{
  "text": "大家好,今天我們要介紹地貌的改變與平衡。\n從地球誕生開始到現在為止,地球的地貌一直在改變。\n而改變地貌的四個主要作用力就是風化、侵蝕、搬運與沉積。\n首先我們先來介紹風化。\n風化的意義就是指,岩石受到空氣、水、生物等環境因素影響,\n漸漸破碎、疏鬆及改變成分的過程。\n簡單的說就是岩石從大到小的過程。\n像岩石中的鐵,會與空氣或水中的氧發生化學反應,生成氧化鐵。\n岩石就會變得鬆軟易碎。\n有時,我們會在河川地上找到一些碎裂的石頭。\n大部分的原因是因為長期的日光曝曬,導致石頭無法承受熱脹冷縮而破裂。\n像這邊的兩張照片,分別是由植物的根與螞蟻在地表上造成不同的變化。\n像人類為了建設而開採大量的水泥,導致山林被破壞。\n以人類的角度來看,其實也是風化的一種。\n接下來我們討論侵蝕。\n首先我們看一段影片。\n影片中我們看到這個人,用噴槍將鐵桶上的鏽除掉。\n這個噴槍噴出來的,其實是含有細砂的高壓空氣。\n這些細砂因為高壓空氣的關係,高速撞擊到鐵鏽,使鐵鏽離開鐵桶。\n這其實就是侵蝕的原理。\n簡單的來說,就是流動的空氣或是水,帶動其中細微的顆粒,撞擊到目標物之後,使得目標物表面受損。\n這就是侵蝕。台灣由於地勢陡峭,許多河流流速特別快,侵蝕的能力也特別強。\n例如泰魯閣的峽谷地形就是這樣造成的。\n這裡我們分析一下河川侵蝕的原理。\n河流流動的時候,靠近岸的兩側,流速會較慢。\n中間的流速則是最快的。\n流速大的時候,可以帶動較大的岩石,也就具有較大的侵蝕力。\n從河床的剖面來說,河中央的侵蝕力較強,容易向下切割。\n河的兩側則沒有這樣的能力,所以最終會造成河谷,會以V形的方式呈現。\n相較於河川,冰川的侵蝕則有很大的不一樣。\n主要的原因,是因為冰川的中間,冰塊都是固體。\n而這些冰塊中間夾長了許多大大小小的岩石。\n整個冰川的流動,就是整個岩塊,跟著冰塊一起移動。\n這些冰塊跟岩塊會在地表產生均勻的侵蝕效果。\n所以大部分冰河侵蝕的現象,都會呈現U形的。\n以下這張照片就是澳洲典型的冰河遺跡。\nU形的曲面非常的明顯。\n有些岩石位於岩面上,長期接受風所帶來細小微粒的撞擊。\n使得岩石慢慢的形成細微的碎裂。\n然後隨風飄逸。久而久之,這些石頭,在岩面上便會呈現非常光滑的侵蝕面。\n這類的岩石又稱為風蝕石。\n海邊的岩石,長時間受到海浪的衝擊,其中也夾雜著許多的砂石顆粒。\n這樣的衝擊也會形成侵蝕的現象。\n照片上這就是典型的海蝕洞。\n接下來我們先介紹搬運的現象。\n想像一下,桌面上有一堆砂子。\n我們在砂子上吹了一口氣,砂子隨風揚起。\n這個仰起的過程,我們就可以說是砂子被風搬運了。\n當風停下來之後,這些砂子又會慢慢的落下來。\n這就是沉積作用。\n搬運與沉積的作用,我們可以從河床上輕易的辨識。\n較大的石頭需要較大的水流才能搬運。\n因此河川上游的大石頭,在水流量大的時候順流而下。\n當水流量變得比較和緩的時候,大石頭就會先沉積下來。\n比較小的石頭呢,會繼續順流而下。\n當水量變得更和緩的時候,較小的石頭也會開始沉積下來。\n以此類推,到最下游的地方,一般來說都是細微的砂子。\n再從岩石的形狀來判斷,上游的石頭經歷過的碰撞較少。\n所以大部分都呈現岩石破碎的樣子。\n在繼續往下游移動的過程中,岩石經歷的碰撞也越來越多。\n漸漸的石頭會變得比較圓潤、光滑。\n通常在河川的中下游,我們可以看到比較多的鵝卵石。\n從剛剛的敘述,我們知道,水在流動的時候,因為流動時同時夾帶許多岩石顆粒,\n這些會對河床造成侵蝕的現象。\n因此當河川進入大海的時候,高低落差不見了,河流的速度也就沒有了。\n這時所有的河流所帶下的岩石顆粒砂石,都會開始沉降。\n因此我們說,大海是河道的最終侵蝕基準面。\n如果河道中間流經過湖泊,那麼河流的流速也會突然陡降。\n這時候也會發生沉降的現象,因為這是暫時的。\n所以我們就說,湖泊是河道暫時侵蝕基準面。\n如果河道當中有一個凸起,這個凸起呢,會接受到比較多的侵蝕現象。\n所以一段時間之後,這個凸起就會消失。\n整個河道會成為均勻分布的平衡狀態。\n假如河道當中有一座橋,橋墩埋在河床下面。\n這時候下游如果有人大量的開採砂石,\n結果上游河床的石頭就會向開採處移動。\n最終使得河床下陷,橋墩裸露。\n這時橋墩很容易被水流侵蝕,導致橋樑被破壞。\n因此橋樑的上下游都不應該開採砂石以維護橋樑的安全。\n同樣的道理,海岸線的位置是河川上游所帶下來的砂石,\n與海浪沖刷所帶走的砂石平衡的結果。\n如果河川上游大量開採砂石,或是築起水壩,\n使得砂石不再流向海洋,\n那麼河川所帶下來的砂石,\n就會少於海浪沖刷所帶走的砂石,\n最終將使海岸線退縮。\n以上就是地貌的改變與平衡的介紹,\n我們下次再會。\n請問一下,請問一下,\n請問一下,請問一下,\n請問一下,請問一下,\n請問一下,請問一下,\n請問一下,請問一下,\n請問一下,請問一下,\n請問一下,請問一下,\n請問一下,請問一下,\n請問一下,請問一下,\n請問一下,請問一下,\n請問一下,請問一下,請問一下,\n請問一下,請問一下,請問一下,\n請問一下,請問一下,請問一下,\n請問一下,請問一下,請問一下,\n請問一下,請問一下,請問一下,請問一下,\n請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請問一下,請",
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      "text": "大家好,今天我們要介紹地貌的改變與平衡。",
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      "text": "從地球誕生開始到現在為止,地球的地貌一直在改變。",
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      "text": "而改變地貌的四個主要作用力就是風化、侵蝕、搬運與沉積。",
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      "text": "首先我們先來介紹風化。",
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      "text": "風化的意義就是指,岩石受到空氣、水、生物等環境因素影響,",
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    {
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      "seek": 2660,
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      "text": "漸漸破碎、疏鬆及改變成分的過程。",
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      "id": 6,
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      "text": "簡單的說就是岩石從大到小的過程。",
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      "text": "像岩石中的鐵,會與空氣或水中的氧發生化學反應,生成氧化鐵。",
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      "text_original": "像岩石中的鐵,會與空氣或水中的氧其化學反應,生成氧化鐵。",
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      "text": "岩石就會變得鬆軟易碎。",
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      "text": "有時,我們會在河川地上找到一些碎裂的石頭。",
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      "text": "大部分的原因是因為長期的日光曝曬,導致石頭無法承受熱脹冷縮而破裂。",
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    {
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      "text": "像這邊的兩張照片,分別是由植物的根與螞蟻在地表上造成不同的變化。",
