JPH0632602Y2 - An educational portable vertical wind tunnel for suspending precipitation particles. - Google Patents

An educational portable vertical wind tunnel for suspending precipitation particles.

Info

Publication number
JPH0632602Y2
JPH0632602Y2 JP8756590U JP8756590U JPH0632602Y2 JP H0632602 Y2 JPH0632602 Y2 JP H0632602Y2 JP 8756590 U JP8756590 U JP 8756590U JP 8756590 U JP8756590 U JP 8756590U JP H0632602 Y2 JPH0632602 Y2 JP H0632602Y2
Authority
JP
Japan
Prior art keywords
wind tunnel
vertical wind
velocity
suspending
precipitation particles
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.)
Expired - Lifetime
Application number
JP8756590U
Other languages
Japanese (ja)
Other versions
JPH0445947U (en
Inventor
豊顕 田中
Original Assignee
気象庁長官
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 気象庁長官 filed Critical 気象庁長官
Priority to JP8756590U priority Critical patent/JPH0632602Y2/en
Publication of JPH0445947U publication Critical patent/JPH0445947U/ja
Application granted granted Critical
Publication of JPH0632602Y2 publication Critical patent/JPH0632602Y2/en
Anticipated expiration legal-status Critical
Expired - Lifetime legal-status Critical Current

Links

Landscapes

  • Aerodynamic Tests, Hydrodynamic Tests, Wind Tunnels, And Water Tanks (AREA)

Description

【考案の詳細な説明】[Detailed description of the device] 【産業上の利用分野】[Industrial applications]

理科教育の現場では現象を直接体験させることが最も重
要な課題である。ところが地学の分野(気象・海洋・地
震火山・天文)では対象とする現象の規模が大きく、ま
た現象が相互に複雑に絡み合っているために、現象を観
察したり、実験で再現することがきわめて困難である場
合が多い。あるいは仮に可能であっても、極めて大がか
りな施設が必要になる。知識偏重の社会的風潮と相まっ
て、地学教育における直接体験は敬遠される傾向にあ
る。ところが地学教育は、地球の温暖化の問題、酸性雨
の問題と言った地球規模の問題に対処するための素養を
身につける上で、ますます重要になっている。 本考案は、気象教育の現場に対して、最も身近な気象現
象である雨や雪(総称して降水粒子)の落下姿勢を調べ
るための、安全でしかも容易に運転できる装置を提供す
る。ことに低学年では雨の落下する姿を生徒自身の目で
確認させること、また高学年では空気の抵抗力と水の表
面張力との相互作用を体験させることを目的としてい
る。 本考案はさらに科学実験用の装置として、例えば大気汚
染質の降水による除去機構あるいは雨の酸性化の仕組み
等を調べる手段として活用できる。また各種展示場の体
験コーナに設置することに依って気象学の普及に役立て
ることが出来る。
In the field of science education, experiencing the phenomenon directly is the most important issue. However, in the field of geology (meteorology, oceans, earthquakes, volcanoes, astronomy), the scale of the target phenomena is large, and the phenomena are intricately intertwined with each other, so it is extremely difficult to observe and reproduce them in experiments. Often difficult. Or even if possible, an extremely large-scale facility is required. Coupled with knowledge-oriented social trends, direct experience in earth science education tends to be shunned. However, geoscience education is becoming more and more important in order to acquire the ability to deal with global warming problems and acid rain problems. The present invention provides a safe and easily operable device for investigating the falling attitude of rain and snow (collectively precipitation particles), which are the most familiar meteorological phenomena, in the field of meteorological education. Especially in the lower grades, the purpose is to let students see the falling rain with their own eyes, and in the upper grades, to experience the interaction between air resistance and water surface tension. The present invention can be further utilized as a device for scientific experiments, for example, as a means for investigating the mechanism of removal of air pollutants by precipitation or the mechanism of acidification of rain. It can also be used to disseminate meteorology by installing it in the experience corners of various exhibition halls.

