JP2016191582A - Method for measuring moisture content ratio and moisture content percentage of soil - Google Patents

Method for measuring moisture content ratio and moisture content percentage of soil Download PDF

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JP2016191582A
JP2016191582A JP2015070789A JP2015070789A JP2016191582A JP 2016191582 A JP2016191582 A JP 2016191582A JP 2015070789 A JP2015070789 A JP 2015070789A JP 2015070789 A JP2015070789 A JP 2015070789A JP 2016191582 A JP2016191582 A JP 2016191582A
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moisture content
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water
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JP6270769B2 (en
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坂井 宏行
Hiroyuki Sakai
宏行 坂井
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Railway Technical Research Institute
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Abstract

PROBLEM TO BE SOLVED: To enable the moisture content ratio and moisture content percentage of soil to be measured easily in the scene of soil sampling.SOLUTION: A soil sample weighing A grams is put into a sucrose aqueous solution of B% in sucrose concentration and C grams in weight, and the sugar content of the stirred solution is measured with a saccharimeter or a refractometer. On the basis of the measured sugar content D%, the X-gram weight of water in the soil is calculated by the following formula (1), and further the moisture content ratio Y% or the moisture content percentage Z% of the soil is calculated by the following formulas (2) and (3). X={(B×C)/D}-C ...(1) Y={X/(A-X)}×100 ...(2) Z=(X/A)×100 ...(3)SELECTED DRAWING: Figure 1

Description

本発明は、土壌の含水比、含水率の測定方法の技術分野に関するものである。   The present invention relates to a technical field of a method for measuring moisture content and moisture content of soil.

一般に、土壌に含まれる水分の割合(含水比、含水率)を知ることは、植生の生育に対する影響、地下水の挙動、盛り土などを含めた斜面崩壊のメカニズムの解析、洪水発生予測等の研究をするにあたり重要な要素の一つであり、そのため日本工業規格としてJIS A 1203で「土の含水比試験方法」が規格されている。このものは、土壌の含水比を、採取した土壌の重量とこれを炉内で乾燥した後の重量とをそれぞれ測定することに基づいて求めるようにしている所謂炉乾燥法である。ところが土壌の乾燥には、110±5℃に保持した恒温乾燥炉内にて18〜24時間もの長時間の乾燥が必要であって作業性が悪いだけでなく、恒温乾燥炉が土壌の採取現場にあることはまずなく、採取した土壌を高温乾燥炉を備えた実験室等に持ち帰って乾燥させなければならず、また実験室まで採取時の含水比を維持したまま持ち込まなければならず、このための特別な技術と操作も必要となり、手間がかかるという問題がある。
これに対し、土壌水分の測定方法として、テンシオメータ法(特許文献1参照)、誘電法(特許文献2参照)、電気抵抗法(特許文献3参照)、熱伝導法(特許文献4参照)、電磁波法(特許文献5参照)等の多くの手法が知られている。
In general, knowing the proportion of water in the soil (water content, water content) is important for research on impacts on vegetation growth, groundwater behavior, analysis of slope failure mechanisms including embankments, and prediction of flood occurrence. Therefore, it is one of the important factors, and as a result, the JIS A 1203 “Soil moisture content test method” is standardized as a Japanese Industrial Standard. This is a so-called furnace drying method in which the moisture content of soil is determined based on measuring the weight of the collected soil and the weight after drying the soil in the furnace. However, soil drying requires a long drying time of 18 to 24 hours in a constant temperature drying furnace maintained at 110 ± 5 ° C., and not only is the workability poor, but the constant temperature drying furnace is used for soil sampling. The collected soil must be brought back to a laboratory equipped with a high-temperature drying furnace and dried, and brought to the laboratory while maintaining the moisture content at the time of collection. Therefore, there is a problem that special techniques and operations are necessary and time-consuming.
On the other hand, as a method for measuring soil moisture, tensiometer method (see Patent Document 1), dielectric method (see Patent Document 2), electric resistance method (see Patent Document 3), heat conduction method (see Patent Document 4), electromagnetic wave Many methods such as the method (see Patent Document 5) are known.

特開平7−244040号公報Japanese Patent Laid-Open No. 7-244040 特許第2913022号公報Japanese Patent No. 2913022 特開2004−77353号公報JP 2004-77353 A 特開2006−194821号公報JP 2006-194421 A 特開2009−98018号公報JP 2009-98018 A

