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Hidrogeologi & Air Bawah Tanah (Hydrogeology and Groundwater)

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Presentation on theme: "Hidrogeologi & Air Bawah Tanah (Hydrogeology and Groundwater)"— Presentation transcript:

1 Hidrogeologi & Air Bawah Tanah (Hydrogeology and Groundwater)

2 Star 5 Ogos 2003

3 Kita sudah bincang mengenai 1.Mineral 2.Batuan 3.Tanah 4.Now AIR pulak

4 Objectives •Memahami perbezaan bidang hidrogeologi dgn hidrologi •Meninjau sumber air dan kitar air •Memahami konsep asas: keliangan (porosity), ketelapan (permeability), akuifer, akuitard, akuiklud. •Memahami konsep paras air dan faktor yg mengawal kedudukannya •Describe the character and behaviour of groundwater in various settings •Discuss environmental problems related to groundwater.

5 Hydrogeology vs hydrology •Sama saja dalam segala segi •Kalau beza sikit sangat

6 Groundwater as an important resource for •Drinking water (life) •Erosion (subterranean caverns) (geological processes) •Equalizer of stream flow (geological processes) •Agriculture

7 Water holding capabilities of rock •Consider properties of rock for storage & transport of water: –Porosity - percentage of rock's volume that is openings –Permeability - ability of rock to transmit a fluid –Aquifer - Rock that is permeable, able to store and transport water (examples) –Aquitard - Rock that is impermeable, acts to hinder or prevent water movement (examples)

8 RESERVOIR AIR •Infinite tapi pasti •Luas tetapi terhad

9 Hydrologic cycle

10 Hydrologic cycle •Powered by solar energy and gravity •Evaporation and precipitation •Continuous recycling of water •Where does water go that falls on the land? –Runoff (air larian) –Infiltration –Evaporation (penyejatan) –Temporary storage as snow and ice –Temp. storage in lakes –Temp storage in plants (evapotranspiration) and animals –Chem reactions with rocks and minerals

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12 •Source of additional water? volcanism (steam) –Volcanism also causes melting of snow caps and mudflows as meltwater mixes with ash

13 Distribution of water on the Earth •Total = 326 million cubic miles •Percentages –97.2% oceans –2.15% ice caps and glaciers –.65% lakes, streams, groundwater, atmosphere (bandingkan dgn slaid no 5)

14 Hydrologic Cycle (in greater details) •A•A. Division of water on Earth •9•97.2% in oceans •2•2.15% in glaciers (largest source of fresh (non- saline) water on Earth) •0•0.62% in groundwater (underground aquifers) •0•0.017% in lakes •0•0.005% in soil moisture •0•0.001% in atmosphere •0•0.0001% in stream channels

15 Water budget • Of all the water that comes out as rain on land: •50% is evaporated and transpired by plants •30% goes into runoff, eventually reaching the ocean •20% goes into groundwater

16 Porosity and Permeability •Dua ciri yg penting yg ada pada batuan dan tanah

17 Porosity (keliangan) is the amount of pore space in a rock (the spaces between the grains) Porosity = volume of pores/total volume

18 Pores (liang)

19 Tazkirah/peringatan •Tahukah anda semua jenis batuan mendak, igneus dan metamorfik? •Tahukah anda ciri2 asas pada ketiga-tiga jenis batuan tersebut? (struktur kimia, sifat fizik dan kimia, proses kejadiannya/pembentukkannya)

20 •Porosity is independent of grain size. •Porosity depends on: •Sorting of the grains (or uniformity of grain size) Are the grains all the same size (well sorted), or are a variety of grain sizes present, with finer grains filling the spaces between the larger grains (poorly sorted)? •Shape of the grains •Packing and arrangement of grains. Cubic packing. Porosity = 47.64% Rhombohedral packing. Porosity = 25.95%

21 sorting High energy environmentLow energy environment

22 Packing?

23 •What are some examples of a rock with high porosity? •What are some examples of a rock with low porosity? JAWAPAN ANDA?

