osallistujien kesken Hankkija-Maatalous Oy:n esimiehille järjestetyssä esimiesvalmennuksessa. Tutkielma on luonteeltaan laadullinen tapaustutkimus. Tutkimusaineisto koostuu yhteensä 10 Hankkija-Maatalous Oy:n ketjuohjauksen esimiehen haastattelusta sekä osuustoimintaa, kohdeorganisaatiota ja syvä-johtamista käsittelevästä kirjallisuudesta. Teemahaastattelut suoritettiin alkukesän 2006 aikana. Tutkimustulokset osoittavat, että syväjohtamisen esimiesvalmennus ei ole pelkästään teoriatasolla toimiva muoti-ilmiö, vaan se antaa konkreettisia työkaluja käytännön esimiestyötä tekeville esimiehille. Osuus-toiminnallinen yritys antaa myös hyvän pohjan pitkäjänteiseen esimiesten ihmistenjohtamisen kehittämiseen.

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Tämän tutkimuksen tarkoituksena on ymmärtää yritystä oppivana organisaationa ja selvittää onko Syväjohtamisen valmennusmalli ja työkalu Peik-ko Finland Oy:lle organisaation ja yksilön oppimista tukevaa. Tutkimus on laadullinen tutkimus, jossa tutkimusaineiston muodostavat Peikko Finland Oy:n johdon ja esimiestehtävissä olevien henkilöiden teemahaastattelut. Tutkimuksen perusteella voidaan todeta, että Syväjohtamisen valmen-nusmalli on yrityksen ja yksilön oppimisen kannalta toimiva työkalu, joka ulkoisen valmennuksen jälkeen tulisi ylläpitää sisäisellä toimintamallilla. Oleellista on ulkoisen valmennuksen jatkamisen yhteydessä lisätä etukäteisinfon osuutta ennen valmennuksen alkamista. Peikko Finland Oy:ssä organisaation ja yksilön oma oppiminen edellyttää yritykseltä oppimista tukevien työkalujen ja yrityksen sisäisen toimintamallin toteuttamista, jonka avulla mahdollisestaan koko organisaation oppiminen ja yhteisten tavoitteiden ymmärtäminen.

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In the last five years deep cracks have appeared in the European project. The 'euro-area crisis' triggered by a severe global financial and economic crisis has put European integration to a major test, more profound than ever before. The experience of recent years has revealed and exacerbated significant deficiencies in the European Union's (EU) economic and political construction. At time it has cast doubt on fundamentals of the European project and raised questions about whether Europe will be able to deal effectively not only with the immediate crisis, but also with the many other serious socio-economic, politico-institutional, societal and global challenges that Europe is and will be confronted with. At the start of a new institutional-political cycle (2014-2019) and while the crisis situation has for a number of reasons improved significantly since the summer of 2012, at least in systemic terms, the Union's new leadership and Member States will now have to take strategic decisions about the future of European integration.

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The authors would like to thank the leadership of the Deep Ocean Stewardship Initiative (DOSI), including Lisa Levin, Maria Baker, and Kristina Gjerde, for their support in developing this review. This work evolved from a meeting of the DOSI Oil and Gas working group supported by the J.M. Kaplan Fund, and associated with the Deep-Sea Biology Symposium in Aveiro, Portugal in September 2015. The members of the Oil and Gas working group that contributed to our discussions at that meeting or through the listserve are acknowledged for their contributions to this work. We would also like to thank the three reviewers and the editor who provided valuable comments and insight into the work presented here. DJ and AD were supported by funding from the European Union's Horizon 2020 research and innovation programme under the MERCES (Marine Ecosystem Restoration in Changing European Seas) project, grant agreement No 689518. AB was supported by CNPq grants 301412/2013-8 and 200504/2015-0. LH acknowledges funding provided by a Natural Environment Research Council grant (NE/L008181/1). This output reflects only the authors' views and the funders cannot be held responsible for any use that may be made of the information contained therein.

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Universidade Estadual de Campinas . Faculdade de Educação Física

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The sustainability of intensive swine production demands alternative destinations for the generated residues. Ashes from swine rice husk-based deep bedding were tested as a mineral addition for cement mortars. The ashes were obtained at 400 to 600ºC, ground and sieved through a 325 mesh sieve (# 0.045 mm). The characterization of the ashes included the determination of the index of pozzolanic activity with lime. The ashes were also tested as partial substitutes of Portland cement. The mortars were prepared using a cement:sand proportion of 1:1.5, and with water/cement ratio of 0.4. Three percentages of mass substitution of the cement were tested: 10, 20 and 30%. Mortar performances were assessed at 7 and 28 days determining their compressive strength. The chosen condition for calcinations at the laboratory scale was related to the maximum temperature of 600ºC since the resulting ashes contained vitreous materials and presented satisfactory values for the pozzolanic index under analysis. The pozzolanic activity indicated promising results for ashes produced at 600ºC as a replacement of up to 30% in cement masses.