しかしながら前記従来のもののうち、特許文献1、2、5のものは装置自体が大型であるうえ、土壌に埋設しなければならず、作業性が劣る、という問題がある。これに対し特許文献3、4のものはセンサ自体を小型にできる、という利点があるが、予め採取した土壌を乾燥させて該乾燥土壌における電気抵抗値や熱伝導率を測定し、さらに該乾燥土壌に所要量の水分を含浸させたものの幾つかについて電気抵抗値や熱伝導率を測定して検量線を作成する必要があるが、土質が異なった場合に同じ検量線を採用できるとは限らず、そのため土質が異なる測定現場ごとにこれらの検量線をいちいち作成しなければならないこともあって面倒かつ煩雑であるという問題がある。さらに、特許文献1〜5のものは、実験室まで採取時の含水比を維持したまま土壌を持ち込まなければならない点は依然として解決されておらず、ここに本発明の解決すべき課題がある。   However, among the above-mentioned conventional ones, Patent Documents 1, 2, and 5 have a problem that the apparatus itself is large and must be embedded in soil, resulting in poor workability. On the other hand, Patent Documents 3 and 4 have the advantage that the sensor itself can be reduced in size, but the previously collected soil is dried to measure the electrical resistance value and thermal conductivity in the dried soil, and then the dried It is necessary to create a calibration curve by measuring the electrical resistance and thermal conductivity of some of the soil impregnated with the required amount of water, but the same calibration curve may not be used when the soil is different. Therefore, there is a problem that these calibration curves must be prepared for each measurement site having different soil properties, which is troublesome and complicated. Further, in Patent Documents 1 to 5, the point that the soil must be brought into the laboratory while maintaining the water content ratio at the time of collection is still unsolved, and there is a problem to be solved by the present invention.

本発明は、上記の如き実情に鑑みこれらの課題を解決することを目的として創作されたものであって、請求項1の発明は、土壌の含水比の測定方法であって、採取した重量Aグラムの土壌を、ショ糖濃度(重量%濃度)B%、重量Cグラムのショ糖水溶液に入れ、撹拌後、濾過して得た溶液の糖度を糖度計または屈折率計により測定し、該測定した糖度D%に基づき、下記式(1)を用いて前記採取した重量Aグラムの土壌中の水の重量Xグラムを演算し、さらに下記式(2)を用いて土壌の含水比Y%を演算するようにしたことを特徴とする土壌の含水比の測定方法である。
X={(B×C)/D}−C ・・・(1)
Y={X/(A−X)}×100 ・・・(2)
請求項2の発明は、土壌の含水比の測定方法であって、採取した重量Aグラムの土壌を、ショ糖濃度(重量%濃度)B%、重量Cグラムのショ糖水溶液に入れ、撹拌して得た溶液の糖度を糖度計または屈折率計により測定し、該測定した糖度D%に基づき、下記式(1)を用いて前記採取した重量Aグラムの土壌中の水の重量Xグラムを演算し、さらに下記式(2)を用いて土壌の含水比Y%を演算するようにしたことを特徴とする土壌の含水比の測定方法である。
X={(B×C)/D}−C ・・・(1)
Y={X/(A−X)}×100 ・・・(2)
請求項3の発明は、請求項1または2において、糖度計または屈折率計により測定した溶液の糖度を、ショ糖水溶液の作製に使用した水と土壌とを用いたブランクテストにより補正することを特徴とする土壌の含水比の測定方法である。
請求項4の発明は、土壌の含水率の測定方法であって、採取した重量Aグラムの土壌を、ショ糖濃度(重量%濃度)B%、重量Cグラムのショ糖水溶液に入れ、撹拌後、濾過して得た溶液の糖度を糖度計または屈折率計により測定し、該測定した糖度D%に基づき、下記式(1)を用いて前記採取した重量Aグラムの土壌中の水の重量Xグラムを演算し、さらに下記式(3)を用いて土壌の含水率Z%を演算するようにしたことを特徴とする土壌の含水率の測定方法である。
X={(B×C)/D}−C ・・・(1)
Z=(X/A)×100 ・・・(3)
請求項5の発明は、土壌の含水率の測定方法であって、採取した重量Aグラムの土壌を、ショ糖濃度(重量%濃度)B%、重量Cグラムのショ糖水溶液に入れ、撹拌して得た溶液の糖度を糖度計または屈折率計により測定し、該測定した糖度D%に基づき、下記式(1)を用いて前記採取した重量Aグラムの土壌中の水の重量Xグラムを演算し、さらに下記式(3)を用いて土壌の含水率Z%を演算するようにしたことを特徴とする土壌の含水率の測定方法である。
X={(B×C)/D}−C ・・・(1)
Z=(X/A)×100 ・・・(3)
請求項6の発明は、請求項4または5において、糖度計または屈折率計により測定した溶液の糖度を、ショ糖水溶液の作製に使用した水と土壌とを用いたブランクテストにより補正することを特徴とする土壌の含水率の測定方法である。
The present invention was created with the object of solving these problems in view of the above-mentioned circumstances, and the invention of claim 1 is a method for measuring the moisture content of soil, and the collected weight A Gram soil is put into a sucrose aqueous solution with a sucrose concentration (weight% concentration) B% and a weight C gram, and after stirring, the sugar content of the solution obtained by filtration is measured with a saccharimeter or a refractometer. Based on the sugar content D%, the weight X gram of water in the soil of the collected weight A gram was calculated using the following formula (1), and the water content ratio Y% of the soil was further calculated using the following formula (2). It is a method for measuring the moisture content of soil, characterized in that it is calculated.
X = {(B × C) / D} −C (1)
Y = {X / (A−X)} × 100 (2)
The invention of claim 2 is a method for measuring the water content ratio of soil, wherein the collected soil having a weight of A gram is placed in a sucrose aqueous solution having a sucrose concentration (weight% concentration) of B% and a weight of C gram and stirred. The sugar content of the solution obtained above was measured with a saccharimeter or a refractometer, and based on the measured sugar content D%, the weight X grams of water in the soil of the weight A gram collected using the following formula (1) was calculated. The soil moisture content measurement method is characterized in that the soil moisture content Y% is calculated using the following formula (2).
X = {(B × C) / D} −C (1)
Y = {X / (A−X)} × 100 (2)
The invention of claim 3 is that in claim 1 or 2, the sugar content of the solution measured by a saccharimeter or a refractometer is corrected by a blank test using water and soil used to prepare a sucrose aqueous solution. This is a characteristic method for measuring the moisture content of soil.
The invention according to claim 4 is a method for measuring the moisture content of soil, wherein the collected soil having a weight of A gram is put into a sucrose aqueous solution having a sucrose concentration (weight% concentration) of B% and a weight of C gram, followed by stirring. The sugar content of the solution obtained by filtration is measured with a saccharimeter or a refractometer, and the weight of water in the soil of the weight A gram collected using the following formula (1) based on the measured sugar content D% The soil moisture content measurement method is characterized in that X gram is calculated and the soil moisture content Z% is calculated using the following equation (3).
X = {(B × C) / D} −C (1)
Z = (X / A) × 100 (3)
The invention of claim 5 is a method for measuring the moisture content of soil, wherein the collected soil having a weight of A gram is placed in a sucrose aqueous solution having a sucrose concentration (weight% concentration) of B% and a weight of C gram and stirred. The sugar content of the solution obtained above was measured with a saccharimeter or a refractometer, and based on the measured sugar content D%, the weight X grams of water in the soil of the weight A gram collected using the following formula (1) was calculated. The soil moisture content measurement method is characterized in that the soil moisture content Z% is calculated using the following equation (3).
X = {(B × C) / D} −C (1)
Z = (X / A) × 100 (3)
The invention of claim 6 is the method according to claim 4 or 5, wherein the sugar content of the solution measured by a saccharimeter or a refractometer is corrected by a blank test using water and soil used for preparing a sucrose aqueous solution. This is a characteristic method for measuring the moisture content of soil.

