Lesestoff

 Kunstbuch
Andreas Erber „Buchstabenbildersalat“
ISBN 978-3-00-067698-7, Hardcover, Fadenbindung, 88 Doppelseiten, 2021. Gibt es bei Ebay.
Eine Melange aus Bilder und Texten, Minidialogen, und Gedichten. Zum Hingucken und nachdenken.

 

(c) Andreas ErberErzählungen
Andreas Erber „Von 84 Arten ins Gras zu beißen“
ISBN 978-3-7368-7386-5, Taschenbuch, 2015. Gibt es bei Ebay.
84 Kurzgeschichten über den Tod, das Sterben, das Loslassen und Abschiednehmen. Mal kurios, mal lustig, mal böse, mal traurig.

 

 

(c) Andreas ErberHistorische Schrift
Andreas Erber „Graf Montgelas und das Gut Großhesselohe“
ISBN 978-3-00-070806-0, Taschenbuch, 104 Seiten, 2017. Gibt es bei Ebay.

Wer hätte das gedacht? Das Gut Großhesselohe im Süden Münchens war bis zum Ende des 19. Jahrhunderts der Vergnügungsort für die bayerischen Hauptstädter schlechthin und stand dem heutigen Oktoberfest in kaum etwas nach. Die Schrift gibt einen spannenden Abriss über die Geschichte des Guts von seinen Anfängen im Mittelalter bis zu seinem so bedeutenden Eigentümer, Maximilian Joseph Graf von Montgelas, Staatsminister und Architekt des modernen Bayerns im frühen 19. Jahrhundert.

 

Kunstbuch
Andreas Erber „Bilder zum Sprechen bringen“
ISBN 978-3-00-063418-5, Hardcover, 88 Doppelseiten, 2019. Ausverkauft.
Im Buch finden Texte und Bilder zusammen. Chaotisch, inspirierend, pointiert, nachdenklich, poetisch. Wunderbar zum Innehalten und zum Staunen und Entdecken. Auch für alle, die selbst nicht schreiben oder malen.

 

235 Gedanken zu „Lesestoff

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    אין עשן כבד או ריח עז שעלול להטריד – רק אידוי עדין ופשוט שנותן חופש פעולה גם במקום ציבורי.

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    תכונה זו מאפשרת לכוונן את השימוש להמוצר – פרחים, שמנים או תרכיזים – ולבחירת המשתמש.

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  • Jan Beutel was half-watching a live stream of Kleines Nesthorn, a mountain peak in the Swiss Alps, when he realized its cacophony of creaks and rumbles was getting louder. He dropped his work, turned up the sound and found himself unable to look away.
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    “The whole screen exploded,” he said.

    Beutel, a computer engineer specializing in mountain monitoring, had just witnessed a glacier collapse. On May 28, an avalanche of millions of tons of ice and rock barreled down the slope, burying Blatten, a centuries-old village nestled in the valley below.

    Local authorities had already evacuated the village after parts of the mountain had crumbled onto the glacier; a 64-year old man believed to have stayed remains missing.

    But no one expected an event of this magnitude.

    Successive rock avalanches onto the glacier increased the pressure on the ice, causing it to melt faster and the glacier to accelerate, eventually destabilizing it and pushing it from its bed. The collapse was sudden, violent and catastrophic. “This one just left no moment to catch a breath,” Beutel said.
    The underlying causes will take time to unravel. A collapse of this magnitude would have been set in motion by geological factors going back decades at least, said Matthias Huss, a glaciologist at the Swiss university ETH Zurich.

    But it’s “likely climate change is involved,” he said, as warming temperatures melt the ice that holds mountains together. It’s a problem affecting mountains across the planet.

    People have long been fascinated with mountains for their dramatic beauty. Some make their homes beneath them — around 1 billion live in mountain communities — others are drawn by adventure, the challenge of conquering peaks.

    These majestic landscapes have always been dangerous, but as the world warms, they are becoming much more unpredictable and much deadlier.

    “We do not fully understand the hazard at the moment, nor how the dangers are changing with climate change,” said David Petley, an Earth scientist at the University of Hull in England.

  • Jan Beutel was half-watching a live stream of Kleines Nesthorn, a mountain peak in the Swiss Alps, when he realized its cacophony of creaks and rumbles was getting louder. He dropped his work, turned up the sound and found himself unable to look away.
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    “The whole screen exploded,” he said.

    Beutel, a computer engineer specializing in mountain monitoring, had just witnessed a glacier collapse. On May 28, an avalanche of millions of tons of ice and rock barreled down the slope, burying Blatten, a centuries-old village nestled in the valley below.