【従来の技術】 落下する雨滴の形を直接調べることはきわめて困難なこ
とである。孫野(1954)は落下する雨滴を直接ストロボ
写真で撮影し、上が球面で下が平面の言わば饅頭形の雨
滴の写真を初めて公表した。しかしこの写真法では雨滴
の大きさと落下速度及び落下中の形態の動的な関係を詳
しく調べることはできない。そこで考え出されたのが垂
直風洞である。落下する雨滴に代わって、逆に空気を吹
き上げ、その上昇気流の中で雨滴を浮かべ、静止した状
態で観察する装置である。 垂直風洞を用いた研究は比較的古く、レナード(Lenar
d,1904)からはじまる。雨滴の大きさ、形と終速度の関
係はブランチャード(Blanchard,1950)からプルパッヒ
ャー(Plupacher,1970)へと比較的多くの研究がなされ
てきた。駒林・権田・磯野(1964)は雨滴の分裂確立を
求め、福田・松尾(1983)は雪結晶の成長と雪片の形成
の研究を行った。また近年関心の高まっている酸性雨の
成因について、プルパッヒャー(Plupacher,1989)は密
閉形の垂直風洞を用いて、落下中の雨滴が空気中に含ま
れるガス状の化学成分が雨滴にとけ込む過程を調べる詳
細な研究を開始している。 以上、実際の研究に用いられている垂直風洞はいずれも
大がかりなものである。特に気流をつくるための送風機
は風量と風圧を確保するために小型でも数10kg以上、
大型では100kgにも及ぶものが用いられており、きわ
めて重い。次に降水粒子を気流の中心軸付近に浮かべる
ために、気流の中心軸の風速をその周囲より若干遅くす
る目的で、風洞の直径の1/10程度の大きさの金網を水平
に中心軸上に固定する方法、あるいは中心軸に防錘形の
デフューザーを取り付ける方法等、いろいろと工夫がな
されており、構造がきわめて複雑になっている。さらに
気流の乱れを取り除くために、複数の金網を直列に配置
する方法、あるいは金網とハニカムを併用する方法のい
ずれかが採用され大型になっている。このように従来の
研究用垂直風洞は大型で、移動して使用することはほと
んど不可能な構造である。さらに取り扱いが複雑であ
り、危険を伴うために教育の現場で使用することは不可
能である。
2. Description of the Related Art It is extremely difficult to directly inspect the shape of a falling raindrop. Sonno (1954) directly shot falling raindrops with strobe photographs, and for the first time published a picture of a so-called bun-shaped raindrop with a spherical upper surface and a flat lower surface. However, this photographic method cannot examine in detail the dynamic relationship between the size of raindrops, the falling velocity, and the morphology during falling. The vertical wind tunnel was conceived there. Instead of falling raindrops, it is a device that blows air upside-down, floating raindrops in the rising air stream and observing in a stationary state. Research using vertical wind tunnels is relatively old, and Lenar
d, 1904). A relatively large amount of research has been conducted on the relationship between raindrop size, shape, and final velocity from Blanchard (1950) to Plupacher (1970). Komabayashi, Gonda and Isono (1964) sought to establish the breakup of raindrops, and Fukuda and Matsuo (1983) studied snowflake growth and snowflake formation. With regard to the cause of acid rain, which has been attracting attention in recent years, Plupacher (1989) uses a closed vertical wind tunnel to explain the process by which a falling raindrop melts the gaseous chemical components contained in the air into the raindrop. Detailed research has begun to investigate. As mentioned above, all vertical wind tunnels used in actual research are large-scale. In particular, the blower for creating the air flow is several tens of kg or more, even if it is small in order to secure the air volume and pressure.
The large ones weigh up to 100 kg and are extremely heavy. Next, in order to float the precipitation particles near the central axis of the air flow, a wire mesh with a size of about 1/10 of the diameter of the wind tunnel is placed horizontally on the central axis in order to slightly slow down the wind speed of the central axis of the air flow. The structure is extremely complicated due to various measures such as fixing to the center or attaching a weight-proof diffuser to the central shaft. Furthermore, in order to remove the turbulence of the air flow, either a method of arranging a plurality of wire nets in series or a method of using a wire net and a honeycomb together is adopted, and the size is increased. As described above, the conventional vertical wind tunnel for research is large in size, and it is almost impossible to move and use it. Furthermore, the handling is complicated and dangerous, and it is impossible to use it in the field of education.