請求項1、2の発明とすることにより、土壌の含水比を、土壌採取現場においても簡単に求めることができる。
請求項3の発明とすることにより、より正確な含水比を求めることができる。
請求項4、5の発明とすることにより、土壌の含水率を、土壌採取現場においても簡単に求めることができる。
請求項6の発明とすることにより、より正確な含水比を求めることができる。
By setting it as invention of Claim 1, 2, the moisture content of a soil can be calculated | required easily also in the soil collection field.
By setting it as invention of Claim 3, a more exact water content ratio can be calculated | required.
By setting it as invention of Claim 4, 5, the moisture content of a soil can be calculated | required easily also in the soil collection field.
By setting it as invention of Claim 6, a more exact water content ratio can be calculated | required.

土壌の含水比、含水率の測定方法を示すフロー図である。It is a flowchart which shows the measuring method of the moisture content of a soil, and a moisture content.

以下、本発明の実施の形態について説明する。
本実施の形態では、糖度の測定に糖度計を用いているが、ショ糖水溶液の糖度(Brix)と屈折率とは換算表等を用いて簡単に換算することができるため、屈折率計によって屈折率を測定し、該測定した屈折率を糖度に換算することで糖度を測定するようにしても良い。つまり、本発明における糖度の測定は、糖度計により直接糖度を測定した場合だけでなく、屈折率計により屈折率を測定し、該測定した屈折率を糖度に換算した場合も含める。
本発明は、ショ糖水溶液の屈折率を基準値として水溶液の糖度(Brix)を測定する糖度計(屈折糖度計)、或いは水溶液の屈折率を測定する屈折率計が広く知られているが、このような糖度計により測定されるショ糖水溶液の糖度、或いは屈折率計により測定される屈折率を糖度に換算して求めたショ糖水溶液の糖度は、該ショ糖水溶液のショ糖濃度(重量%濃度)を示す値であるから、糖度計あるいは屈折率計を用いてショ糖水溶液のショ糖濃度を簡単且つ正確に測定できることを利用して、土壌の含水比、含水率を測定しようとするものである。
この測定に用いるショ糖(シュークロース:sucrose)は、水に対する溶解度が211.5g/100mL(20℃)もあって溶解しやすいものであり、土壌中の水分にも容易に溶解する。そのうえショ糖は、人体や自然環境に対して無害であるため、測定後、ショ糖水溶液を測定現場に廃棄しても環境上問題になることがない。
さらに、本実施の形態では、土壌の含水比、含水率を測定するにあたり、糖度計または糖度計により測定された糖度を、ショ糖水溶液の作製に使用した水と土壌とを用いたブランクテストにより補正する。これにより、ショ糖水溶液の作製に使用した水や土壌に糖度の測定値に影響を与える物質が含まれていても、該物質の有無や多少に関わらず、土壌の含水比、含水率を正確に測定することができる。尚、以下の説明において、ショ糖濃度は全て重量%濃度である。
Embodiments of the present invention will be described below.
In this embodiment, a saccharimeter is used to measure the saccharide content, but the saccharose aqueous solution (Brix) and the refractive index can be easily converted using a conversion table or the like. You may make it measure sugar content by measuring a refractive index and converting this measured refractive index into sugar content. That is, the measurement of the sugar content in the present invention includes not only the case where the sugar content is directly measured by a saccharimeter, but also the case where the refractive index is measured by a refractometer and the measured refractive index is converted to a sugar content.
In the present invention, a saccharimeter (refractive saccharimeter) for measuring the sugar content (Brix) of an aqueous solution with the refractive index of the sucrose aqueous solution as a reference value, or a refractometer for measuring the refractive index of an aqueous solution is widely known. The sugar content of the aqueous sucrose solution measured by such a sugar content meter or the sugar content of the aqueous solution of sucrose obtained by converting the refractive index measured by a refractometer into sugar content is determined by the sucrose concentration (weight) of the aqueous solution of sucrose. % Sucrose concentration and refractometer, it is possible to measure the sucrose concentration of sucrose aqueous solution easily and accurately using a saccharimeter or refractometer, and try to measure the water content ratio and water content of the soil. Is.
Sucrose (sucrose) used for this measurement has a solubility in water of 211.5 g / 100 mL (20 ° C.) and is easily dissolved, and is easily dissolved in moisture in the soil. In addition, since sucrose is harmless to the human body and the natural environment, even if the sucrose aqueous solution is discarded at the measurement site after measurement, there is no environmental problem.
Furthermore, in the present embodiment, when measuring the water content ratio and moisture content of the soil, the sugar content measured by the saccharimeter or the saccharimeter is measured by a blank test using the water and soil used to prepare the sucrose aqueous solution. to correct. As a result, even if the water or soil used to prepare the aqueous sucrose solution contains a substance that affects the measured value of sugar content, the water content ratio and water content of the soil can be accurately determined regardless of the presence or absence of the substance. Can be measured. In the following description, all sucrose concentrations are weight% concentrations.

