smaller amounts of other elements) gradually dissociate from the plant matter, increasing its relative carbon content.Coal also contains inorganic components, known as ash. Ash includes minerals such as pyrite [24] and marcasite [25] formed from metals that accumulated in the living tissues of the ancient plants. Quartz [26], clay, and other minerals are also added to coal deposits by wind and groundwater [27]. Ash [28] lowers the fixed carbon content of coal, decreasing its heating value.
NOTES TO THE TEXT
[1] sedimentary rock��������
[2] tropical swamps���ȴ�����
[3] Lush vegetation��ïʢ��ֲ��
[4] club mosses��ʯ��
[5] horsetails����β��ľ������һ��ֲ�
[6] layers of mud and sand����ɰ��
[7] decayed plant material�����õ�ֲ�����
[8] peat����̿
[9] minerals������
[10] lignite����ú
[11] subbituminous coal������ú
[12] bituminous coal����ú
[13] anthracite������ú
[14] Permian��������
[15] Triassic��������
[16] Jurassic��٪��
[17] Cretaceous�����Ѽ�
[18] Tertiary��������
[19] cellulose������
[20] reinforcing material���ӹ̵IJ���
[21] cell walls��ϸ����
[22] lignin��ľ��
[23] tannins������������
[24] pyrite��������
[25] marcasite ��������
[26] quartz��ʯӢ
[27] groundwater������ˮ
[28] ash���ҷ�
��һҳ[1][2]