【考案が解決しようとする課題】[Problems to be solved by the device]

本考案では従来の研究用垂直風洞を一般の教室でも使用
できるように小型軽量化し児童生徒が安全に使用できる
ようにすることである。
According to the present invention, the conventional vertical wind tunnel for research is made small and lightweight so that it can be used in a general classroom so that children and students can use it safely.

【課題を解決するための手段】[Means for Solving the Problems]

従来の研究用風洞の作動原理を厳密に分析した結果、降
水粒子を安定して浮遊させるために必要な垂直風洞の備
えるべき条件は、次の三点に集約できることが明らかに
なった。風洞内の気流速度が浮かべようとする降水粒
子の落下速度以上であること、風洞の中心軸を含む断
面で二山形の速度分布をもっていること、気流に乱れ
が少ないこと。本考案は上記三点の要件を完全に満たす
と同時に、上記の課題を一挙に解決するものである。 実施例に対応する第1図を用いて以下に本考案の内容を
説明する。本考案の垂直風洞は次の5つの部分から構成
される。気流を発生させるための軸流ファン(1)、気
流を整流するための整流用ハニカム(2)、鉛直方向に
速度勾配を作るためのテーパー管(3)、二つの風洞パ
イプ(4)、および以上4つの異なる部分を同軸且つ鉛
直に積み上げ、必要な場所に移動できるようにするため
の風洞固定枠(5)。 使用の軸流ファン(1)は一般にはダクトを接続して換
気ファンとして市販されているものである。整流用ハニ
カム(2)は、内径50mm,長さ180mmの塩化ビニールパ
イプ内に、直径4mm,長さ180mmの市販のストローを270
本束ねて固定したものである。テパー管(3)は透明な
プラスチック製のコップの底を抜いたものである。風洞
パイプ(4)は水道の配管に用いる塩化ビニールの、大
きさの異なる2種類のジョイント(100x75,75x50)を使
用した。さらに風洞固定枠(5)は市販の鉄パイプ入り
塩化ビニールパイプを用い、可搬形にするため図の縦方
向のパイプはネジで取り外しが出来るようにした。 この構成に依って大きさ(縦横高さ)380x380x900mm、
全重量約10kgとなり、可搬形の要請が満たされた。フ
ァンは最下部に取り付け、しかも周囲が枠で囲われてい
るので、操作上の安全も確保された。
As a result of rigorous analysis of the working principle of the conventional research wind tunnel, it became clear that the conditions required for the vertical wind tunnel to stably suspend the precipitation particles can be summarized into the following three points. The velocity of the airflow in the wind tunnel is higher than the velocity of the falling precipitation particles, the velocity distribution is bimodal in the cross section including the central axis of the wind tunnel, and there is little turbulence in the air flow. The present invention completely satisfies the above three requirements and simultaneously solves the above problems. The contents of the present invention will be described below with reference to FIG. 1 corresponding to the embodiment. The vertical wind tunnel of the present invention is composed of the following five parts. An axial fan (1) for generating an air flow, a rectifying honeycomb (2) for rectifying the air flow, a taper pipe (3) for creating a velocity gradient in the vertical direction, two wind tunnel pipes (4), and A wind tunnel fixing frame (5) for stacking the above four different parts coaxially and vertically so that they can be moved to a required place. The axial fan (1) used is generally one that is connected to a duct and is commercially available as a ventilation fan. The straightening honeycomb (2) is a vinyl chloride pipe with an inner diameter of 50 mm and a length of 180 mm, and a commercially available straw with a diameter of 4 mm and a length of 180 mm is used for 270
The book is bundled and fixed. The Tepper tube (3) is a clear plastic cup with the bottom removed. The wind tunnel pipe (4) used two types of joints (100x75, 75x50) of vinyl chloride, which are used for water supply pipes and have different sizes. Furthermore, the wind tunnel fixing frame (5) is a commercially available vinyl chloride pipe containing an iron pipe, and in order to make it portable, the vertical pipe in the figure can be removed with screws. Depending on this configuration, the size (height and height) 380x380x900mm,
The total weight is about 10 kg, which satisfies the requirement of portable type. Since the fan is installed at the bottom and is surrounded by a frame, operational safety is ensured.