図1に土壌の含水比Y%或いは含水率Z%を測定する手順をフロー図で示すが、まず、現場で重量Aグラムの土壌試料を採取する。そして、採取した重量Aグラムの土壌試料を、ショ糖濃度B%、重量Cグラムのショ糖水溶液に入れて、よく撹拌した後に濾過する。この場合、ショ糖水溶液は、作製したものを現場に持参しても良いが、現地調達した水(地下水、井戸水、河川水、湧水、水道水等、土壌採取の現地で調達できる水であって、成分未調整の水)を用いて現場でショ糖水溶液を作製しても良い。該ショ糖水溶液のショ糖濃度B%は、土壌の湿潤状態を見て適宜(例えば、ショ糖濃度10%〜60%)決定する。また、濾過する際のフィルターとしては、水が浸潤しない材料で製造したものが好ましく、例えばガラス製やシリコーン、ポリテトラフルオロエチレンのような合成樹脂製等のものが採用される。
次いで、前記撹拌後に濾過して得られた溶液(該溶液を、以降、試料溶液と称する)の糖度D%を糖度計により測定する。糖度の測定は、市販されている汎用の糖度計(屈折糖度計)を用いて行うことができる。この場合に、携帯型であれば現場に簡単に持参でき、都合がよい。また、前述したように、糖度計に代えて屈折計により屈折率を測定し、該屈折率から糖度を求めても良い。
FIG. 1 is a flowchart showing a procedure for measuring the moisture content Y% or the moisture content Z% of the soil. First, a soil sample having a weight of A gram is collected on site. Then, the collected soil sample having a weight of A gram is put into a sucrose aqueous solution having a sucrose concentration of B% and a weight of C gram, and is stirred and filtered. In this case, the sucrose aqueous solution may be brought to the site. However, locally procured water (ground water, well water, river water, spring water, tap water, etc.) is water that can be procured locally. In addition, an aqueous sucrose solution may be prepared on site using water that has not yet been adjusted. The sucrose concentration B% of the sucrose aqueous solution is appropriately determined (for example, sucrose concentration 10% to 60%) in view of the wet state of the soil. Moreover, as a filter at the time of filtering, what was manufactured with the material which water does not infiltrate is preferable, for example, the thing made from synthetic resin like glass, silicone, polytetrafluoroethylene, etc. are employ | adopted.
Next, the sugar content D% of the solution obtained by filtration after the stirring (this solution is hereinafter referred to as a sample solution) is measured with a saccharimeter. The sugar content can be measured using a commercially available general-purpose sugar content meter (refractive sugar content meter). In this case, if it is a portable type, it can be easily brought to the site and is convenient. Further, as described above, the refractive index may be measured by a refractometer instead of the saccharimeter, and the saccharide degree may be obtained from the refractive index.