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Shallow-water tropical reefs and the deep sea represent the two most diverse marine environments. Understanding the origin and diversification of this biodiversity is a major quest in ecology and evolution. The most prominent and well-supported explanation, articulated since the first explorations of the deep sea, holds that benthic marine fauna originated in shallow, onshore environments, and diversified into deeper waters. In contrast, evidence that groups of marine organisms originated in the deep sea is limited, and the possibility that deep-water taxa have contributed to the formation of shallow-water communities remains untested with phylogenetic methods. Here we show that stylasterid corals (Cnidaria: Hydrozoa: Stylasteridae)-the second most diverse group of hard corals-originated and diversified extensively in the deep sea, and subsequently invaded shallow waters. Our phylogenetic results show that deep-water stylasterid corals have invaded the shallow-water tropics three times, with one additional invasion of the shallow-water temperate zone. Our results also show that anti-predatory innovations arose in the deep sea, but were not involved in the shallow-water invasions. These findings are the first robust evidence that an important group of tropical shallow-water marine animals evolved from deep-water ancestors.

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Equatorial podzols are soils characterized by thick sandy horizons overlying more clayey horizons. Organic matter produced in the topsoil is transferred in depth through the sandy horizons and accumulate at the transition, at a depth varying from 1 to more than 3 m, forming deep horizons rich in organic matter (Bh horizons). Although they cover great surfaces in the equatorial zone, these soils are still poorly known. Studying podzols from Amazonia, we found out that the deep Bh horizons in poorly drained podzol areas have a thickness higher than 1m and store unexpected amounts of carbon. The average for the studied area was 66.7 +/- 5.8 kgCm(-2) for the deep Bh and 86.8 +/- 7.1 kgCm(-2) for the whole profile. Extrapolating to the podzol areas of the whole Amazonian basin has been possible thanks to digital maps, giving an order of magnitude around 13.6 +/- 1.1 PgC, at least 12.3 PgC higher than previous estimates. This assessment should be refined by additional investigations, not only in Amazonia but in all equatorial areas where podzols have been identified. Because of the lack of knowledge on the quality and behaviour of the podzol organic matter, the question of the feedback between the climate and the equatorial podzol carbon cycle is open.

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Background: While microRNAs (miRNAs) play important roles in tissue differentiation and in maintaining basal physiology, little is known about the miRNA expression levels in stomach tissue. Alterations in the miRNA profile can lead to cell deregulation, which can induce neoplasia. Methodology/Principal Findings: A small RNA library of stomach tissue was sequenced using high-throughput SOLiD sequencing technology. We obtained 261,274 quality reads with perfect matches to the human miRnome, and 42% of known miRNAs were identified. Digital Gene Expression profiling (DGE) was performed based on read abundance and showed that fifteen miRNAs were highly expressed in gastric tissue. Subsequently, the expression of these miRNAs was validated in 10 healthy individuals by RT-PCR showed a significant correlation of 83.97% (P<0.05). Six miRNAs showed a low variable pattern of expression (miR-29b, miR-29c, miR-19b, miR-31, miR-148a, miR-451) and could be considered part of the expression pattern of the healthy gastric tissue. Conclusions/Significance: This study aimed to validate normal miRNA profiles of human gastric tissue to establish a reference profile for healthy individuals. Determining the regulatory processes acting in the stomach will be important in the fight against gastric cancer, which is the second-leading cause of cancer mortality worldwide.

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Objective: In this study we evaluated the ablation rate of superficial and deep dentin irradiated with different Er:YAG laser energy levels, and observed the micromorphological aspects of the lased substrates with a scanning electron microscope (SEM). Background Data: Little is known about the effect of Er: YAG laser irradiation on different dentin depths. Materials and Methods: Sixty molar crowns were bisected, providing 120 specimens, which were randomly assigned into two groups ( superficial or deep dentin), and later into five subgroups (160, 200, 260, 300, or 360 mJ). Initial masses of the specimens were obtained. After laser irradiation, the final masses were obtained and mass losses were calculated followed by the preparation of specimens for SEM examination. Mass-loss values were subjected to two-way ANOVA and Fisher's least significant difference multiple-comparison tests (p < 0.05). Results: There was no difference between superficial and deep dentin. A significant and gradual increase in the mass-loss values was reached when energies were raised, regardless of the dentin depth. The energy level of 360 mJ showed the highest values and was statistically significantly different from the other energy levels. The SEM images showed that deep dentin was more selectively ablated, especially intertubular dentin, promoting tubule protrusion. At 360 mJ the micromorphological features were similar for both dentin depths. Conclusion: The ablation rate did not depend on the depth of the dentin, and an energy level lower than 360 mJ is recommended to ablate both superficial and deep dentin effectively without causing tissue damage.

