CN105787263B - A kind of definite method of large-scale shallow water lake strength of turbulence spatial framework - Google Patents

A kind of definite method of large-scale shallow water lake strength of turbulence spatial framework Download PDF

Info

Publication number
CN105787263B
CN105787263B CN201610097002.6A CN201610097002A CN105787263B CN 105787263 B CN105787263 B CN 105787263B CN 201610097002 A CN201610097002 A CN 201610097002A CN 105787263 B CN105787263 B CN 105787263B
Authority
CN
China
Prior art keywords
lake
suspension
concentration
spatial
strength
Prior art date
Legal status (The legal status is an assumption and is not a legal conclusion. Google has not performed a legal analysis and makes no representation as to the accuracy of the status listed.)
Active
Application number
CN201610097002.6A
Other languages
Chinese (zh)
Other versions
CN105787263A (en
Inventor
龚志军
张运林
施坤
秦伯强
刘笑菡
周永强
Current Assignee (The listed assignees may be inaccurate. Google has not performed a legal analysis and makes no representation or warranty as to the accuracy of the list.)
Nanjing Institute of Geography and Limnology of CAS
Original Assignee
Nanjing Institute of Geography and Limnology of CAS
Priority date (The priority date is an assumption and is not a legal conclusion. Google has not performed a legal analysis and makes no representation as to the accuracy of the date listed.)
Filing date
Publication date
Application filed by Nanjing Institute of Geography and Limnology of CAS filed Critical Nanjing Institute of Geography and Limnology of CAS
Priority to CN201610097002.6A priority Critical patent/CN105787263B/en
Publication of CN105787263A publication Critical patent/CN105787263A/en
Application granted granted Critical
Publication of CN105787263B publication Critical patent/CN105787263B/en
Active legal-status Critical Current
Anticipated expiration legal-status Critical

Links

Classifications

    • GPHYSICS
    • G16INFORMATION AND COMMUNICATION TECHNOLOGY [ICT] SPECIALLY ADAPTED FOR SPECIFIC APPLICATION FIELDS
    • G16ZINFORMATION AND COMMUNICATION TECHNOLOGY [ICT] SPECIALLY ADAPTED FOR SPECIFIC APPLICATION FIELDS, NOT OTHERWISE PROVIDED FOR
    • G16Z99/00Subject matter not provided for in other main groups of this subclass

Abstract

The present invention provides a kind of definite method of large-scale shallow water lake strength of turbulence spatial framework, including:Lake region prevailing wind direction for many years is obtained based on history weather data analysis day by day;Each mesh point east, south, west, north 4 orientation offshore distance in lake is calculated, mesh point offshore distance under 2 prevailing wind directions is chosen and sums it up as lake remoulding indes, and then obtains the spatial distribution of remoulding indes, characterizes the spatial framework of lake strength of turbulence;Each mesh point concentration of suspension in lake is obtained according to actual measurement or remote sensing image inverting;Each mesh point remoulding indes of calculating are subjected to correlation analysis and spatial framework consistency analysis with corresponding concentration of suspension, it is whether consistent according to the remoulding indes spatial framework of foundation and concentration of suspension spatial framework height, and it whether there is extremely notable positive correlation between the two, carry out the efficiency analysis of remoulding indes.The present invention is suitable for all kinds of large-scale shallow water lakes, while operating method is easy, easy to spread and application.