そして、該測定した糖度D%に基づき、下記の式(1)を用いて、前記採取した重量Aグラムの土壌中の水の重量Xグラムを演算する。
X={(B×C)/D}−C ・・・(1)
尚、ショ糖水溶液の作製に用いた水や土壌中に、糖度の測定値に影響を与える物質が含まれていると考えられる場合(例えば、ショ糖水溶液の作製に現地調達した成分未調整の水を用いた場合)には、後述するように、前記糖度計により測定した糖度D%に代えて補正糖度Dhを用いる。
さらに、前記式(1)で演算された土壌中の水の重量Xグラムに基づき、下記式(2)を用いて、採取した土壌の含水比Y%((土壌中の水の重量/土壌中の乾燥土壌の重量)×100%)を演算する。或いは、下記の式(3)を用いて、採取した土壌の含水率Z%((土壌中の水の重量/土壌の重量)×100%)を演算する。
Y={X/(A−X)}×100 ・・・(2)
Z=(X/A)×100 ・・・(3)
Then, based on the measured sugar content D%, the weight X gram of water in the soil of the collected weight A gram is calculated using the following formula (1).
X = {(B × C) / D} −C (1)
In addition, when it is thought that the substance which affects the measured value of sugar content is contained in the water and soil used for the preparation of the sucrose aqueous solution (for example, the unadjusted ingredients procured locally for the preparation of the sucrose aqueous solution) In the case of using water), as will be described later, the corrected sugar content Dh is used instead of the sugar content D% measured by the sugar content meter.
Further, based on the weight X grams of water in the soil calculated by the above formula (1), using the following formula (2), the moisture content Y% of the collected soil ((weight of water in soil / in soil) The dry soil weight) × 100%) is calculated. Alternatively, the moisture content Z% ((weight of water in soil / weight of soil) × 100%) of the collected soil is calculated using the following formula (3).
Y = {X / (A−X)} × 100 (2)
Z = (X / A) × 100 (3)

ここで、上記式(1)、(2)、(3)および後述する式(4)、(5)、(6)において、
A:採取した土壌の重量(グラム)
B:ショ糖水溶液のショ糖濃度(%)
C:ショ糖水溶液の重量(グラム)
D:試料溶液の糖度(%)
E:ショ糖水溶液中のショ糖の重量(グラム)
F:試料溶液のショ糖濃度(%)
X:土壌中の水の重量(グラム)
Y:土壌の含水比(%)
Z:土壌の含水率(%)
である。
Here, in the above formulas (1), (2), (3) and formulas (4), (5), (6) described later,
A: Weight of collected soil (gram)
B: Sucrose concentration in sucrose aqueous solution (%)
C: Weight of sucrose aqueous solution (gram)
D: Sugar content (%) of sample solution
E: Weight of sucrose in sucrose aqueous solution (gram)
F: Sucrose concentration of sample solution (%)
X: Weight of water in the soil (gram)
Y: Soil moisture content (%)
Z: Moisture content of soil (%)
It is.

具体的には、例えば、50mLのプラスチック製試験管またはバッグ等の容器に土壌試料15グラムを入れ、このものに、ショ糖濃度が50%のショ糖水溶液を15グラム入れてよく振盪(例えば2分間)し、この溶液を濾過(例えば孔径0.45μmのフィルター)して得られた試料溶液の糖度を糖度計により測定し、該測定した糖度D%に基づき、前記式(1)を用いて採取した土壌中の水の重量Xグラムを演算し、さらに前記式(2)或いは(3)を用いて採取した土壌の含水比Y%或いは含水率Z%を演算する。
尚、土壌試料に含まれる粘土分が少ない場合など、ショ糖水溶液と振盪後に得られた溶液の濁度が低い場合には濾過を省略することができ、たいていの土壌試料においては濾過を省略して差し支えない。
Specifically, for example, a soil sample of 15 grams is put in a 50 mL plastic test tube or a container such as a bag, and 15 grams of a sucrose aqueous solution having a sucrose concentration of 50% is put in this sample and shaken (for example, 2 The sugar content of the sample solution obtained by filtering this solution (for example, a filter having a pore diameter of 0.45 μm) is measured with a saccharimeter, and the above formula (1) is used based on the measured sugar content D%. The weight X gram of water in the collected soil is calculated, and the water content ratio Y% or the water content Z% of the soil sampled is calculated using the formula (2) or (3).
Note that filtration can be omitted when the aqueous solution of sucrose and the solution obtained after shaking are low, such as when the soil sample contains a small amount of clay, and filtration is omitted for most soil samples. It does not matter.