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Background: The New World screw-worm (NWS), Cochliomyia hominivorax, is one of the most important myiasis-causing flies, causing severe losses to the livestock industry. In its current geographical distribution, this species has been controlled by the application of insecticides, mainly organophosphate (OP) compounds, but a number of lineages have been identified that are resistant to such chemicals. Despite its economic importance, only limited genetic information is available for the NWS. Here, as a part of an effort to characterize the C. hominivorax genome and identify putative genes involved in insecticide resistance, we sampled its transcriptome by deep sequencing of polyadenylated transcripts using the 454 sequencing technology. Results: Deep sequencing on the 454 platform of three normalized libraries (larval, adult male and adult female) generated a total of 548,940 reads. Eighteen candidate genes coding for three metabolic detoxification enzyme families, cytochrome P450 monooxygenases, glutathione S transferases and carboxyl/cholinesterases were selected and gene expression levels were measured using quantitative real-time polymerase chain reaction (qRT-PCR). Of the investigated candidates, only one gene was expressed differently between control and resistant larvae with, at least, a 10-fold down-regulation in the resistant larvae. The presence of mutations in the acetylcholinesterase (target site) and carboxylesterase E3 genes was investigated and all of the resistant flies presented E3 mutations previously associated with insecticide resistance. Conclusions: Here, we provided the largest database of NWS expressed sequence tags that is an important resource, not only for further studies on the molecular basis of the OP resistance in NWS fly, but also for functional and comparative studies among Calliphoridae flies. Among our candidates, only one gene was found differentially expressed in resistant individuals, and its role on insecticide resistance should be further investigated. Furthermore, the absence of mutations in the OP target site and the high frequency of mutant carboxylesterase E3 indicate that metabolic resistance mechanisms have evolved predominantly in this species.

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In-situ measurements in convective clouds (up to the freezing level) over the Amazon basin show that smoke from deforestation fires prevents clouds from precipitating until they acquire a vertical development of at least 4 km, compared to only 1-2 km in clean clouds. The average cloud depth required for the onset of warm rain increased by similar to 350 m for each additional 100 cloud condensation nuclei per cm(3) at a super-saturation of 0.5% (CCN0.5%). In polluted clouds, the diameter of modal liquid water content grows much slower with cloud depth (at least by a factor of similar to 2), due to the large number of droplets that compete for available water and to the suppressed coalescence processes. Contrary to what other studies have suggested, we did not observe this effect to reach saturation at 3000 or more accumulation mode particles per cm(3). The CCN0.5% concentration was found to be a very good predictor for the cloud depth required for the onset of warm precipitation and other microphysical factors, leaving only a secondary role for the updraft velocities in determining the cloud drop size distributions. The effective radius of the cloud droplets (r(e)) was found to be a quite robust parameter for a given environment and cloud depth, showing only a small effect of partial droplet evaporation from the cloud's mixing with its drier environment. This supports one of the basic assumptions of satellite analysis of cloud microphysical processes: the ability to look at different cloud top heights in the same region and regard their r(e) as if they had been measured inside one well developed cloud. The dependence of r(e) on the adiabatic fraction decreased higher in the clouds, especially for cleaner conditions, and disappeared at r(e)>=similar to 10 mu m. We propose that droplet coalescence, which is at its peak when warm rain is formed in the cloud at r(e)=similar to 10 mu m, continues to be significant during the cloud's mixing with the entrained air, cancelling out the decrease in r(e) due to evaporation.

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Heavy quark production has been very well studied over the last years both theoretically and experimentally. Theory has been used to study heavy quark production in ep collisions at HERA, in pp collisions at Tevatron and RHIC, in pA and dA collisions at RHIC, and in AA collisions at CERN-SPS and RHIC. However, to the best of our knowledge, heavy quark production in eA has received almost no attention. With the possible construction of a high energy electron-ion collider, updated estimates of heavy quark production are needed. We address the subject from the perspective of saturation physics and compute the heavy quark production cross section with the dipole model. We isolate shadowing and nonlinear effects, showing their impact on the charm structure function and on the transverse momentum spectrum.

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The thick weathering profiles of humid tropical areas are an important, yet generally neglected, source of information on landscape evolution. Six complete profiles of the weathering mantle were sampled by drilling on the three stepped levels of the Campos do Jordao Plateau, on the NW flank of the Continental Rift of Southeastern Brazil. Mineralogical and micromorphological analyses of drill core samples, complemented by geochemical interpretations and by previous data on the upper saprolite, indicate continuity of a general lateritic trend during the entire process of mantle formation. Lateritization phases of different intensity were defined and considered to reflect adjustment to changes in environmental conditions created by the gradual uplift of the plateau to its present position. Older and more superficial materials related to intense lateritic weathering are characterized by allitization with direct formation of gibbsite from silicates, probably related to tropical climates existing immediately before the formation of the continental rift, during the Paleogene, and also before any significant increase in altitude. Monosialitization phase with general kaolinitization and restricted indirect formation of gibbsite from silicates could be associated to less aggressive climates that followed the Neogene (Miocene?) accentuation of uplift rates along the continental rift. The changes produced by uplift in the tropical climate eventually favored the development of a podzolization trend in soils above 1800m. (C) 2011 Elsevier BM. All rights reserved.