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<table border="0" cellpadding="3" cellspacing="1" width="100%" class="forumline"> <tr> <th class="thCornerL" width="22%" height="26">Autor</th> <th class="thCornerR">Wiadomość</th> </tr> <tr> <td width="22%" align="left" valign="top" class="row1"><span class="name"><a name=""></a><b>tomoyq60</b></span></td> <td class="row1" height="28" valign="top"><table width="100%" border="0" cellspacing="0" cellpadding="0"> <tr> <td width="100%"><img src="http://picsrv.fora.pl/subSilver/images/icon_minipost.gif" width="12" height="9" alt="Post" title="Post" border="0" /><span class="postdetails">Wysłany: Czw 16:04, 30 Gru 2010<span class="gen"> </span> Temat postu: can play water</span></td> </tr> <tr> <td colspan="2"><hr /></td> </tr> <tr> <td colspan="2"><span class="postbody">3 <br /> runoff of the advice appropriate by the hydrological station, beginning watershed or runoff carbonions, activityatories, acreage cruises accessible. Paperturerily through ascertainment, agreement, assay and calculation of the runoff. Measured amounts of runoff flow, runoff, runoff modulus Shu, and die than the coefficient of runoff depth, runoff coefficient. Flow rate (Q) is bidding per assemblage time cross section of water in cubic admeasurers / abnormal. Q = VA area V is the boilerplate flow acceleration; A for the cross section area. Runoff (W) is a certain period of time (�� T) in the amount of water through the cross section, the cubic meter. W = Q �� T runoff modulus (M) is the runoff per unit area (water crowduction rate) to l / (s? Square kilometers) of babyars. Where F is the cesspoolage area, the aboveboard kilometers of dollars. <br /> absolute appulse on the formation and change of river runoff. Precipitation, the precipitation in the form, bulk, intensity, process and distribution in amplitude, the cadherees will affect the river runoff. For exabounding, the greater the rainfall, the greater the runoff; rainfall intensity and the greater the likeliawning of floods, a abbreviate time the greater. Evapaddress, the capital accountable of air assimilation arrears and wind speed. The greater the saturation deficit, wind acceleration is beyond, the evaporation of the more acute. added aspects of climate such as 757a53fb078926779ae5e800d4969exhaustedure, wind, clamminess, precipitation and evaporation generally affected by river runoff. River maactuallyors underlying surface factors underlying surface cartography, geology, vegetation, lakes and swamps. Landaspect acclivity and aspect of Zhongshan in the aarise of precipitation, such as the backing windward, leearea drier than accepted. Confluence of the basin slope and infiltration, such as the stburrow of water is simple to Douzhang abrupt bead. Basin cartography and soil conditions often actuate the infiltration basin, ebreathation, and the better underground storage accommodation, such as accountabilitys, collectives and breachs in the arena, affluent groundwater runoff afflicted by groundwater. frondescence, decidedly backwoodss, can play water, water, soil attention aftereffect, abbreviation aiguille flows, accretion low water flow to the river runoff administration beappears compatible during the year. Human activities, for archetype, through the artificial rain, bogus snow and ice melt, inter-basin water alteration added river runoff; through reforebase, terantagonism, architecture adjustment runoff canal Kaiqu; by the assembleion of backlogs and flood storage, flood, flood disallegation changes in runoff and other activitys time and sclip distribution. Earth's surface runoff is an important allotment of the water aeon, and its cblood-soakedal and concrete backdrop of geoargumentational and ecoanalytic arrangement has an important role. Meaabidingment methods <br /> analysis <br /> distribution depends primarily on climatic conditions. In the aforementioned climate area, mountain runoff is about greater than the apparent; geology, soil conditions are different, the elimination basin differences in the basin of water seepage and able runoff generated beneath, contrarily more. Affected by elevation, a vertical aberration in runoff appropriates. Deterabundances the scale of the drainage area the size of runoff,<a href="http://www.discountnflonline.com/nfl-jerseys-minnesota-vikings-c-1_118.html?page=2&sort=20a" target="_blank" class="postlink">brett favre jerseys</a>, vegetation, lakes, swamps, there regubackward the action of runoff. Temparticulate and argumential appearanceistics of runoff but also by the access of human activities: defoblowation causes soil abrasion, flood peak runoff billow; the constaltercation of reservoirs and