Description

A kind of definite method of large-scale shallow water lake strength of turbulence spatial framework
Technical field
The present invention relates to environmental science and monitoring technical fields, are related to a kind of Lake Water energetic disturbance strength determining method, A kind of more particularly to definite method of large-scale shallow water lake strength of turbulence spatial framework.
Background technology
Easily sediment resuspension is influenced shallow lake caused by by the hydrodynamic(al)s force-disturbance such as stormy waves, and sediment resuspension exists Control Shallow Lake Ecosystems structurally and functionally play an important role.Influence of the hydrodynamic force to Shallow Lake Ecosystems It is many, mainly includes:
1)The disturbance of stormy waves causes the internal loading of nutritive salt and phytoplankton recovery in bed mud, adds water nutrition Concentration, the growth for promoting algae, promote primary productivity to improve;
2)Changing the redox environment of water-soil environment makes microorganism change, so as to influence the degradation of organic matter and ore deposit Change;
3)Determine cyanobacteria sinking, floating, vertical migration and horizontal drift, and then control cyanobacterial bloom spatial and temporal distributions and Migration accumulation;
4)The settling flux of deposit caused by hydrodynamic(al) force-disturbance often adds the concentration of suspension of overlying water, promotes light Attenuation, reduce euphotic zone depth, often inhibit Primary Productivity of Lake and influence submerged plant spatial framework;
5)Hydrodynamic(al) force-disturbance can destroy submerged plant and emergent aquactic plant root, stem, leaf, influence plant growth and distribution.
It is shallow lake that, which there is more than 1/3rd freshwater lake in China, and the middle and lower reach of Yangtze River is even more that China's shallow lake is concentrated Distributed areas summarize the typical large-scale shallow water lake such as Poyang Lake, Dongting Lake, Taihu Lake, Chaohu, and hydrodynamic(al) force-disturbance is in these lakes Vital effect is play in pool water environment and ecosystem development.Therefore, quick, easy definite large-scale shallow water lake Hydrodynamic force strength of turbulence is the premise and basis for carrying out lake ecological environment evolution research.
Hydrodynamic force strength of turbulence spatial framework is obtained there are mainly two types of method, a kind of method be by multiple website waves, Lake current instrument Simultaneous Determination, another method are that conditions setting carries out hydrodynamic simulation under prevailing wind direction.Hydrodynamic(al) force-disturbance is strong The on-site measurement of degree will set up the even tens of set waves of more sets, lake current instrument Simultaneous Determination hydrodynamic force strength of turbulence in different waters It is extremely difficult.Even if carry out hydrodynamic intensity Simultaneous Determination, the hydrodynamic force strength of turbulence value of acquisition also tend to be it is discrete, very Difficulty is interpolated on different mesh points.And hydrodynamic simulation is often to obtain under the conditions of preferable boundary condition and wind field, with There are still larger gaps for hydrodynamic force strength of turbulence under actual environment.What is more important either on-site measurement or hydrodynamic(al) Power is simulated, and had not only been needed expensive instrument but also had been needed professional person, it is difficult to quickly realize hydrodynamic force strength of turbulence spatial framework really It is fixed, therefore the influence research for carrying out general hydrodynamic(al) force-disturbance to environmental element can not be met.
The content of the invention
The present invention seeks to establish a kind of definite side of simple, quick large-scale shallow water lake strength of turbulence spatial framework Method, suitable for all kinds of large-scale shallow water lakes, while operating method is easy, easy to spread and application.
In the present invention, the height of large-scale shallow water lake mesh point concentration of suspension reflects the strong of mesh point hydrodynamic(al) force-disturbance Weak, in the art, concentration of suspension is commonly used to characterize hydrodynamic force strength of turbulence, judges the validity of remoulding indes.
To achieve the above object, the present invention adopts the following technical scheme that:
A kind of definite method of large-scale shallow water lake strength of turbulence spatial framework, the described method comprises the following steps:
S1, lake region prevailing wind direction for many years is obtained based on history weather data analysis day by day;
S2, each mesh point east, south, west, north 4 orientation offshore distance in lake is calculated, it is off line chooses 2 prevailing wind directions Lattice point offshore distance is summed it up as lake remoulding indes, and then obtains the spatial distribution of remoulding indes, characterizes lake strength of turbulence Spatial framework;
S3, each mesh point concentration of suspension, concentration of suspension in lake are obtained according to actual measurement or remote sensing image inverting Height reflect the power of mesh point hydrodynamic(al) force-disturbance;
S4, each mesh point remoulding indes of calculating are subjected to correlation analysis and spatial framework with corresponding concentration of suspension Consistency analysis, it is whether consistent according to the remoulding indes spatial framework of foundation and concentration of suspension spatial framework height, and two It whether there is extremely notable positive correlation between person, carry out the efficiency analysis of remoulding indes.
As a further improvement on the present invention, the definite method of " prevailing wind direction for many years " is specially in the step S1:
Based on long-range meteorological observe data, analysis north, north-northeast, northeast, east-north-east, east, east-south-east, the southeast, south-southeast, The frequency that 16 south, south-southwest, southwest, W.S.W, west, cc north, northwest, North by Northwest wind directions occur, so determine east, south, Lake prevailing wind direction for many years under west, 4, north orientation.
As a further improvement on the present invention, offshore distance calculating method is specially in the step S2:
According to each mesh point in lake, determine the orientation offshore back gauge of its east, south, west, north 4, calculate each grid Offshore and then obtains the space lattice of remoulding indes apart from adduction value for characterizing lake remoulding indes o'clock under 2 prevailing wind directions Office.
As a further improvement on the present invention, the mesh point is dimensioned to 100m*100m to 1000m*1000m.
As a further improvement on the present invention, the spatial distribution acquisition methods of concentration of suspension are specific in the step S3 For:
Based on full lake, several concentration of suspension interpolation for being uniformly distributed website measure obtain the space point of concentration of suspension Cloth.
As a further improvement on the present invention, the step S3 includes 50-100 and is uniformly distributed website.
As a further improvement on the present invention, the spatial distribution acquisition methods of concentration of suspension are specific in the step S3 For:
Concentration of suspension spatial distribution is obtained based on MODIS, MERIS image data inverting.
As a further improvement on the present invention, the spatial resolution of concentration of suspension spatial distribution is in the step S3 250m*250m or 300m*300m.
As a further improvement on the present invention, the efficiency analysis of remoulding indes specifically includes in the step S4:
If the remoulding indes spatial framework and concentration of suspension spatial framework established are highly consistent, and exist between the two Extremely notable positive correlation, the then remoulding indes built are effective remoulding indes, and otherwise, the remoulding indes of structure are invalid disturbance Index.
The beneficial effects of the invention are as follows:
(1)It is not required to carry out wave, lake current on-site measurement and hydrodynamic simulation, you can determine the space lattice of lake strength of turbulence Office;
(2)Operation is very easy, required at low cost, and this method only needs to know that the prevailing wind direction in research lake can calculate The spatial framework of remoulding indes and definite strength of turbulence;
(3)The present invention, which enriches and developed Lake Water energetic disturbance, determines method, can be widely applied to be to carry out large size Large-scale shallow water lake Hydrodynamic Process and its ecology are deepened in the research that shallow lake hydrodynamic(al) force-disturbance develops to lake ecological environment Understanding in terms of environmental effect.
Description of the drawings
Fig. 1 is the definite method flow diagram of the medium-and-large-sized shallow lake strength of turbulence spatial framework of the present invention;
Fig. 2 is the 1956-2014 TAI HU AREAs wind direction frequency that meteorological data counts day by day in a specific embodiment of the invention Rate rose is schemed;
Fig. 3 is the medium-and-large-sized shallow lake remoulding indes definition of a specific embodiment of the invention(Remoulding indes=X1+X2);
Fig. 4 divides for the remoulding indes space being calculated under Taihu Lake north wind prevailing in a specific embodiment of the invention and east wind Cloth;
Fig. 5 is the Taihu Lake suspension for observing interpolation of data in a specific embodiment of the invention based on 67 websites October in 2004 Object concentration space general layout;
Fig. 6 is that the Taihu Lake based on the extraction of 50 scape MERIS remote sensing images of 2003-2011 in a specific embodiment of the invention hangs Float concentration space general layout;
Fig. 7 is Taihu Lake concentration of suspension and remoulding indes based on MERIS Extraction of Image in a specific embodiment of the invention Between linear relationship.
Specific embodiment
Below with reference to each embodiment shown in the drawings, the present invention will be described in detail.But these embodiments are not The limitation present invention, structure that those of ordinary skill in the art are made according to these embodiments, method or change functionally It changes and is all contained in protection scope of the present invention.
The invention discloses a kind of definite methods of large-scale shallow water lake strength of turbulence spatial framework, comprise the following steps:
S1, lake region prevailing wind direction for many years is obtained based on history weather data analysis day by day;
The definite method of " prevailing wind direction for many years " is specially:
Based on long-range meteorological observe data, analysis north, north-northeast, northeast, east-north-east, east, east-south-east, the southeast, south-southeast, The frequency that 16 south, south-southwest, southwest, W.S.W, west, cc north, northwest, North by Northwest wind directions occur, so determine east, south, Lake prevailing wind direction for many years under west, 4, north orientation.
S2, each mesh point east, south, west, north 4 orientation offshore distance in lake is calculated, it is off line chooses 2 prevailing wind directions Lattice point offshore distance is summed it up as lake remoulding indes, and then obtains the spatial distribution of remoulding indes, characterizes lake strength of turbulence Spatial framework;
Wherein, offshore distance calculating method is specially:
According to each mesh point in lake, determine the orientation offshore back gauge of its east, south, west, north 4, calculate each grid Offshore and then obtains the space lattice of remoulding indes apart from adduction value for characterizing lake remoulding indes o'clock under 2 prevailing wind directions Office.Preferably, mesh point is dimensioned to 100m*100m to 1000m*1000m etc. in the present invention.
S3, each mesh point concentration of suspension, concentration of suspension in lake are obtained according to actual measurement or remote sensing image inverting Height reflect the power of mesh point hydrodynamic(al) force-disturbance;
The spatial distribution acquisition methods of concentration of suspension include two kinds:
(1), it is several based on full lake(50-100)The concentration of suspension interpolation for being uniformly distributed website measure obtains suspended matter The spatial distribution of concentration.Or,
(2), 250m*250m 300m*300m spatial resolutions are obtained based on MODIS, MERIS image data inverting Concentration of suspension spatial distribution.
S4, each mesh point remoulding indes of calculating are subjected to correlation analysis and spatial framework with corresponding concentration of suspension Consistency analysis, it is whether consistent according to the remoulding indes spatial framework of foundation and concentration of suspension spatial framework height, and two It whether there is extremely notable positive correlation between person, carry out the efficiency analysis of remoulding indes.
Wherein, the efficiency analysis of remoulding indes specifically includes:
If the remoulding indes spatial framework and concentration of suspension spatial framework established are highly consistent, and exist between the two Extremely notable positive correlation, the then remoulding indes built are effective remoulding indes, and otherwise, the remoulding indes of structure are invalid disturbance Index.
Below with the strong large-scale shallow water lake Taihu Lake of hydrodynamic(al) force-disturbance(Area is 2338km2)For example, to the present invention It is described further.Taihu Lake area is 2338 km2, and its mean depth only has 1.9m, the square root of area of lake divided by average The lake power that the depth of water calculates is than up to 25.6, and when the power in lake ratio is more than 0.8, the deposit in entire lake be likely to by Hydrodynamic(al) force-disturbance is formed on, therefore Taihu Lake is a typical large-scale shallow water lake, hydrodynamic(al) force-disturbance is strong.