【作用】[Action]

軸流ファン(1)が作り出す気流の速度分布の特徴は、
中心軸近傍における流速が周辺域の流速より小さいこ
と、つまり中心軸を含む気流の速度分布が二山形になっ
ていることである。この特徴は雨滴を中心軸近傍に浮遊
させるための必要条件である。ところが軸流ファンの気
流は軸方向に捻れがあり、渦巻状になっている。この特
徴は雨滴を安定して浮遊させるには不都合である。この
気流の捻れ、つまり渦は、整流用ハニカム(2)で完全
に除去することが出来た。整流されたしかも二山形の速
度分布を持つ気流はテーパー管(3)によって雨滴の落
下速度に対応した上昇気流を連続的に実現した。
The characteristics of the velocity distribution of the air flow created by the axial fan (1) are:
The flow velocity near the central axis is smaller than the flow velocity in the peripheral region, that is, the velocity distribution of the air flow including the central axis has a double mountain shape. This feature is a necessary condition for floating raindrops near the central axis. However, the air flow of the axial fan has a twist in the axial direction and has a spiral shape. This feature is inconvenient for a stable suspension of raindrops. The twist of the air flow, that is, the vortex, could be completely removed by the rectifying honeycomb (2). The rectified airflow with a double mountain velocity distribution continuously realized an updraft corresponding to the falling velocity of raindrops by means of the taper pipe (3).

【実施例】【Example】

この考案の垂直風洞の性能を調べるために次の実験を行
った。軸流ファン(1)と整流用ハニカム(2)および
上に開いたテーパー管(3)を第1図のように鉛直に、
それぞれの中心軸を一致させて、連結した。組立を完了
した後、軸流ファンを交流100ボルトの電源に接続
し、低、中、高の三段階の回転速度で運転した。それぞ
れの回転速度に対応した風速分布を熱線風速計を用いて
測定し、さらに整流の状態はハニカムから吹き出す煙の
流れに依って調べた。垂直風洞本体の気流吹き出し口、
即ちテーパー管の入口に於ける風速の測定結果を第3図
に、さらにテーパー管の出口に於ける速度分布を第4図
に示す。二つの場所、つまりテーパー管の入口と出口に
於ける速度分布は、いずれも中心軸を含む二山形の分布
をしており、整流された捻れの無い、鉛直気流が作られ
ていることが確認された。このことから、テーパー管内
の任意な高さに於ける上昇気流の速度分布は、テーパー
管の入口と出口で測定された速度の範囲内にあることが
容易に推測できる。したがってテーパー管内の上昇気流
中で、落下速度が上昇気流の速度範囲内にある雨滴であ
れば、上昇気流の速度と落下速度が等しい位置で、浮遊
できることを示している。 この垂直風洞を用いて、等価直径(完全な球体としたと
きの直径)5mmの水滴(落下速度:9m/s)を浮かべた
ところ約20分間安定して浮遊した。この浮遊時間は、
充分に整備された研究用垂直風洞での長時間の例に相当
する。
The following experiment was conducted to investigate the performance of the vertical wind tunnel of this invention. As shown in FIG. 1, the axial fan (1), the rectifying honeycomb (2), and the taper pipe (3) opened above are vertically arranged as shown in FIG.
The respective central axes were aligned and connected. After the assembly was completed, the axial fan was connected to a power supply of 100 V AC and operated at three rotation speeds of low, medium and high. The wind speed distribution corresponding to each rotation speed was measured by using a hot wire anemometer, and the rectification state was examined by the flow of smoke blown from the honeycomb. Airflow outlet of the vertical wind tunnel body,
That is, the measurement result of the wind velocity at the inlet of the taper pipe is shown in FIG. 3, and the velocity distribution at the outlet of the taper pipe is shown in FIG. The velocity distributions at the two locations, namely at the inlet and outlet of the tapered pipe, have a bimodal distribution that includes the central axis, and it is confirmed that a rectified, non-twisted vertical airflow is created. Was done. From this, it can be easily inferred that the velocity distribution of the ascending air flow at an arbitrary height in the tapered pipe is within the velocity range measured at the inlet and outlet of the tapered pipe. Therefore, it is shown that, in the ascending airflow in the tapered tube, if the raindrop has a falling velocity within the velocity range of the ascending airflow, it can float at a position where the ascending airflow velocity and the falling velocity are equal. Using this vertical wind tunnel, a water droplet (falling speed: 9 m / s) having an equivalent diameter of 5 mm (diameter when it was a perfect sphere) was floated, and it floated stably for about 20 minutes. This floating time is
This corresponds to a long-term example in a well-equipped research vertical wind tunnel.

