CN1664582A - Method for measuring dome soil erosion amount - Google Patents
Method for measuring dome soil erosion amount Download PDFInfo
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- CN1664582A CN1664582A CN2005100336028A CN200510033602A CN1664582A CN 1664582 A CN1664582 A CN 1664582A CN 2005100336028 A CN2005100336028 A CN 2005100336028A CN 200510033602 A CN200510033602 A CN 200510033602A CN 1664582 A CN1664582 A CN 1664582A
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- particle diameter
- erosion amount
- measuring flume
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Abstract
The invention relates to a method of measuring the eroded dome soil, which including the following steps: (a) designing a measuring slot, which comprises two-stage same slots taking on the upper and lower step gradation, the length, width, depth of the cavity is 300-400cm,40-50cm,50-80cm, the gradation of the upper and lower is 30-50cm; (b) setting the slot on the dome to be measured, the top of the upper slot clings to the dome and accepts the water and sand;(c) after cushioning and depositing through two-stage slot, measuring the grain diameter of the soil in the slot and the original soil, computing the eroded quantity according to the formula Wt : Wt=WDm/BDm.
Description
Technical field
The present invention relates to measurement and computing method to the slope soil erosion amount.
Background technology
Water and soil conservation is the long-term and arduous ecological engineering of China.In order to prevent erosion, often need to measure the soil erosion amount of soil erosion in the research and production construction.Traditional slope soil erosion measuring method normally carries out in " sediment run-off field ".So-called " sediment run-off field " is to build the rectangle wall hurdle body of building certain area on domatic, and cutting off the rainwash of inside and outside, hurdle, and the place near the ground, centre of body of wall establishes an apopore below domatic, connects to introduce with pipeline and measures bucket." sediment run-off field " measure the slope runoff amount still can, but it is extremely inaccurate to be used for the mensuration of soil erosion amount.The subject matter of its existence is: (1) is built the hurdle wall and has been stirred the domatic soil body, has destroyed former domatic soil body state of nature; (2) restriction of tested measuring tank volume, the fence area generally is no more than 40m
2And the wall hurdle intercepts, and the domatic a large amount of runoffs of marge are not flowed through in the field, have greatly reduced former domatic run-off, and the slope erosion power difference that runoff produces is very big; (3) axial pencil water is after the quantity of sand and mud that osculum is discharged also is different from the sediment loss amount of domatic promotion.
The objective of the invention is to propose a kind of survey meter method of new slope soil erosion amount,, reach more accurately and measure purpose easily to overcome the existing problem of above-mentioned traditional slope soil erosion measuring method.
The object of the present invention is achieved like this, design a measuring flume, this measuring flume is by on becoming, the differential identical cell body of two-stage of downstairs is formed, the length of the vallecular cavity of every grade of cell body, wide, be respectively 300~400cm deeply, 40~50cm, 50~80cm, on, following groove is differential at 30~50cm, measuring flume is installed on soil erosion amount to be measured domatic, it is domatic to receive water sand that the upper groove body top is close to, after the buffering precipitation of two-stage measuring flume, by to last, the particle diameter of the grain soil of following groove deposition and the mensuration that corrodes the particle diameter of preceding former soil sample grain soil are calculated soil erosion amount W as follows
t:
W
t=W
Dm/B
Dm
In the formula, D
mBe the native maximum particle diameter of grain of following groove deposition, W
DmFor last groove deposition whole amass in the soil particle diameter D greater than D
mThe general assembly (TW) of whole soil grains, B
DmFor particle diameter D in the former soil sample before corroding greater than D
mThe shared number percent of soil particle.
For when measuring, can all flow into lower groove after making the water of upper groove body full, two abutment walls of the upper groove body of described measuring flume and lower groove connection can make it to form slightly high lock hurdle.When calculating the domatic area of water, to being difficult to differentiate part, available close bolt or thin plate are slightly separated for individual flows simultaneously.
The present invention has following technique effect:
(1) this method has been got rid of the domatic soil that domatic destruction and artificial interference cause and has been stirred and the hydrological characteristics change; Measured value is subjected to the restriction of domatic area size less, can reflect the erosion condition of soil more truly;
(2) through the buffering of measuring flume two-stage precipitation, the sedimentation of most of soil erosion is in groove, and is few by the part clay that spilling water is taken away for less domatic of soil clay particle content, can ignore;
(3) this measuring flume is used for the domatic measurement of water body swelling and subsiding zone, and is upper and lower when mobile at cell body when water level, can be directly used in to measure bank slope soil wave and wash in a pan the erosion amount;
(4) also to have a facility simple for this measuring method, and cost is low, the advantage that measuring method is easy.
Description of drawings
Fig. 1 is the structural representation of the designed measuring flume of the present invention.