Fig. 2 is based on Taihu Lake Dongshan meteorological site 1956-2014 wind directions that meteorological measuring comes out day by day frequency Rate rose is schemed.By this figure it was determined that TAI HU AREA prevailing wind direction for northwester it is by north, southeaster is by east, by east, south, west, Northern 4 orientation are classified, and the prevailing wind direction of TAI HU AREA is north wind and east wind.
Fig. 3 is the definition of remoulding indes, and Taihu Lake is under prevailing wind direction north wind and east wind effect, and mesh point is from northern bank and eastern bank The sum of distance be remoulding indes.
Fig. 4 is the remoulding indes spatial distribution being calculated under Taihu Lake north wind prevailing and east wind.Two are calculated according to step S2 It is remoulding indes that mesh point offshore distance, which sums it up, under a prevailing wind direction, and as can be seen from Figure 4, there are apparent spaces for Taihu Lake remoulding indes Difference, high level are located at west, west and south littoral zone and open waters, low value and are distributed in north, the east and southeast arm of lake and bank Band.
Fig. 5, Fig. 6 are respectively the Taihu Lake concentration of suspension spatial framework based on actual measurement and the extraction of MERIS remote sensing images.Pass through Fig. 5, Fig. 6 it was determined that Taihu Lake concentration of suspension there are apparent spatial diversity, high level is located at west, west and south littoral zone and opens Spacious waters, low value are distributed in north, the east and southeast arm of lake and littoral zone, and shallow lake concentration of suspension is largely determined by wind The influence of sediment resuspension caused by wave disturbance, therefore its height reflection wave disturbance intensity, spatial distribution refer to disturbance Number space distribution height is consistent.
Fig. 7 is each mesh point of MERIS Extraction of Image(Pixel point)Between concentration of suspension and corresponding remoulding indes Linear relationship chart.By this figure it can be found that concentration of suspension has extremely notable positive correlation with remoulding indes, embody the present invention and carry The remoulding indes gone out can characterize shallow lake strength of turbulence well, be that one kind is quick, easy strength of turbulence spatial framework is true Determine method.
Data needed for the method for the present invention and data are as follows:
1)Meteorological data:The long-term wind speed and direction data day by day of TAI HU AREA Dongshan weather station 1956-2014, for counting Study area's prevailing wind direction.
2)Concentration of suspension data:Concentration of suspension spatial framework that in October, 2004,67, Taihu Lake website observed, 50 scape MERIS remote sensing images of 2003-2011 extract Taihu Lake concentration of suspension spatial framework, for evaluating the accurate of remoulding indes Property and feasibility.
Operating procedure:
(1)TAI HU AREA Dongshan weather station 1956-2014 wind speed and direction observation data day by day are compiled first, are based on Long-range meteorological observes data, analysis north, north-northeast, northeast, east-north-east, east, east-south-east, the southeast, south-southeast, south, south-southwest, west The frequency that south, W.S.W, west, cc north, northwest, the wind direction of North by Northwest 16 occur, and then determine the orientation of east, south, west, north 4 Lake prevailing wind direction for many years, north wind and east wind are Taihu Lake prevailing wind direction for many years.
(2)Calculate each 4 orientation offshore distances in mesh point east, south, west, north in Taihu Lake, choose prevailing wind direction under north wind and Each mesh point remoulding indes are used as with a distance from northern bank and eastern bank under east wind effect, and then obtain the space point of Taihu Lake remoulding indes Cloth characterizes the spatial framework of lake strength of turbulence;
(3)It is empty that concentration of suspension is obtained according to the Taihu Lake concentration of suspension data interpolating that October in 2004,67 websites monitored Between general layout, while each mesh point suspended matter is obtained in lake based on 50 scape MERIS remote sensing image datas invertings of 2003-2011 Concentration, the height of concentration of suspension reflect the power of mesh point hydrodynamic(al) force-disturbance;
(4)The Taihu Lake suspended matter that each mesh point remoulding indes in the Taihu Lake of calculating are obtained with actual measurement and remote sensing image inverting Concentration carries out spatial framework consistency analysis and correlation analysis, finds the remoulding indes space lattice that the method for the present invention is defined and calculated Office is highly consistent with concentration of suspension spatial framework, and there is extremely notable positive correlation between remoulding indes and concentration of suspension, And then demonstrate the validity of remoulding indes.
The beneficial effects of the invention are as follows:
(1)It is not required to carry out wave, lake current on-site measurement and hydrodynamic simulation, you can determine the space lattice of lake strength of turbulence Office;
(2)Operation is very easy, required at low cost, and this method only needs to know that the prevailing wind direction in research lake can calculate The spatial framework of remoulding indes and definite strength of turbulence;
(3)The present invention, which enriches and developed Lake Water energetic disturbance, determines method, can be widely applied to be to carry out large size Large-scale shallow water lake Hydrodynamic Process and its ecology are deepened in the research that shallow lake hydrodynamic(al) force-disturbance develops to lake ecological environment Understanding in terms of environmental effect.
It should be appreciated that although this specification is described in terms of embodiments, but not each embodiment only includes one A independent technical solution, this description of the specification is merely for the sake of clarity, and those skilled in the art should will say For bright book as an entirety, the technical solution in each embodiment may also be suitably combined to form those skilled in the art can With the other embodiment of understanding.
Those listed above is a series of to be described in detail only for feasibility embodiment of the invention specifically Bright, they are not to limit the scope of the invention, all equivalent implementations made without departing from skill spirit of the present invention Or change should all be included in the protection scope of the present invention.