    Local authorities had already evacuated the village after parts of the mountain had crumbled onto the glacier; a 64-year old man believed to have stayed remains missing.

    But no one expected an event of this magnitude.

    Successive rock avalanches onto the glacier increased the pressure on the ice, causing it to melt faster and the glacier to accelerate, eventually destabilizing it and pushing it from its bed. The collapse was sudden, violent and catastrophic. “This one just left no moment to catch a breath,” Beutel said.
    The underlying causes will take time to unravel. A collapse of this magnitude would have been set in motion by geological factors going back decades at least, said Matthias Huss, a glaciologist at the Swiss university ETH Zurich.

    But it’s “likely climate change is involved,” he said, as warming temperatures melt the ice that holds mountains together. It’s a problem affecting mountains across the planet.

    People have long been fascinated with mountains for their dramatic beauty. Some make their homes beneath them — around 1 billion live in mountain communities — others are drawn by adventure, the challenge of conquering peaks.

    These majestic landscapes have always been dangerous, but as the world warms, they are becoming much more unpredictable and much deadlier.

    “We do not fully understand the hazard at the moment, nor how the dangers are changing with climate change,” said David Petley, an Earth scientist at the University of Hull in England.

  • Jan Beutel was half-watching a live stream of Kleines Nesthorn, a mountain peak in the Swiss Alps, when he realized its cacophony of creaks and rumbles was getting louder. He dropped his work, turned up the sound and found himself unable to look away.
    кракен ссылка
    “The whole screen exploded,” he said.

    Beutel, a computer engineer specializing in mountain monitoring, had just witnessed a glacier collapse. On May 28, an avalanche of millions of tons of ice and rock barreled down the slope, burying Blatten, a centuries-old village nestled in the valley below.

    Local authorities had already evacuated the village after parts of the mountain had crumbled onto the glacier; a 64-year old man believed to have stayed remains missing.

    But no one expected an event of this magnitude.

    Successive rock avalanches onto the glacier increased the pressure on the ice, causing it to melt faster and the glacier to accelerate, eventually destabilizing it and pushing it from its bed. The collapse was sudden, violent and catastrophic. “This one just left no moment to catch a breath,” Beutel said.
    The underlying causes will take time to unravel. A collapse of this magnitude would have been set in motion by geological factors going back decades at least, said Matthias Huss, a glaciologist at the Swiss university ETH Zurich.

    But it’s “likely climate change is involved,” he said, as warming temperatures melt the ice that holds mountains together. It’s a problem affecting mountains across the planet.

    People have long been fascinated with mountains for their dramatic beauty. Some make their homes beneath them — around 1 billion live in mountain communities — others are drawn by adventure, the challenge of conquering peaks.

    These majestic landscapes have always been dangerous, but as the world warms, they are becoming much more unpredictable and much deadlier.

    “We do not fully understand the hazard at the moment, nor how the dangers are changing with climate change,” said David Petley, an Earth scientist at the University of Hull in England.

  • Jan Beutel was half-watching a live stream of Kleines Nesthorn, a mountain peak in the Swiss Alps, when he realized its cacophony of creaks and rumbles was getting louder. He dropped his work, turned up the sound and found himself unable to look away.
    kraken darknet
    “The whole screen exploded,” he said.

    Beutel, a computer engineer specializing in mountain monitoring, had just witnessed a glacier collapse. On May 28, an avalanche of millions of tons of ice and rock barreled down the slope, burying Blatten, a centuries-old village nestled in the valley below.

    Local authorities had already evacuated the village after parts of the mountain had crumbled onto the glacier; a 64-year old man believed to have stayed remains missing.

    But no one expected an event of this magnitude.

    Successive rock avalanches onto the glacier increased the pressure on the ice, causing it to melt faster and the glacier to accelerate, eventually destabilizing it and pushing it from its bed. The collapse was sudden, violent and catastrophic. “This one just left no moment to catch a breath,” Beutel said.
    The underlying causes will take time to unravel. A collapse of this magnitude would have been set in motion by geological factors going back decades at least, said Matthias Huss, a glaciologist at the Swiss university ETH Zurich.

    But it’s “likely climate change is involved,” he said, as warming temperatures melt the ice that holds mountains together. It’s a problem affecting mountains across the planet.

    People have long been fascinated with mountains for their dramatic beauty. Some make their homes beneath them — around 1 billion live in mountain communities — others are drawn by adventure, the challenge of conquering peaks.