【考案の効果】[Effect of device]

本考案の垂直風洞は小型軽量で、しかも操作が容易且つ
安全にまとめることが出来たので、開発の当面の目的で
あった秋田地方気象台の一般公開及び気象庁主催の「お
天気フェアー」で供覧した。小学生から大人まで、参加
者のほとんど全てが興味を示し、装置を自分で操作し、
いろいろな大きさの水滴を浮かべ、気流中での水滴の形
と運動を自分の目で確認した。浮遊しているときの形状
は饅頭形であり、一般に想像されているような涙形でな
いことを容易に知らせることが出来た。雨滴は浮遊して
いる間にも水分が蒸発し、小さくなり、落下速度も小さ
くなる。その結果当初浮遊していた位置よりも上に移動
することも確認された。一つの水滴が浮遊しているとこ
ろへさらに他の一つの水滴を浮かべると互いに追いかけ
るような運動をし、やがて合体し、一つの大きな水滴と
なって浮遊した。場合に依っては小さな水滴に分裂して
気流の外に飛び出すこともあった。こうした風洞内での
一連の現象は自然の雲の中での雨滴の振舞いを再現する
ものであり、見学者の多くに科学的な興味をひきおこす
ことができた。 以上2箇所での公開実演の実績から、本考案の可搬形垂
直風洞は教育の現場に於いても、さらに研究用としても
充分活用できる見通しが得られた。
Since the vertical wind tunnel of the present invention is compact and lightweight, and can be easily and safely assembled, it was exhibited at the Akita Local Meteorological Observatory's general public and the "Weather Fair" sponsored by the Meteorological Agency, which was the immediate objective of development. From elementary school students to adults, almost all of the participants showed interest, operated the device by themselves,
Water droplets of various sizes were floated, and the shape and movement of the water droplets in the airflow were confirmed with their own eyes. The shape when it was floating was manju, and it was possible to easily inform that it was not the teardrop shape that is generally imagined. While the raindrops are floating, the water content evaporates and becomes smaller, and the falling speed becomes smaller. As a result, it was also confirmed that it would move above the initially floating position. When another water drop floats on the surface where one water drop floats, they move to follow each other, and eventually they coalesce and float as one big water drop. In some cases, it may break into small water droplets and jump out of the air stream. A series of such phenomena in the wind tunnel reproduces the behavior of raindrops in the natural clouds, and was able to bring scientific interest to many visitors. From the results of the public demonstrations at the above two locations, it is possible to obtain the prospect that the portable vertical wind tunnel of the present invention can be fully utilized not only in the field of education but also for research.

【図面の簡単な説明】[Brief description of drawings]

第1図は本考案の教育用可搬形垂直風洞の側面図、第2
図は同平面図である。図に付した番号は1……軸流ファ
ン、2……整流用ハニカム、3……テーパー管、4……
風洞パイプ、5……風洞固定枠をそれぞれ示す。第3図
はテーパー管の入口における気流の速度分布、第4図は
テーパー管の出口における気流の速度分布を示す。第4
図を第3図の上に配置してあるのは、第1図に示すテー
パー管(3)内の空気の流れが下から上に向かっている
ことに対応させたためである。第3図及び第4図のグラ
フには、軸流ファンを低、中、高速で運転したときの3
通りの速度分布をL,M,Hの記号を付けてそれぞれ示
してある。
FIG. 1 is a side view of a portable vertical wind tunnel for education according to the present invention, and FIG.
The figure is a plan view of the same. The numbers attached to the figure are 1 ... axial fan, 2 ... rectifying honeycomb, 3 ... taper tube, 4 ...
Wind tunnel pipe, 5 ... Shows the wind tunnel fixed frame, respectively. FIG. 3 shows the velocity distribution of the air flow at the inlet of the taper pipe, and FIG. 4 shows the velocity distribution of the air flow at the outlet of the taper pipe. Fourth
The reason why the drawing is arranged above FIG. 3 is that it corresponds to the air flow in the tapered pipe (3) shown in FIG. 1 going from the bottom to the top. The graphs in FIGS. 3 and 4 show 3 when the axial fan is operated at low, medium and high speeds.
The respective velocity distributions are shown with the symbols L, M, and H respectively.