Claims (7)

  1. A kind of 1. definite method of large-scale shallow water lake strength of turbulence spatial framework, which is characterized in that the described method includes following Step:
    S1, lake region prevailing wind direction for many years is obtained based on history weather data analysis day by day;
    Wherein, the definite method of the prevailing wind direction for many years is:
    Based on long-range meteorological observe data, analysis north, north-northeast, northeast, east-north-east, east, east-south-east, the southeast, south-southeast, south, The frequency that 16 south-southwest, southwest, W.S.W, west, cc north, northwest, North by Northwest wind directions occur, so determine east, south, west, Lake prevailing wind direction for many years under northern 4 orientation;
    S2, each mesh point east, south, west, north 4 orientation offshore distance in lake is calculated, chooses mesh point under 2 prevailing wind directions Offshore distance is summed it up as lake remoulding indes, and then obtains the spatial distribution of remoulding indes, characterizes the sky of lake strength of turbulence Between general layout;
    S3, each mesh point concentration of suspension, the height of concentration of suspension in lake are obtained according to actual measurement or remote sensing image inverting The low power for reflecting mesh point hydrodynamic(al) force-disturbance;
    S4, each mesh point remoulding indes of calculating and corresponding concentration of suspension are subjected to correlation analysis and spatial framework is consistent Property analysis, it is whether consistent according to the remoulding indes spatial framework of foundation and concentration of suspension spatial framework height, and the two it Between with the presence or absence of extremely notable positive correlation, carry out the efficiency analysis of remoulding indes.
  2. 2. a kind of definite method of large-scale shallow water lake strength of turbulence spatial framework according to claim 1, feature exist In in the step S2, mesh point is dimensioned to 100m*100m to 1000m*1000m.
  3. 3. a kind of definite method of large-scale shallow water lake strength of turbulence spatial framework according to claim 1, feature exist In the spatial distribution acquisition methods of concentration of suspension are specially in the step S3:
    Based on full lake, several concentration of suspension interpolation for being uniformly distributed website measure obtain the spatial distribution of concentration of suspension.
  4. 4. a kind of definite method of large-scale shallow water lake strength of turbulence spatial framework according to claim 3, feature exist In the step S3 includes 50-100 and is uniformly distributed website.
  5. 5. a kind of definite method of large-scale shallow water lake strength of turbulence spatial framework according to claim 1, feature exist In the spatial distribution acquisition methods of concentration of suspension are specially in the step S3:
    Concentration of suspension spatial distribution is obtained based on MODIS, MERIS image data inverting.
  6. 6. a kind of definite method of large-scale shallow water lake strength of turbulence spatial framework according to claim 5, feature exist In the spatial resolution of concentration of suspension spatial distribution is 250m*250m or 300m*300m in the step S3.
  7. 7. a kind of definite method of large-scale shallow water lake strength of turbulence spatial framework according to claim 1, feature exist In the efficiency analysis of remoulding indes specifically includes in the step S4:
    If the remoulding indes spatial framework and concentration of suspension spatial framework established are highly consistent, and presence between the two is extremely aobvious Positive correlation is write, then the remoulding indes built are effective remoulding indes, and otherwise, the remoulding indes of structure refer to for invalid disturbance Number.
CN201610097002.6A 2016-02-22 2016-02-22 A kind of definite method of large-scale shallow water lake strength of turbulence spatial framework Active CN105787263B (en)

