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ÀÛ¼ºÀÏ : 17-07-14 19:21
[Inter] Groundwater Á¤¸®
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   Groundwater.docx (15.9K) [11] DATE : 2017-07-14 19:21:05
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<Groundwater>


[1] ¹®´ÜÁ¤¸®

1¹®´Ü
#Definition of groundwater
1. saturate the ground -> fill all the spaces
2. meteoric water -> water cycle
-> ordinary -> soak into ground from surface, precipitation, lake and stream
-> long period remain
 space in the solid ground -> hold all this water?
2¹®´Ü
#Process of sediment
1. common spaces -> among particles of unconsolidated sand and gravel
2. this material beneath soil = fast rivers carrying loads of sediment
ex. ice sheets -> melt -> huge volumes of water flow -> water with pebbles, gravel and sand(outwash) -> water flow slow down -> deposit

3¹®´Ü
#sediment
now -> smaller scale -> sediment-laden river or stream emerge [valley  flat land(slow-> deposit -> fanwise] or river  lake or sea [slow -> deposit -> lake floor, seafloor]
future -> located in land

4¹®´Ü
#unconsolidated sediment
lowland(once the bed of a river =former riverbed = sandbars) -> buried by soil(sediment=gravels and sands) -> be saturated with groundwater  unconsolidated sediment

5¹®´Ü
#consolidated sediment
Consolidated sediment contain pore -> the gaps among the original grains=unconsolidated sediment not totally plug(pore O) -> dissolve by groundwater -> consolidation -> consolidated sediment as porous as unconsolidated sediment
6¹®´Ü
#porous
both loose(unconsolidated) or cemented(consolidated) consist of space -> crystalline rocks solid -> except basalt(Çö¹«¾Ï) -> very porous

7¹®´Ü
# Porosity
empty space -> porosity -> not same permeability -> porosity depend on ¡®size¡¯

8¹®´Ü
# Surface tension
sample -> in a dry place, much of water in a sample will drain -> without surface tension : water would drain / surface tension : water is held

9¹®´Ü
#Pore size
even though their porosities same -> the amount of water varies -> depend on ¡°size¡±
-> large pores : too heavy for surface tension to hold -> drain away
-> small pores : too light to overcome the force of surface tension -> holding water in place

[2] Áö¹®Á¤¸®

saturate (into)
È컶 Àû½Ã´Ù, ½º¸çµé´Ù
= soak (into)

by far
ÈξÀ, ´Ü¿¬ÄÚ
 far
ad ¸Ö¸®, ¾ÆµæÈ÷
 far and away ÈξÀ, ´Ü¿¬
 so far ÀÌ Á¡±îÁö´Â, ±× ¶§±îÁö´Â
 far from Á¶±Ýµµ ~¾Ê´Ù = not at all

into
prep. ¾ÈÀ¸·Î, -À¸·Î (¹æÇ⼺)

 ¹æÇ⼺
 water has soaked into the ground ( water  ground)
 the ground from the surface, precipitation ( surface, precipitation  ground )

At first thought
¾ð¶æ º¸¾ÒÀ» ¶§
= swift look, take a glance into, give(take, throw ..) a glance at, steal a glance at

bed
¹Ù´Ú
=base

flow
vi È帣´Ù / n È帧
 flow away Èê·¯°¡´Ù
 flow into ~·Î µé¾î°¡´Ù
 flow from »ù¼Ú´Ù, ³ª¿À´Ù
 flow with ¹ü¶÷ÇÏ´Ù, ÃæºÐÇÏ´Ù
 = circulate

loads of
¸¹Àº
= tons of

glacial outwash = outwash
ºùÇÏ¿¡¼­ Èê·¯³»¸° ÅðÀû¹°
= glacial drift

to this day
¿À´Ã³¯±îÁö
=up to now, until now

drop
=deposit

consolidate
°áÇÕÇÏ´Ù, ±»¾îÁö´Ù
= cement

, or ,
~ÀÎÁö °£¿¡

cling to
°í¼öÇÏ´Ù
=adhere


±ÛÀÚ¼ö: 1366ÀÚ

 
 

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