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      "text": "像人類為了建設而開採大量的水泥,導致山林被破壞。",
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    {
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      "text": "以人類的角度來看,其實也是風化的一種。",
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      "text_original": "以聚光的角度來看,其實也是風化了一種。",
      "correction_applied": true,
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    {
      "id": 14,
      "seek": 5560,
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      "text": "接下來我們討論侵蝕。",
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      "text_original": "接下來我們討論青石。",
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      "text": "首先我們看一段影片。",
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      "text": "影片中我們看到這個人,用噴槍將鐵桶上的鏽除掉。",
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      "text": "這個噴槍噴出來的,其實是含有細砂的高壓空氣。",
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      "text": "這些細砂因為高壓空氣的關係,高速撞擊到鐵鏽,使鐵鏽離開鐵桶。",
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      "text": "這其實就是侵蝕的原理。",
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      "text": "簡單的來說,就是流動的空氣或是水,帶動其中細微的顆粒,撞擊到目標物之後,使得目標物表面受損。",
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      "text": "這就是侵蝕。台灣由於地勢陡峭,許多河流流速特別快,侵蝕的能力也特別強。",
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      "text_original": "這就是青石。台灣由於地勢陡峭,許多河流流速特別快,青石的能力也特別強。",
      "correction_applied": true,
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      "text": "例如泰魯閣的峽谷地形就是這樣造成的。",
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      "text": "這裡我們分析一下河川侵蝕的原理。",
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      "text_original": "這裡我們分析一下河川青石的原理。",
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      "text": "河流流動的時候,靠近岸的兩側,流速會較慢。",
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      "text": "中間的流速則是最快的。",
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      "text": "流速大的時候,可以帶動較大的岩石,也就具有較大的侵蝕力。",
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      "text": "從河床的剖面來說,河中央的侵蝕力較強,容易向下切割。",
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      "text": "河的兩側則沒有這樣的能力,所以最終會造成河谷,會以V形的方式呈現。",
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      "text": "相較於河川,冰川的侵蝕則有很大的不一樣。",
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      "text": "主要的原因,是因為冰川的中間,冰塊都是固體。",
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      "text": "而這些冰塊中間夾長了許多大大小小的岩石。",
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      "text": "整個冰川的流動,就是整個岩塊,跟著冰塊一起移動。",
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      "text": "這些冰塊跟岩塊會在地表產生均勻的侵蝕效果。",
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      "text_original": "這些冰塊跟岩塊會在地表產生均勻的青石效果。",
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      "text": "所以大部分冰河侵蝕的現象,都會呈現U形的。",
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      "text": "以下這張照片就是澳洲典型的冰河遺跡。",
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      "text": "U形的曲面非常的明顯。",
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      "text": "有些岩石位於岩面上,長期接受風所帶來細小微粒的撞擊。",
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      "text_original": "有些岩石位於銀楓面上,長期接受風所帶來細小微粒的撞擊。",
      "correction_applied": true,
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      "text": "使得岩石慢慢的形成細微的碎裂。",
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    {
      "id": 39,
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      "text": "然後隨風飄逸。久而久之,這些石頭,在岩面上便會呈現非常光滑的侵蝕面。",
      "tokens": [
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      "text_original": "然後隨風飄逸。久而久之,這些石頭,在銀楓面上便會呈現非常光滑的青石面。",
