Casa Caldesi. Un'ipotesi di restauro per il complesso architettonico faentino

Il Palazzo è un'architettura ben presente nell’immaginario collettivo soprattutto per il fatto che sia comunemente indicato come l’antica dimora dei Manfredi, signori della città. Tanto importante da sollevare sulla stampa locale periodiche ondate di indignazione per il suo stato di abbandono. Il recente studio di Lucio Donati dimostra come gli antichi proprietari fossero in realtà i Bazolini prima e i Viarani poi. A conclusione dell’articolo proponeva quindi di chiamare il fabbricato secondo il nome dei reali proprietari. In questa tesi ho deciso invece di chiamare il fabbricato con il nome di Casa Caldesi. Il precario stato di conservazione indica l’urgenza di un pronto intervento di restauro. Questa tesi propone una delle possibili ipotesi di progetto. Visto lo stato delle cose ho scelto un progetto di restauro che prevedesse una funzione mista residenziale e ad uffici. Mantenendo lungo via Manfredi le vetrine e quindi la funzione commerciale al dettaglio negli spazi che già una volta ospitavano i negozi. Il progetto si è soffermato in particolare nel disegno delle residenze. L’obiettivo di ripristinare i grandi ambienti decorati è stato rispettato attraverso un paziente lavoro di distribuzione capace di conservare e valorizzare la bellezza dei locali, senza perdere i requisiti di funzionalità e comodità adeguati alle moderne residenze. Questa scelta funzionale anche se può sembrare scontata e compatibile con un palazzo che da sempre è stata una residenza, presenta tuttavia alcune problematiche. L’ipotesi di restauro quindi si pone il problema di organizzare gli spazi del palazzo in appartamenti ed uffici, ripristinare la spazialità di tutti i grandi ambienti decorati e renderli compatibili con le esigenze abitative odierne.

Ina-casa la fiorita. Strategie di rigenerazione urbana per un riuso condiviso.

Gran parte del patrimonio edilizio italiano è costituito da un'edilizia minore realizzata per lo più negli anni successivi al secondo dopoguerra. Una delle più significative esperienze di ricostruzione è rappresentata dai quartieri Ina-Casa, che oltre a rispondere all'elevata richiesta abitativa, hanno contribuito a dare una forma all'espansione disorganizzata delle città e si sono rivelati l'ultima vera occasione per gli architetti di essere protagonisti della storia nazionale. Tuttavia, ad oggi, manca la consapevolezza diffusa del grande valore storico, identitario e patrimoniale di queste porzioni di città e della necessità di un congruo intervento di valorizzazione e riqualificazione. Specialmente nelle piccole realtà, come Cesena, questo ha comportato una forte alterazione dei caratteri originari secondo scelte arbitrarie ed interventi disomogenei. A seguito dell'analisi approfondita della piccola unità di vicinato della Fiorita, si è deciso di adottare un approccio metodologico diversificato tra aspetti urbanistici e relativi al singolo alloggio. Da una parte è stato elaborato un progetto urbanistico che tenesse conto di tutte le specificità del luogo, in particolare della presenza di una popolazione residente molto attiva e determinata nella valorizzazione del proprio quartiere. Dall'altra è stato redatto un manuale di possibili interventi, pensati per rispondere alle attuali esigenze estetiche, prestazionali e funzionali dell'alloggio, corredato da un sistema incentivante a punteggio. Nell'insieme questa esperienza evidenzia le potenzialità di un progetto di rigenerazione urbana che può essere sperimentato anche in altri contesti della città.

Abandoned Coal Mine Drainage and Its Remediation: Impacts on Stream Ecosystem Structure and Function

The effects of abandoned mine drainage (AMD) on streams and responses to remediation efforts were studied using three streams (AMD-impacted, remediated, reference) in both the anthracite and the bituminous coal mining regions of Pennsylvania (USA). Response variables included ecosystem function as well as water chemistry and macroinvertebrate community composition. The bituminous AMD stream was extremely acidic with high dissolved metals concentrations, a prolific mid-summer growth of the filamentous alga, Mougeotia, and .10-fold more chlorophyll than the reference stream. The anthracite AMD stream had a higher pH, substrata coated with iron hydroxide(s), and negligible chlorophyll. Macroinvertebrate communities in the AMD streams were different from the reference streams, the remediated streams, and each other. Relative to the reference stream, the AMD stream(s) had (1) greater gross primary productivity (GPP) in the bituminous region and undetectable GPP in the anthracite region, (2) greater ecosystem respiration in both regions, (3) greatly reduced ammonium uptake and nitrification in both regions, (4) lower nitrate uptake in the bituminous (but not the anthracite) region, (5) more rapid phosphorus removal from the water column in both regions, (6) activities of phosphorus-acquiring, nitrogenacquiring, and hydrolytic-carbon-acquiring enzymes that indicated extreme phosphorus limitation in both regions, and (7) slower oak and maple leaf decomposition in the bituminous region and slower oak decomposition in the anthracite region. Remediation brought chlorophyll concentrations and GPP nearer to values for respective reference streams, depressed ecosystem respiration, restored ammonium uptake, and partially restored nitrification in the bituminous (but not the anthracite) region, reduced nitrate uptake to an undetectable level, restored phosphorus uptake to near normal rates, and brought enzyme activities more in line with the reference stream in the bituminous (but not the anthracite) region. Denitrification was not detected in any stream. Water chemistry and macroinvertebrate community structure analyses capture the impact of AMD at the local reach scale, but functional measures revealed that AMD has ramifications that can cascade to downstream reaches and perhaps to receiving estuaries.