24 Wentworth scale - grain size scale Particle nameParticle diameter •Boulders> 256 m •Cobbles mm •Pebbles mm •Sand1/16 – 2 mm •Silt1/ /16 mm (or mm) •Clay< 1/256 mm (or < mm) <2 mikron

25 1Terrigenous (detrital or clastic) – bumi/benuaTerrigenous (detrital or clastic)  Conglomerate or Breccia  Sandstone Sandstone  Siltstone  Shale  claystone 2Chemical/biochemicalChemical/biochemical  Evaporites Evaporites  Carbonate sedimentary rocks (limestones and dolostone) Carbonate sedimentary rocks  Siliceous sedimentary rocks Siliceous sedimentary rocks 3Organic (coals)Organic (coals)  Other – ironstones Pengelasan batuan mendak POROSITY? Ada/tak ada Rendah/tinggi

26 Permeability (ketelapan) is the ease with which fluids flow through a rock or sediment •A rock is permeable if fluids pass through it, and impermeable if fluid flow through the rock is negligible

27 Definition of permeability Rujukan: Rock Slope Engineering by Hoek and Bray (1979)

28 Permeability depends on: •Grain size Coarser-grained sediments are more permeable than fine-grained sediments because the pores between the grains are larger. •Sorting •Grain shape •Packing (controls pore size)

29 •What are some examples of a rock with high permeability? •What are some examples of a rock with low permeability? JAWAPAN ANDA?

30 Classification of igneous rocks

31 Mineral yg terdapat pada zon metamorfik REGIONAL

32 Changes that occur in the transformation to become metamorphic rocks Rumus

33 FACIES GRADE

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35 Hubungan antara porosity-permeability

36 •AQUIFER, AQUICLUDES, WATER TABLE, UNCONFINED, CONFINED AND PERCHED WATERS

37 Aquifers and aquicludes •An aquifer is a water-bearing rock. Aquifers have high porosity and high permeability. •Examples of rock types that could be aquifers? •Aquicludes are water-excluding rocks. They have little or no porosity or permeability. •Examples of rock types that could be aquicludes?

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39 •Note that some impermeable rock types may serve as aquifers if they are highly jointed. Water may be in the joints or cracks in the rock

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41 Water table/Paras air •Bergantung kpd topografi

42 Water table

43 The Water Table (Paras air) •When it rains, some of the water percolates or soaks into the ground. We call this infiltration. Some of the water is held in the soil because it clings to the soil particles because of molecular attraction. It may evaporate from the soil or be used by plants (zone of aeration, also called the vadose zone). Both air and water occupy the pores spaces.

44 •Excess water penetrates downward until it reaches the water table. Below this point, all of the pore spaces are filled with water (zone of saturation (ZON TEPU), also called the phreatic zone).

45 •The water table is the top of the zone of saturation. •The water table is not flat. It mimics the topography, but is more subdued. It stands somewhat higher under hills, and lower under valleys.

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49 •Where the water table intersects (or lies above) the ground surface, springs, lakes, swamps, or rivers are present. In humid areas, groundwater movement supplies a flow of water to a stream or river. •If a well is drilled, the waterlevel in the well is at the water table.

50 •The position of the water table may fluctuate with droughts. •If water is withdrawn from a well, the water table is lowered in the immediate vicinity of the well. The lowered surface of the water table around a well forms a conical depression in the water table. It is called the cone of depression. •If significant quantities of water are withdrawn from a well, the cone of depression may be so large that it affects the water level of other wells nearby.

51 Water table & groundwater flow Processes •Recharge-precipitation and infiltration •Discharge-rivers, runoff, pumping •Relation to topography •Relation to seasonality

52 Water table & groundwater flow

53 groundwater

54 Artesian Wells

55 Perched water

56 Groundwater as resource •Seasonal changes •Effects of pumping •Pollution of groundwater •Ogallala aquifer

57 Problems associated with groundwater withdrawal •Ground water depletion •Subsidence • Sinkhole formation •Groundwater pollution or contamination •Saltwater encroachment

58 Seawater before and after pumping

59 groundwater

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61 •Ogallala Aquifer

62 PUMPING TEST

63 DRAWDOWN

64 Sensor untuk mengesan paras air (piezometer)

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