      "correction_applied": true,
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    {
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      "text": "這類的岩石又稱為風蝕石。",
      "tokens": [
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      "text_original": "這類的岩石又稱為風魔石。",
      "correction_applied": true,
      "correction_source": "llm_correct_a_presegmentation"
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    {
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      "text": "海邊的岩石,長時間受到海浪的衝擊,其中也夾雜著許多的砂石顆粒。",
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      "text_original": "海邊的岩石,長時間受到海浪的衝擊,其中也夾長著許多的砂石顆粒。",
      "correction_applied": true,
      "correction_source": "llm_correct_a_presegmentation"
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    {
      "id": 42,
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      "text": "這樣的衝擊也會形成侵蝕的現象。",
      "tokens": [
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      "text_original": "這樣的衝擊也會形成青石的現象。",
      "correction_applied": true,
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    {
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      "text": "照片上這就是典型的海蝕洞。",
      "tokens": [
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      "text_original": "照片上這就是典型的海石洞。",
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      "text": "接下來我們先介紹搬運的現象。",
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    {
      "id": 45,
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      "text": "想像一下,桌面上有一堆砂子。",
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      "text": "我們在砂子上吹了一口氣,砂子隨風揚起。",
      "tokens": [
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      "text_original": "我們在砂子上吹了一口氣,砂子隨風仰起。",
      "correction_applied": true,
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      "text": "這個仰起的過程,我們就可以說是砂子被風搬運了。",
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      "text": "當風停下來之後,這些砂子又會慢慢的落下來。",
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    {
      "id": 49,
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      "text": "這就是沉積作用。",
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      "text": "搬運與沉積的作用,我們可以從河床上輕易的辨識。",
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      "text": "較大的石頭需要較大的水流才能搬運。",
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      "text": "因此河川上游的大石頭,在水流量大的時候順流而下。",
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      "text": "當水流量變得比較和緩的時候,大石頭就會先沉積下來。",
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      "text": "比較小的石頭呢,會繼續順流而下。",
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      "text": "當水量變得更和緩的時候,較小的石頭也會開始沉積下來。",
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      "text": "以此類推,到最下游的地方,一般來說都是細微的砂子。",
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    {
      "id": 57,
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      "text": "再從岩石的形狀來判斷,上游的石頭經歷過的碰撞較少。",
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      "text": "所以大部分都呈現岩石破碎的樣子。",
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      "text": "在繼續往下游移動的過程中,岩石經歷的碰撞也越來越多。",
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      "text": "漸漸的石頭會變得比較圓潤、光滑。",
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      "text": "通常在河川的中下游,我們可以看到比較多的鵝卵石。",
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      "text": "從剛剛的敘述,我們知道,水在流動的時候,因為流動時同時夾帶許多岩石顆粒,",
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      "text_original": "從剛剛的敘述,我們知道,水在流動的時候,因為流動時同時夾下來許多岩石顆粒,",
      "correction_applied": true,
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    {
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      "text": "這些會對河床造成侵蝕的現象。",