前記式(1)は、以下のようにして導き出される。
まず、ショ糖濃度B%、重量Cグラムのショ糖水溶液中のショ糖の重量Eグラムは、以下の式(4)で表される。
E=B×C/100 ・・・(4)
一方、土壌とショ糖水溶液とを撹拌濾過して得られた試料溶液は、ショ糖水溶液のショ糖濃度が土壌中に含まれていた水分によって希釈された状態であって、そのショ糖濃度F%は、下記の式(5)によって表される。
F={E/(C+X)}×100 ・・・(5)
ここで、糖度計により測定される糖度はショ糖濃度を示す値であるから、試料溶液の糖度D%は試料溶液のショ糖濃度F%と等しく(F=D)、前記式(5)のFをDに置き換えると以下の式(6)が成立する。
D={E/(C+X)}×100 ・・・(6)
そして、前記式(6)中のEに式(4)の右辺を代入して整理することにより、前記式(1)が導かれる。
さらに、式(1)により演算されるXは土壌中の水の重量であり、土壌の重量Aグラムは測定により判明しているから、前記式(2)、(3)を用いて土壌の含水比Y%、含水率Z%を演算することができる。
The formula (1) is derived as follows.
First, a weight E gram of sucrose in a sucrose aqueous solution having a sucrose concentration of B% and a weight C gram is represented by the following formula (4).
E = B × C / 100 (4)
On the other hand, the sample solution obtained by stirring and filtering the soil and the aqueous sucrose solution is in a state in which the sucrose concentration of the aqueous sucrose solution is diluted with water contained in the soil, and the sucrose concentration F % Is represented by the following formula (5).
F = {E / (C + X)} × 100 (5)
Here, since the sugar content measured by the sugar content meter is a value indicating the sucrose concentration, the sugar content D% of the sample solution is equal to the sucrose concentration F% of the sample solution (F = D), and the equation (5) When F is replaced with D, the following equation (6) is established.
D = {E / (C + X)} × 100 (6)
Then, by substituting the right side of Expression (4) for E in Expression (6) and rearranging, Expression (1) is derived.
Further, X calculated by the formula (1) is the weight of water in the soil, and the weight A gram of the soil is known from the measurement. Therefore, the water content of the soil is calculated using the formulas (2) and (3). The ratio Y% and the moisture content Z% can be calculated.

ところで、前記式(1)、(2)、(3)を用いて土壌の含水比、含水率を演算するにあたり、式(1)を導くための式(6)が成立するには、糖度計により測定された試料溶液の糖度D%が試料溶液のショ糖濃度F%と等しいことが前提となる。このため、ショ糖水溶液の作製に用いた水や土壌中に、糖度の測定値に影響する物質が含まれていない場合、あるいは含まれていても微量であって誤差範囲内である場合には問題ないが、試料溶液の糖度の測定値に影響する物質が微量以上含まれていると、糖度計により測定される試料溶液の糖度が、実際の試料溶液のショ糖濃度よりも大きく測定されてしまい、正確な含水比、含水率を演算できないことがある。そこで、これに対処するため、本実施の形態では、ブランクテストにより糖度計で測定される試料溶液の糖度の値を補正する。   By the way, in calculating the water content ratio and water content of the soil using the above formulas (1), (2), and (3), in order to establish the formula (6) for deriving the formula (1), It is assumed that the sugar content D% of the sample solution measured by the above is equal to the sucrose concentration F% of the sample solution. Therefore, if the water or soil used to make the aqueous sucrose solution does not contain substances that affect the measured value of sugar content, or if they are contained, they are in trace amounts and within the error range. No problem, but if there is a trace amount of substances that affect the measured sugar content of the sample solution, the sugar content of the sample solution measured by the saccharimeter is measured to be greater than the sucrose concentration of the actual sample solution. As a result, accurate moisture content and moisture content may not be calculated. Therefore, in order to cope with this, in the present embodiment, the value of the sugar content of the sample solution measured with a saccharimeter is corrected by a blank test.

前記ブランクテストにより試料溶液の糖度の値の補正を行う場合には、重量Aグラムの土壌を、ショ糖濃度B%、重量Cグラムのショ糖水溶液の作製に用いた水と同じ水(重量(C×(100−B)/100)グラム)に入れ、撹拌後、濾過して得た水の糖度を測定し、該測定した糖度E%をブランクとする。そして、以下の式(7)に示すように、測定した試料溶液の糖度D%から上記ブランクE%を減じ、該減じた値を、試料溶液の補正糖度Dh%とする。
Dh=D−E ・・・(7)
そして、以下の式(8)に示すように、前記式(1)における試料溶液の糖度D%に替えて補正糖度Dh%を用いて、土壌中の水の重量Xグラムを演算する。
X={(B×C)/Dh}−C ・・・(8)
さらに、上記式(8)で演算されたXの値を用いて、前記式(2)、(3)により土壌中の含水比Y%、含水率Z%を演算する。
ここで、上記式(7)、(8)において、
B:ショ糖水溶液のショ糖濃度(%)
C:ショ糖水溶液の重量(グラム)
D:試料溶液の糖度(%)
Dh:試料溶液の補正糖度(%)
E:ブランク(%)
X:土壌中の水の重量(グラム)
である。
そして、このようにブランクテストにより糖度計で測定された試料溶液の糖度の値を補正することにより、ショ糖水溶液の作製に用いた水や土壌中に試料溶液の糖度の測定値に影響する物質が含まれていても、該物質の有無や多少を気にすることなく、土壌の含水比、含水率を正確に測定することができる。
When the sugar content of the sample solution is corrected by the blank test, the weight of A gram of soil is the same as the water used for the preparation of the sucrose aqueous solution having a sucrose concentration of B% and a weight of C gram (weight ( C × (100-B) / 100) grams), and after stirring, the sugar content of the water obtained by filtration is measured, and the measured sugar content E% is used as a blank. Then, as shown in the following formula (7), the blank E% is subtracted from the sugar content D% of the measured sample solution, and the reduced value is used as the corrected sugar content Dh% of the sample solution.
Dh = DE (7)
Then, as shown in the following formula (8), the weight X gram of water in the soil is calculated using the corrected sugar level Dh% instead of the sugar level D% of the sample solution in the formula (1).
X = {(B × C) / Dh} −C (8)
Furthermore, using the value of X calculated by the above equation (8), the water content ratio Y% and the water content Z% in the soil are calculated by the above equations (2) and (3).
Here, in the above formulas (7) and (8),
B: Sucrose concentration in sucrose aqueous solution (%)
C: Weight of sucrose aqueous solution (gram)
D: Sugar content (%) of sample solution
Dh: Corrected sugar content (%) of the sample solution
E: Blank (%)
X: Weight of water in the soil (gram)
It is.
And, by correcting the sugar content value of the sample solution measured with the saccharimeter by the blank test in this way, substances that affect the measured value of the sugar content of the sample solution in the water or soil used to prepare the aqueous sucrose solution Even if it is contained, the moisture content and moisture content of the soil can be accurately measured without worrying about the presence or absence of the substance.