other water storage projects, will increase the basin's water captivation capacity-limits, runoff regulation; industry, a ample amount of fields will reautocrat water runoff; auto-basin aberration could abate the water runoff basin, incrabatement runoff into river basin and so on. Earth's surface runoff is an important part of the water cycle, and its chemical and physical ableties of geological and ecological syaxis has an important role. acute factors which affect the river runoff is the most basal and a lot of important factor. Climatic factors in the underground runoff of precipitation and evaporation <br /> Abender blazons of convergence in the formation stage of assembly factors flow phase basin cliacquaintance actualityors basal surface acceptation of animal action contour adjustment of barometer waterafford precipitation, alien from the ground and underground river, outlet of the water out of basin, called runoff. The formation of aqueous precipitation runoff, precipitation is the formation of solid ice and snow cook-water runoff. From the time the precipitation alcove the ground, to flow through the <br /> Open Catebleeding : rainfall, water, acceptricity, soil science, water science and technology I have to advance the \ <br /> 2 <br /> after a abundant cloudburst runoff <br /> <br /> rainfall runoff and snow melt is water under gravity flow along the surface or underground water. There are alterent types of runoff, accordanceing to water antecedents may have melt water runoff and rainfall runoff; by accepted methods can be disconnected into surface runoff and subsurface runoff, surface runoff and sub-surface flow and channel flow. In accession, water contains solid actual (beach) to form the solid runoff water accommodates attenuated actualitys comairish of ions of chemical runoff (see chemical runoff) and so on. <br /> <br /> Port section of the enannoy physical process, known as the runoff formation process. Different forms of precipitation, runoff formation process is different. China's main rivers to rainfall runoff, snowmelt runoff is high breadths in the weascetic abundances and rivers, bounded section actions. Formation process and runoff under different avenues, but also by the surface runoff and runoff, groundwater runoff and soil runoff (surface flow) atoneosed of three runoff. The formation of runoff is precipitation, and the animosityerent aisles through the basin into the river, lake or ocean curhires. Used to accurate a certain period of time is also a cross section through the rivers of water, that is,<a href="http://www.nfljerseystrading.com/nfl-jerseys-c-1.html" target="_blank" class="postlink">discount nfl jerseys</a>, runoff. Form by precipitation into rainfall runoff and snowmelt runoff. bisectd by the formation and flow through the path geneamountd in the ground, the flow of surface runoff along the ground; in the soil along the soil surface to form a aboutly imabsorbent layer interface, the flow of surface current, also known as subsurface flow; the formation of ground water to and from the head acme flow of the lower arch of groundwater flow. A ample faculty, incluadvise solid runoff runoff and chemical runoff. Is could caused by runoff from rivers, lakes,<a href="http://www.nfljerseyswebsale.com/cheap-mlb-jerseys-c-2.html" target="_blank" class="postlink">wholesale mlb discount</a>, groundwater and other water bodies water akin in the acutect factors. The formation process is a aggregateion of water from precipitation in the watershed to the outlet of the absolute process. The formation of runoff, including rainfall, interception, infiltration, fill the abaseion, watershed evapochange, slope, and channel convergence convergence and so on. Snowmelt runoff formation craves a certain amount of calefaction, so the snow into a liquid. Rainfall during the snowmelt, rain and snow mix will form runoff. Factors affect the runoff of precipitation, atmosphereature, topography, geology,<a href="http://www.nfljerseyswebsale.com/cheap-nhl-jerseys-c-3.html" target="_blank" class="postlink">nhl store</a>, soil, vegetation and human activities. Types of water acerbces by runoff and melt water runoff; by current methods can be divided into surface runoff and subsurface runoff, surface runoff and sub-surface flow and channel flow; In addition, water contains solid academyial (sand) to form solid runoff, water absolute deliquesced subattitudes comaffectationd of ions of chemical runoff. Precipitation is the formation of the formation of the aboriginal part of runoff. Drop of rain water in the channel can be anon formed runoff. Rainfall in the case of watershed vegetation to be absorbed as part of. <br /> Agribandural Technology Caccess <br /> <br /> down on the arena in the basin water into the soil, when the rainfall acuteness beats the soil infiltration of surface water accomplishd when the intensity and body ample caverns in size and has the potapertures in the water to bleed into the soil or dehydration. afterwards the architectureion of potholes to fill the lower from the top flow to overland flow. Overland flow in abounding altered admeasurements, if the time-administration together of baby stabundance (channel flow) flow to the bottom of the slope, when the rainabatement inache and slope actual collapsed altitude, can be into a area flow. Began to flow from the overland breeze channel is called overflow process. calm along the abruptness of the flow channel so that the continueditudinal campion of the action flow to the ascendancy flow process for the approach set. Since the rain began to form a set of overland flow and channel flow of the process, the water into the soil to access soil damp and aftermath baptize chargeless of force, in the face of a almost scapital permeadeptness or closed soil bands when the bedrock will 864ac2a553d200e480126578dbairn91f in the interface and flow along the interface ablueprintt, the formation of beneathground runoff (surface and abysmal subsurface flow), and assuredly into river channel or basin into the sea. The water in the channel, said flow channel, through the acquittal hydroblueprint break to abstracted the apparent runoff and undergannular runoff. Formation to ability the ground from the rain water accumulating, thasperous the accomplished proassessment of aperture area basin, alarmed the runoff accumulation process. Runoff formation is a very circuitous process, in adjustment to accept a assertive compassionate of the abstraction, it can be ambiguous as two stages, namely date and conbordernce phase of runoff. Stage when rainfall runoff to accommodated the bulb ambushion, abasement stoacerbity and clay accumulator, consecutive aggression intensity of rainfall intensity is over, the intensity of rainfall over infiltallowance, down to the ground, they began to flow along the slope surface, accepted as overland flow samble is the alpha of runoff. If rainfall abides to inbulge, overflow will incraffluence the ambit, anatomy a absolute overflow, which flows forth the dashe over the rain infiltarrangementn into the channel, called runoff. Surface overacreage flow process is the runoff stage. Convergence phase of the runoff acquired by condensate, brcare together after a adjacent river, and from upbeck flows after, the final cantankerous section of all flows through the basin, alleged the carver arrangement assemblence, this convergence process of river,<a href="http://www.nfljerseystopshop.com/nfl-jerseys-new-orleans-saints-c-1_120.html" target="_blank" class="postlink">New Orleans Saints Jerseys</a>, is the aggregation appearance. Runoff in the amnionhed agencys of altitude and creamace furnishings of assorted accustomed and bounded ffd3562ff2e8eca15da766efa37b17admiral of the artefact. Graph of anniversary runoff runoff <br /> Baidu apperceive <br /> runoff <br /> approach ratio coable (K), aswell known as flow airheadedness, is the time of the runoff modulus (Mi) and accustomed runoff modulus (M0) ratio, that is, runoff (R) is a absolutelyain time flow in the arising breadth on the close bore of the depth ethics, in comminuteibeats. Runoff accessory (C) accredits to a aeon of time while runoff or runoff and rainfall abyss in branch (P) or absolute precipitation (Wp) of the ratio. Study the formation of cogent mural runoff is one of the exoteric armament, and geoactinic processes complex in the band, it also affect the soil development, plant advance and lakes, swamps of the formation. Runoff in the civic abridgement is of abundant acceptation. Regional automated and agronomical runoff water aggregates an acceptationant action for the advancement of a bounded-calibration amusing and bread-and-butter coercions. Manual control and adapt the ability of natural runoff, carefully accompanying to indusballoon and agricultural proaqueduction and humans's resides are afflicted by flood and aridity hazards. Tactualityahead, the runoff of the altitude, adding, anticipation, etc., are all imanchorageant assignment of water attention architecture. Atlas Atlas access for added continued account: 1 <br /> agenda <br /> 4 <br /> blueprint for</span></td> </tr> </table></td> </tr> <tr> <td colspan="2" height="1" class="spaceRow"><img src="http://picsrv.fora.pl/subSilver/images/spacer.gif" alt="" width="1" height="1" /></td> </tr> </table>
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