Embodiment
Below be an embodiment of the present invention: prepare measuring flume as shown in Figure 1 earlier, this measuring flume constitutes upper and lower two-stage stepped appearance cell body by upper groove body 1 and lower groove 2, the length and width of the vallecular cavity of upper groove body 1 and lower groove 2, be respectively 300cm, 40,50cm deeply, upper and lower groove is differential to be 35cm, form slightly high lock hurdle 3 at two abutment walls of upper groove body and lower groove connection, upper and lower cell body downside at measuring flume has osculum, and this osculum need stop up with embolism 4 during measurement.When the survey timing of carrying out the slope soil erosion amount, measuring flume is installed on measured soil erosion amount domatic, it is domatic to receive water sand that the upper groove body top is close to, and after the buffering precipitation of two-stage measuring flume, calculates soil erosion amount by the following method:
(1) soil sample of following groove deposition is done granularmetric analysis, determine the value D of its maximum particle diameter
m
(2) the complete long-pending soil sample of last groove deposition is screened, count out particle diameter D greater than D
mThe general assembly (TW) W of whole soil grains
Dm
(3) get the preceding former soil sample of erosion and do granularmetric analysis, calculate particle diameter D greater than D
mThe shared number percent B of soil particle
Dm
(4) with W
DmDivided by B
DmGet final product to such an extent that be etched the general assembly (TW) of soil.By formula promptly: W
t=W
Dm/ B
DmCalculate the general assembly (TW) that has been etched soil.
Claims (2)
1. the survey meter method of a slope soil erosion amount, it is characterized in that designing a measuring flume, this measuring flume is by on becoming, the differential identical cell body of two-stage of downstairs is formed, the length of the vallecular cavity of every grade of cell body, wide, be respectively 300~400cm deeply, 40~50cm, 50~80cm, on, following groove is differential at 30~50cm, measuring flume is installed on soil erosion amount to be measured domatic, it is domatic to receive water sand that the upper groove body top is close to, after the buffering precipitation of two-stage measuring flume, by to last, the particle diameter of the grain soil of following groove deposition and the mensuration that corrodes the particle diameter of preceding former soil sample grain soil are calculated soil erosion amount W as follows
t:
W
t=W
Dm/B
Dm
In the formula, D
mBe the native maximum particle diameter of grain of following groove deposition, W
DmFor last groove deposition whole amass in the soil particle diameter D greater than D
mThe general assembly (TW) of whole soil grains, B
DmFor particle diameter D in the former soil sample before corroding greater than D
mThe shared number percent of soil particle.
2. the survey meter method of slope soil erosion amount according to claim 1 is characterized in that the upper groove body of described measuring flume and two abutment walls of lower groove connection form slightly high lock hurdle.
Priority Applications (1)
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CNB2005100336028A CN100371712C (en) | 2005-03-18 | 2005-03-18 | Method for measuring dome soil erosion amount |
Applications Claiming Priority (1)
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CNB2005100336028A CN100371712C (en) | 2005-03-18 | 2005-03-18 | Method for measuring dome soil erosion amount |
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CN1664582A true CN1664582A (en) | 2005-09-07 |
CN100371712C CN100371712C (en) | 2008-02-27 |
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Cited By (6)
Publication number | Priority date | Publication date | Assignee | Title |
---|---|---|---|---|
CN101086494B (en) * | 2007-07-03 | 2010-05-26 | 浙江大学 | Foundation and slope engineering model test platform |
CN101776679A (en) * | 2010-03-08 | 2010-07-14 | 北京林业大学 | Technology for observing slope soil erosion on fixed point by probability integration method |
CN101241119B (en) * | 2008-02-03 | 2011-04-20 | 中国科学院武汉岩土力学研究所 | Rock earth model test groove based on experiment environment and contact face variety and test method |
CN101236191B (en) * | 2008-02-28 | 2011-04-20 | 浙江省水利河口研究院 | Soil erosion real time monitoring instrument |
CN105842426A (en) * | 2016-06-06 | 2016-08-10 | 中国科学院地球化学研究所 | Method for calculating soil erosion or deposit volume in karst region by stone forest |
CN111796075A (en) * | 2020-08-03 | 2020-10-20 | 中国科学院、水利部成都山地灾害与环境研究所 | Terrace-structured device for simulating slope surface water and soil loss and non-point source pollution |
Family Cites Families (2)
Publication number | Priority date | Publication date | Assignee | Title |
---|---|---|---|---|
US5191787A (en) * | 1990-04-11 | 1993-03-09 | The United States Of America As Represented By The Secretary Of Agriculture | Soil erodibility testing |
CN1250943C (en) * | 2003-11-05 | 2006-04-12 | 西南农业大学 | Natural dome soil and water losses monitoring system using nine pore bypass method |
-
2005
- 2005-03-18 CN CNB2005100336028A patent/CN100371712C/en not_active Expired - Fee Related
Cited By (6)
Publication number | Priority date | Publication date | Assignee | Title |
---|---|---|---|---|
CN101086494B (en) * | 2007-07-03 | 2010-05-26 | 浙江大学 | Foundation and slope engineering model test platform |
CN101241119B (en) * | 2008-02-03 | 2011-04-20 | 中国科学院武汉岩土力学研究所 | Rock earth model test groove based on experiment environment and contact face variety and test method |
CN101236191B (en) * | 2008-02-28 | 2011-04-20 | 浙江省水利河口研究院 | Soil erosion real time monitoring instrument |
CN101776679A (en) * | 2010-03-08 | 2010-07-14 | 北京林业大学 | Technology for observing slope soil erosion on fixed point by probability integration method |
CN105842426A (en) * | 2016-06-06 | 2016-08-10 | 中国科学院地球化学研究所 | Method for calculating soil erosion or deposit volume in karst region by stone forest |
CN111796075A (en) * | 2020-08-03 | 2020-10-20 | 中国科学院、水利部成都山地灾害与环境研究所 | Terrace-structured device for simulating slope surface water and soil loss and non-point source pollution |
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CN100371712C (en) | 2008-02-27 |
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