Hardystonite From the Desert View Mine, California

The fluorescent mineral hardystonite is confirmed in a specimen from the Desert View Mine, California. Hardystonite had been known only from Franklin, New Jersey for over 100 years.

Impact of copper mine tailings (stamp sand) on survival and development of aquatic organisms near Gay, Michigan

Heavy metal-rich copper mine tailings, called stamp sands, were dumped by mining companies directly into streams and along the Lake Superior shoreline, degrading Keweenaw Peninsula waterways. One of the largest disposal sites is near Gay, Michigan, where tailings have been moved along the shoreline by currents since mining ceased. As a result, the smallest sand particles have been washed into deeper water and are filling the interstitial spaces of Buffalo Reef, a critical lake trout spawning site. This research is the first to investigate if stamp sand is detrimental to survival and early development of eggs and larvae of lake sturgeon, lake trout, and Northern leopard frogs, and also examines if the presence of stamp sands influences substrate selection of earthworms. This study found that stamp sand had significantly larger mean particle sizes and irregular shapes compared to natural sand, and earthworms show a strong preference for natural substrate over any combination that included stamp sand. Additionally, copper analysis (Cu2+) of surface water over stamp sand and natural sand showed concentrations were significantly higher in stamp sand surface water (100 μg/L) compared to natural sand surface water (10 μg/L). Frog embryos had similar hatch success over both types of sand, but tadpoles reared over natural sand grew faster and had higher survival rates. Eggs of lake sturgeon showed similar hatch success and development over natural vs. stamp sand over 17 days, while lake trout eggs hatched earlier and developed faster when incubated over stamp sand, yet showed similar development over a 163 day period. Copper from stamp sand appears to impact amphibians more than fish species in this study. These results will help determine what impact stamp sand has on organisms found throughout the Keweenaw Peninsula which encounter the material at some point in their life history.

Economic sustainability of the Flambeau Mine Ladysmith, Wisconsin

Today sustainable development is a very pertinent issue. Communities do not want companies, specifically mining companies, to deplete a natural resource and leave. The goal is to minimize the negative impacts of mining and the boom/bust cycles of natural resource extraction. In this study a three part framework was developed to analyze the sustainability of the Flambeau Mine in Ladysmith, Wisconsin. The first and second part dealt with an in-depth local and regional analysis and whether the community was developing within its own vision. The third part used nine sustainability measures including: 1. Need Present Generation 2. Future Need 3. Acceptable Legacy 4. Full-Cost 5. Contribution to Economic Development 6. Equity 7. Consent 8. Respect for Ecological Limits, Maintenance of Ecological Integrity and Landscape Requirements 9. Offsetting Restoration This study concluded that the Flambeau Mine was sustainable relative to the first two criteria and that it can be considered mostly sustainable relative to the nine criteria. Overall it can be stated that the Flambeau Mine was a beneficial project to the Ladysmith Wisconsin area. Additionally it appeared to decrease the public’s negative perception of mining. Recommendations for future analytical work are made. Suggestions are made as to how mining companies could increase the potential for the attainment of sustainability in projects. It is recommended that this framework be used by other industries.

Paleomagnetic Study of the Portage Lake Volcanics exposed in the Quincy Mine

A detailed paleomagnetic and rock-magnetic investigation was conducted on thirty six basaltic flows of the ~1095 Ma Portage Lake Volcanics. The flows were sampled along the East Adit of the Quincy Mine (Hancock, MI). Thirty two flows yielded well-defined primary magnetization directions carried by magnetite. A secondary magnetization component carried by hematite was also found in twenty nine flows. After correction for serial correlation between the flows, nineteen independent mean directions were calculated. The corresponding paleomagnetic pole is located at 25.5 °N, 182.1 °W (A95 = 3.5°). The new pole overlaps with the pole from the ~1087 Ma Lake Shore Traps suggesting a standstill of the North American plate during that time period. The low angular dispersion of virtual geomagnetic poles (S = 7.9°) suggests that the flows were erupted within a short time period, or that the strength of geomagnetic secular variation was lower than that of the recent field.