    These majestic landscapes have always been dangerous, but as the world warms, they are becoming much more unpredictable and much deadlier.

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    Автоматические мойки бывают различных типов: полностью автоматические станции, портальные системы, роботизированные установки и мойки самообслуживания. Они отличаются по стоимости, скорости и уровню автоматизации. Например, автоматическая бесконтактная автомойка — это быстрая и бесконтактная станция, подходящая для больших потоков клиентов, а робот мойка — более технологичное решение с возможностью мойки грузовиков и автомобилей премиум-класса.

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    The amount of groundwater that has been pumped out of the Colorado River Basin since 2003 is enough to fill Lake Mead, researchers report in a study published earlier this week. Most of that water was used to irrigate fields of alfalfa and vegetables grown in the desert Southwest.

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    “We’re using it faster and faster,” said Jay Famiglietti, an Arizona State University professor and the study’s senior author.

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    The Arizona State University research team measured more than two decades of NASA satellite observations and used land modeling to trace how groundwater tables in the Colorado River basin were dwindling. The team focused mostly on Arizona, a state that is particularly vulnerable to future cutbacks on the Colorado River.
    Groundwater makes up about 35% of the total water supply for Arizona, said Sarah Porter, director of the Kyl Center for Water Policy at Arizona State University, who was not directly involved in the study.

    The study found groundwater tables in the Lower Colorado River basin, and Arizona in particular, have declined significantly in the last decade. The problem is especially pronounced in Arizona’s rural areas, many of which don’t have groundwater regulations, and little backup supply from rivers. With wells in rural Arizona increasingly running dry, farmers and homeowners now drill thousands of feet into the ground to access water.

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  • Deep below the surface of the ground in one of the driest parts of the country, there is a looming problem: The water is running out — but not the kind that fills lakes, streams and reservoirs.
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    The amount of groundwater that has been pumped out of the Colorado River Basin since 2003 is enough to fill Lake Mead, researchers report in a study published earlier this week. Most of that water was used to irrigate fields of alfalfa and vegetables grown in the desert Southwest.

    No one knows exactly how much is left, but the study, published in the journal Geophysical Research Letters, shows an alarming rate of withdrawal of a vital water source for a region that could also see its supply of Colorado River water shrink.

    “We’re using it faster and faster,” said Jay Famiglietti, an Arizona State University professor and the study’s senior author.

    In the past two decades, groundwater basins – or large, underground aquifers – lost more than twice the amount of water that was taken out of major surface reservoirs, Famiglietti’s team found, like Mead and Lake Powell, which themselves have seen water levels crash.

    The Arizona State University research team measured more than two decades of NASA satellite observations and used land modeling to trace how groundwater tables in the Colorado River basin were dwindling. The team focused mostly on Arizona, a state that is particularly vulnerable to future cutbacks on the Colorado River.
    Groundwater makes up about 35% of the total water supply for Arizona, said Sarah Porter, director of the Kyl Center for Water Policy at Arizona State University, who was not directly involved in the study.

    The study found groundwater tables in the Lower Colorado River basin, and Arizona in particular, have declined significantly in the last decade. The problem is especially pronounced in Arizona’s rural areas, many of which don’t have groundwater regulations, and little backup supply from rivers. With wells in rural Arizona increasingly running dry, farmers and homeowners now drill thousands of feet into the ground to access water.

    Scientists don’t know exactly how much groundwater is left in Arizona, Famiglietti added, but the signs are troubling.

    “We have seen dry stream beds for decades,” he said. “That’s an indication that the connection between groundwater and rivers has been lost.”

  • Deep below the surface of the ground in one of the driest parts of the country, there is a looming problem: The water is running out — but not the kind that fills lakes, streams and reservoirs.
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    The amount of groundwater that has been pumped out of the Colorado River Basin since 2003 is enough to fill Lake Mead, researchers report in a study published earlier this week. Most of that water was used to irrigate fields of alfalfa and vegetables grown in the desert Southwest.

    No one knows exactly how much is left, but the study, published in the journal Geophysical Research Letters, shows an alarming rate of withdrawal of a vital water source for a region that could also see its supply of Colorado River water shrink.

    “We’re using it faster and faster,” said Jay Famiglietti, an Arizona State University professor and the study’s senior author.

    In the past two decades, groundwater basins – or large, underground aquifers – lost more than twice the amount of water that was taken out of major surface reservoirs, Famiglietti’s team found, like Mead and Lake Powell, which themselves have seen water levels crash.