Claims (1)

【実用新案登録請求の範囲】[Scope of utility model registration request] 【請求項1】軸流ファンと整流用ハニカムのみの組み合
わせを特徴とする降水粒子を浮遊させるための教育用可
搬形垂直風洞
1. A portable vertical wind tunnel for education for suspending precipitation particles, characterized by a combination of an axial fan and a rectifying honeycomb only.
JP8756590U 1990-08-22 1990-08-22 An educational portable vertical wind tunnel for suspending precipitation particles. Expired - Lifetime JPH0632602Y2 (en)

Priority Applications (1)

Application Number Priority Date Filing Date Title
JP8756590U JPH0632602Y2 (en) 1990-08-22 1990-08-22 An educational portable vertical wind tunnel for suspending precipitation particles.

Applications Claiming Priority (1)

Application Number Priority Date Filing Date Title
JP8756590U JPH0632602Y2 (en) 1990-08-22 1990-08-22 An educational portable vertical wind tunnel for suspending precipitation particles.

Publications (2)

Publication Number Publication Date
JPH0445947U JPH0445947U (en) 1992-04-20
JPH0632602Y2 true JPH0632602Y2 (en) 1994-08-24

Family

ID=31820013

Family Applications (1)

Application Number Title Priority Date Filing Date
JP8756590U Expired - Lifetime JPH0632602Y2 (en) 1990-08-22 1990-08-22 An educational portable vertical wind tunnel for suspending precipitation particles.

Country Status (1)

Country Link
JP (1) JPH0632602Y2 (en)

Also Published As

Publication number Publication date
JPH0445947U (en) 1992-04-20

Similar Documents

Publication Publication Date Title
Uehara et al. Wind tunnel experiments on how thermal stratification affects flow in and above urban street canyons
Scorer Natural Aerodynamics: International Series of Monographs on Aeronautical Sciences and Space Flight: Aerodynamics, Vol. 1
Morton Geophysical vortices
Hoydysh et al. Kinematics and dispersion characteristics of flows in asymmetric street canyons
McCormack Aerostatic spacing: on things becoming lighter than air
Mestayer et al. Spray droplet generation, transport, and evaporation in a wind wave tunnel during the humidity exchange over the sea experiments in the simulation tunnel
Fleming Wind stresses in buildings: with a chapter on earthquakes and earthquake resistance
Depaul a Study of Pollutant Dispersion in AN Urban Street Canyon.
Jones et al. Aeroform: designing for wind and air movement
Ward Temperature inversion as a factor in formation of tornadoes
Gayev et al. Flow and Transport Processes with Complex Obstructions: Applications to Cities, Vegetative Canopies and Industry
Pols et al. Hands‐on aeronautics for middle school students
CN211956881U (en) A teaching aid to demonstrate the relationship between fluid pressure and flow velocity
Abdo et al. Three dimensional simulation of ventilation flow through a solar windcatcher
Goens Fire whirls
Quackenbos A natural philosophy
Škvorc Aerodynamic characteristics of tall buildings with porous façades
JPS58105034A (en) Simulated testing method for scattering of granular substance
Atesmen Case Studies in Fluid Mechanics with Sensitivities to Governing Variables
Fletcher Mechanics of flight
BUSCH Danish Atomic Energy Commission, Research Establishment Risø, Roskilde, Denmark
Brasure An Experimental Study of the Teacher Demonstration and the Individual Laboratory Methods in the Teaching of Physics
BROWN A study of pollutant dispersal in a 2-dimensional field including gravity effects[Final Scientific Report, 30 Apr. 1983- 29 Apr. 1984]
Sauer et al. A wind tunnel study of airflow near model swine confinement buildings
Mészáros FIRE TORNADO

Legal Events

Date Code Title Description
EXPY Cancellation because of completion of term