このように本発明が実施されたものにおいては、採取した重量Aグラムの土壌を、ショ糖濃度B%、重量Cグラムのショ糖水溶液に入れ、撹拌後、濾過して得た溶液の糖度を糖度計または屈折率計により測定し、該測定した糖度D%に基づき、前記式(1)を用いて前記採取した重量Aグラムの土壌中の水の重量Xグラムを演算し、さらに前記式(2)、(3)を用いて土壌中の含水比Y%、含水率X%を演算するようにしたものであるから、土壌の採取現場においても土壌中の含水比、含水率を短時間のうちに簡単に求めることができる。而して、実験室まで採取時の含水比、含水率を維持したまま土壌を持ち込む必要がないうえ、従来のような面倒な作業や検量線の作成も不要になって、含水比、含水率の測定作業の効率を大幅に向上させることができる。
尚、この場合に、濾過操作は場合によっては省略することができるのは前述のとおりである。
また、糖度の測定は、糖度計により直接糖度を測定する場合だけでなく、屈折率計により屈折率を測定し、該測定した屈折率を糖度に換算する場合も含めることも、前述のとおりである。
しかもショ糖は人体や自然環境に対して無害であるため、測定後、採取現場に廃棄しても公害等の問題が発生することがなく、グリセリンのように、消防法の適用を受けることもなく、調達や管理が容易である。
In the case where the present invention has been carried out in this manner, the collected weight A gram of soil is put into a sucrose aqueous solution having a sucrose concentration of B% and a weight C gram, and after stirring, the sugar content of the obtained solution is filtered. Measured with a saccharimeter or a refractometer, and based on the measured sugar content D%, the weight (g) of water in the soil of the collected weight (A gram) was calculated using the formula (1). 2) Since the moisture content Y% and moisture content X% in the soil are calculated using (3), the moisture content and moisture content in the soil can be reduced in a short time even at the soil sampling site. You can easily ask for it. Therefore, it is not necessary to bring the soil to the laboratory while maintaining the moisture content and moisture content at the time of sampling, and it is no longer necessary to create laborious work and calibration curves as in the past. The efficiency of the measurement work can be greatly improved.
In this case, as described above, the filtering operation can be omitted in some cases.
In addition, the measurement of the sugar content includes not only the case where the sugar content is directly measured by a sugar content meter, but also the case where the refractive index is measured by a refractometer and the measured refractive index is converted into the sugar content as described above. is there.
In addition, since sucrose is harmless to the human body and the natural environment, there is no problem of pollution even if it is discarded at the collection site after measurement. It is easy to procure and manage.

さらにこのものにおいて、糖度計または屈折率計により測定した溶液の糖度D%を、ショ糖水溶液の作製に使用した水と土壌とを用いたブランクテストにより補正し、該補正した糖度Dhに基づいて含水比、含水率を演算することにより、ショ糖水溶液の作製に使用した水や土壌中に糖度の測定値に影響する物質が含まれていても、該物質の有無や多少を気にすることなく、土壌の含水比、含水率をより正確に測定することができる。   Furthermore, in this, the sugar content D% of the solution measured by a saccharimeter or a refractometer is corrected by a blank test using water and soil used for the preparation of the sucrose aqueous solution, and based on the corrected saccharide content Dh. By calculating the water content and water content, even if the water or soil used to prepare the sucrose aqueous solution contains substances that affect the measured sugar content, the presence or absence of the substances should be considered. In addition, the water content ratio and water content of the soil can be measured more accurately.

本発明は、土壌中の含水比、含水率を測定する場合に利用することができる。
The present invention can be used when measuring the moisture content and moisture content in soil.