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      "text": "因此當河川進入大海的時候,高低落差不見了,河流的速度也就沒有了。",
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      "text": "這時所有的河流所帶下的岩石顆粒砂石,都會開始沉降。",
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      "text": "因此我們說,大海是河道的最終侵蝕基準面。",
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      "text": "如果河道中間流經過湖泊,那麼河流的流速也會突然陡降。",
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      "text_original": "如果河道中間流經過湖泊,那麼河流的流速也會突然抖降。",
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      "text": "這時候也會發生沉降的現象,因為這是暫時的。",
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      "text": "所以我們就說,湖泊是河道暫時侵蝕基準面。",
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    {
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      "text": "如果河道當中有一個凸起,這個凸起呢,會接受到比較多的侵蝕現象。",
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      "text": "所以一段時間之後,這個凸起就會消失。",
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    {
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      "text": "整個河道會成為均勻分布的平衡狀態。",
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    {
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      "text": "假如河道當中有一座橋,橋墩埋在河床下面。",
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    {
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      "text": "這時候下游如果有人大量的開採砂石,",
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      "text": "結果上游河床的石頭就會向開採處移動。",
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      "text": "最終使得河床下陷,橋墩裸露。",
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      "text": "這時橋墩很容易被水流侵蝕,導致橋樑被破壞。",
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      "text": "因此橋樑的上下游都不應該開採砂石以維護橋樑的安全。",
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      "text": "同樣的道理,海岸線的位置是河川上游所帶下來的砂石,",
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    {
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      "text": "與海浪沖刷所帶走的砂石平衡的結果。",
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    {
      "id": 81,
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      "text": "如果河川上游大量開採砂石,或是築起水壩,",
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      "text_original": "如果河川上游大量開採砂石,或是足起水壩,",
      "correction_applied": true,
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    {
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      "text": "使得砂石不再流向海洋,",
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    {
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      "text": "那麼河川所帶下來的砂石,",
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    {
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      "text": "就會少於海浪沖刷所帶走的砂石,",
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      "text": "最終將使海岸線退縮。",
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    {
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      "text": "以上就是地貌的改變與平衡的介紹,",
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    {
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      "text": "我們下次再會。",
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    {
      "id": 88,
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      "text": "請問一下,請問一下,",
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      "text": "請問一下,請問一下,",
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    {
      "id": 90,
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      "text": "請問一下,請問一下,",
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    {
      "id": 91,
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      "text": "請問一下,請問一下,",
      "tokens": [
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    {
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