Priority Applications (1)

Application Number Priority Date Filing Date Title
CN201610097002.6A CN105787263B (en) 2016-02-22 2016-02-22 A kind of definite method of large-scale shallow water lake strength of turbulence spatial framework

Applications Claiming Priority (1)

Application Number Priority Date Filing Date Title
CN201610097002.6A CN105787263B (en) 2016-02-22 2016-02-22 A kind of definite method of large-scale shallow water lake strength of turbulence spatial framework

Publications (2)

Publication Number Publication Date
CN105787263A CN105787263A (en) 2016-07-20
CN105787263B true CN105787263B (en) 2018-05-18

Family

ID=56402252

Family Applications (1)

Application Number Title Priority Date Filing Date
CN201610097002.6A Active CN105787263B (en) 2016-02-22 2016-02-22 A kind of definite method of large-scale shallow water lake strength of turbulence spatial framework

Country Status (1)

Country Link
CN (1) CN105787263B (en)

Citations (4)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
CN1563928A (en) * 2004-03-16 2005-01-12 中国科学院南京地理与湖泊研究所 Method and appts. for indoor simulating refloating state of underwater deposition
JP2009187293A (en) * 2008-02-06 2009-08-20 Nec Corp Time-series data analysis system, method and program
CN103175946A (en) * 2013-03-04 2013-06-26 中国科学院南京地理与湖泊研究所 System and method for automatically monitoring lake-flooding of shallow lake
CN103473463A (en) * 2013-09-17 2013-12-25 中国环境科学研究院 Method of quantitative determination of background concentration of nitrogen and phosphorus of water body of lake basins