    The Arizona State University research team measured more than two decades of NASA satellite observations and used land modeling to trace how groundwater tables in the Colorado River basin were dwindling. The team focused mostly on Arizona, a state that is particularly vulnerable to future cutbacks on the Colorado River.
    Groundwater makes up about 35% of the total water supply for Arizona, said Sarah Porter, director of the Kyl Center for Water Policy at Arizona State University, who was not directly involved in the study.

    The study found groundwater tables in the Lower Colorado River basin, and Arizona in particular, have declined significantly in the last decade. The problem is especially pronounced in Arizona’s rural areas, many of which don’t have groundwater regulations, and little backup supply from rivers. With wells in rural Arizona increasingly running dry, farmers and homeowners now drill thousands of feet into the ground to access water.

    Scientists don’t know exactly how much groundwater is left in Arizona, Famiglietti added, but the signs are troubling.

    “We have seen dry stream beds for decades,” he said. “That’s an indication that the connection between groundwater and rivers has been lost.”

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    Оптимальная длина вольфрамового стержня составляет от 2 до 3 дюймов. Это позволяет достичь необходимой устойчивости дуги и хорошей концентрации тепла. Использование более короткого элемента может привести к нестабильной подаче тока, а слишком длинный будет затруднять контроль за процессом.
    Для меди рекомендуем выбрать пробойник диаметром 1,6 мм. Этот параметр обеспечивает надёжный контакт с поверхностью, предотвращает перегрев и минимизирует вероятность гидрирования. При этом важно учитывать, что использование таких электрических компонентов, как рутиловые или целлюлозные, может также повлиять на выбор подходящего размера, так как их характеристики могут не совпадать с медными сплавами.
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    Как выбрать оптимальную длину электрода для различных толщин меди
    Для меди толщиной до 3 мм рекомендуется использовать стержни длиной 1-2 см. Эта длина обеспечивает необходимую стабильность дуги и предотвращает перегрев. Для меди в диапазоне от 3 до 6 мм подойдут электроды длиной 2-3 см, что позволяет создать эффективную цепь при сварке и снизить риск образования пор и дефектов.
    При работе с материалами толщиной от 6 до 8 мм стоит выбирать длину 3-4 см. Это обеспечит хорошую доступность к шву и правильное распределение тепла. Для меди от 8 до 12 мм оптимальный вариант – 4-5 см. Эта длина позволяет достичь глубокой пропайки, что критично для обеспечения прочности соединения.
    При толщине свыше 12 мм рекомендуется использовать электроды длиной 5-6 см. Это поможет справиться с большими объемами металла и обеспечит надежное соединение без перегрева электрода. Учитывайте, что для точных работ по сварке небольших компонентов идеальна длина в 1-3 см, что обеспечит высокий контроль процесса.
    Кроме длины, важно учитывать и диаметр стержня. Более толстые электроды требуют большего прогрева, поэтому выбирайте их в соответствии с размерами соединяемых деталей. Экспериментируйте с вариантами, чтобы достичь наилучших результатов. Непосредственно перед процессом не забудьте протестировать параметры сварки на образцах, чтобы убедиться в их эффективности.
    Влияние длины вольфрамового электрода на качество сварного шва
    При выборе оптимальной длины вольфрамового изделия стоит ориентироваться на следующие параметры. Для достижения стабильного дугового процесса рекомендуется использовать длину 3-4 мм. Это позволит обеспечить хорошее формирование дуги и минимизировать вероятность залипания на поверхности, что существенно улучшит качество соединения.
    При увеличении длины выше 4-5 мм может наблюдаться нестабильность и увеличение диаметра дуги. Как следствие, это порождает трудности с контролем температуры и влияет на глубину проплавления. В таких случаях шов может обладать недостаточной прочностью и прочными дефектами.
    Для работы с тонкими изделиями целесообразно применять длину в пределах 2-3 мм. В данной ситуации это помогает избежать перегрева основного материала и уменьшает риск возникновения деформаций. Такой подход позволяет добиться более тонкого и аккуратного шва, подходящего для ответственных элементов конструкции.
    Не исключено, что специфика металла тоже играет свою роль. При работе с медью рекомендуется использовать электроды с небольшой длиной, что помогает достичь качественного проплавления благодаря высокой теплопроводности материала. Для более толстых плит может потребоваться увеличение длины для адекватного проникновения.
    Проведение тестов с разными размерами не повредит: эксперименты помогут найти оптимальные параметры для конкретных условий. На практике важно учитывать не только длину, но и диаметр, а также тип используемого оборудования. Все эти факторы в совокупности влияют на конечный результат и качество выполненной работы.

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