Claims (6)

土壌の含水比の測定方法であって、採取した重量Aグラムの土壌を、ショ糖濃度(重量%濃度)B%、重量Cグラムのショ糖水溶液に入れ、撹拌後、濾過して得た溶液の糖度を糖度計または屈折率計により測定し、該測定した糖度D%に基づき、下記式(1)を用いて前記採取した重量Aグラムの土壌中の水の重量Xグラムを演算し、さらに下記式(2)を用いて土壌の含水比Y%を演算するようにしたことを特徴とする土壌の含水比の測定方法。
X={(B×C)/D}−C ・・・(1)
Y={X/(A−X)}×100 ・・・(2)
A method for measuring the water content ratio of soil, in which a collected weight of gram of soil is placed in a sucrose aqueous solution having a sucrose concentration (weight% concentration) of B% and a weight of C gram, stirred and then filtered. The sugar content is measured by a sugar content meter or a refractometer, and based on the measured sugar content D%, the weight X grams of water in the soil of the collected weight A grams is calculated using the following formula (1). A method for measuring the moisture content of soil, wherein the moisture content Y% of the soil is calculated using the following formula (2).
X = {(B × C) / D} −C (1)
Y = {X / (A−X)} × 100 (2)
土壌の含水比の測定方法であって、採取した重量Aグラムの土壌を、ショ糖濃度(重量%濃度)B%、重量Cグラムのショ糖水溶液に入れ、撹拌して得た溶液の糖度を糖度計または屈折率計により測定し、該測定した糖度D%に基づき、下記式(1)を用いて前記採取した重量Aグラムの土壌中の水の重量Xグラムを演算し、さらに下記式(2)を用いて土壌の含水比Y%を演算するようにしたことを特徴とする土壌の含水比の測定方法。
X={(B×C)/D}−C ・・・(1)
Y={X/(A−X)}×100 ・・・(2)
A method for measuring the moisture content of soil, wherein the collected weight A gram of soil is placed in a sucrose aqueous solution having a sucrose concentration (weight% concentration) B% and a weight C gram, and the sugar content of the solution obtained by stirring is determined. Measured with a saccharimeter or a refractometer, and based on the measured sugar content D%, the weight X gram of water in the soil of the collected weight A gram was calculated using the following formula (1). A method for measuring the moisture content of soil, wherein the moisture content Y% of the soil is calculated using 2).
X = {(B × C) / D} −C (1)
Y = {X / (A−X)} × 100 (2)
請求項1または2において、糖度計または屈折率計により測定した溶液の糖度を、ショ糖水溶液の作製に使用した水と土壌とを用いたブランクテストにより補正することを特徴とする土壌の含水比の測定方法。   The water content ratio of the soil according to claim 1 or 2, wherein the sugar content of the solution measured by a saccharimeter or a refractometer is corrected by a blank test using water and soil used for preparing a sucrose aqueous solution. Measuring method. 土壌の含水率の測定方法であって、採取した重量Aグラムの土壌を、ショ糖濃度(重量%濃度)B%、重量Cグラムのショ糖水溶液に入れ、撹拌後、濾過して得た溶液の糖度を糖度計または屈折率計により測定し、該測定した糖度D%に基づき、下記式(1)を用いて前記採取した重量Aグラムの土壌中の水の重量Xグラムを演算し、さらに下記式(3)を用いて土壌の含水率Z%を演算するようにしたことを特徴とする土壌の含水率の測定方法。
X={(B×C)/D}−C ・・・(1)
Z=(X/A)×100 ・・・(3)
A method for measuring the moisture content of soil, in which a sample of A gram of soil collected is placed in an aqueous sucrose solution having a sucrose concentration (wt% concentration) of B% and a weight of C gram, stirred and then filtered. The sugar content is measured by a sugar content meter or a refractometer, and based on the measured sugar content D%, the weight X grams of water in the soil of the collected weight A grams is calculated using the following formula (1). A method for measuring the moisture content of soil, wherein the moisture content Z% of the soil is calculated using the following formula (3).
X = {(B × C) / D} −C (1)
Z = (X / A) × 100 (3)
土壌の含水率の測定方法であって、採取した重量Aグラムの土壌を、ショ糖濃度(重量%濃度)B%、重量Cグラムのショ糖水溶液に入れ、撹拌して得た溶液の糖度を糖度計または屈折率計により測定し、該測定した糖度D%に基づき、下記式(1)を用いて前記採取した重量Aグラムの土壌中の水の重量Xグラムを演算し、さらに下記式(3)を用いて土壌の含水率Z%を演算するようにしたことを特徴とする土壌の含水率の測定方法。
X={(B×C)/D}−C ・・・(1)
Z=(X/A)×100 ・・・(3)
A method for measuring the moisture content of soil, wherein the collected weight A gram of soil is placed in a sucrose aqueous solution having a sucrose concentration (weight% concentration) B% and a weight C gram, and the sugar content of the solution obtained by stirring is determined. Measured with a saccharimeter or a refractometer, and based on the measured sugar content D%, the weight X gram of water in the soil of the collected weight A gram was calculated using the following formula (1). A method for measuring the moisture content of soil, characterized in that the moisture content Z% of the soil is calculated using 3).
X = {(B × C) / D} −C (1)
Z = (X / A) × 100 (3)
請求項4または5において、糖度計または屈折率計により測定した溶液の糖度を、ショ糖水溶液の作製に使用した水と土壌とを用いたブランクテストにより補正することを特徴とする土壌の含水率の測定方法。   The moisture content of the soil according to claim 4 or 5, wherein the sugar content of the solution measured by a saccharimeter or a refractometer is corrected by a blank test using water and soil used for preparing the sucrose aqueous solution. Measuring method.
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