Patent Citations (4)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
CN1563928A (en) * 2004-03-16 2005-01-12 中国科学院南京地理与湖泊研究所 Method and appts. for indoor simulating refloating state of underwater deposition
JP2009187293A (en) * 2008-02-06 2009-08-20 Nec Corp Time-series data analysis system, method and program
CN103175946A (en) * 2013-03-04 2013-06-26 中国科学院南京地理与湖泊研究所 System and method for automatically monitoring lake-flooding of shallow lake
CN103473463A (en) * 2013-09-17 2013-12-25 中国环境科学研究院 Method of quantitative determination of background concentration of nitrogen and phosphorus of water body of lake basins

Non-Patent Citations (1)

* Cited by examiner, † Cited by third party
Title
"大型浅水湖泊沉积物内源营养盐释放模式及其估算方法";秦伯强 等;《中国科学(D辑:地球科学)》;20051230;第33-44页 *

Also Published As

Publication number Publication date
CN105787263A (en) 2016-07-20

Similar Documents

Publication Publication Date Title
Chen et al. Statistical analysis of regional air temperature characteristics before and after dam construction
Wu et al. Increasing fragmentation and squeezing of coastal wetlands: Status, drivers, and sustainable protection from the perspective of remote sensing
Ge et al. Analysis of the impact on ecosystem and environment of marine reclamation--A case study in Jiaozhou Bay
Uncles Physical properties and processes in the Bristol Channel and Severn Estuary
Liu et al. Topographic mapping of offshore sandbank tidal flats using the waterline detection method: A case study on the Dongsha Sandbank of Jiangsu Radial Tidal Sand Ridges, China
Pasquali et al. The effects of urban and economic development on coastal zone management
Wang Evolution of Yellow River Delta coastline based on remote sensing from 1976 to 2014, China
Prahalad et al. Tasmanian coastal saltmarsh community transitions associated with climate change and relative sea level rise 1975–2009
Garcia-Ayllon Long-term GIS analysis of seaside impacts associated to infrastructures and urbanization and spatial correlation with coastal vulnerability in a mediterranean area
Heath et al. Modelling the sensitivity of suspended sediment profiles to tidal current and wave conditions
CN111855942A (en) Monitoring system for ship and ocean oil spill pollution based on 3S technology
Kolander et al. Quantification of moraine cliff coast erosion on Wolin Island (Baltic Sea, northwest Poland)
Latapy et al. Mesoscale morphological changes of nearshore sand banks since the early 19th century, and their influence on coastal dynamics, Northern France
CN102081033A (en) Suspended sand concentration calculating method based on coastal zone imager
Liu et al. Spatiotemporal changes to the river channel and shoreline of the yellow river delta during a 40-year period (1976–2017)
Tang et al. Channel bed adjustment of the lowermost Yangtze River estuary from 1983 to 2018: Causes and implications
CN105787263B (en) A kind of definite method of large-scale shallow water lake strength of turbulence spatial framework
CN112580270A (en) Seabed sand wave evolution simulation method
Liu et al. Dynamic monitoring and its influencing factors analysis of coastline in the Laizhou Bay since 1985
Schmitt et al. Use of swath bathymetry in the investigation of sand dune geometry and migration around a near shore ‘banner’tidal sandbank
Plew The hydrodynamic effects of long-line mussel farms
CN102109456B (en) Method for calculating high-suspension sediment concentration of Landsat satellite sensors
CN110188155A (en) A kind of synthetic method of vortex three-dimensional information
Wang et al. Assessing the vulnerability of changing coasts, Hainan Island, China
Li et al. Spatiotemporal change patterns of coastlines in Xiangshan Harbor (Zhejiang, China) during the past 40 years

Legal Events

Date Code Title Description
C06 Publication
PB01 Publication
C10 Entry into substantive examination
SE01 Entry into force of request for substantive examination
CB03 Change of inventor or designer information
CB03 Change of inventor or designer information

Inventor after: Gong Zhijun

Inventor after: Zhang Yunlin

Inventor after: Shi Kun

Inventor after: Qin Boqiang

Inventor after: Liu Xiaohan

Inventor after: Zhou Yongqiang

Inventor before: Zhang Yunlin

Inventor before: Shi Kun

Inventor before: Qin Boqiang

Inventor before: Liu Xiaohan

Inventor before: Zhou Yongqiang

GR01 Patent grant
GR01 Patent grant