JPH02256718A - Bedrock slope face tree-planting material and bedrock slope face tree-planting method - Google Patents
Bedrock slope face tree-planting material and bedrock slope face tree-planting methodInfo
- Publication number
- JPH02256718A JPH02256718A JP7489089A JP7489089A JPH02256718A JP H02256718 A JPH02256718 A JP H02256718A JP 7489089 A JP7489089 A JP 7489089A JP 7489089 A JP7489089 A JP 7489089A JP H02256718 A JPH02256718 A JP H02256718A
- Authority
- JP
- Japan
- Prior art keywords
- soil
- bedrock
- organic material
- slope
- capacity
- 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.)
- Granted
Links
- 239000000463 material Substances 0.000 title claims abstract description 33
- 238000000034 method Methods 0.000 title claims description 7
- 239000002689 soil Substances 0.000 claims abstract description 72
- 239000011368 organic material Substances 0.000 claims abstract description 29
- 239000001963 growth medium Substances 0.000 claims abstract description 23
- 238000005341 cation exchange Methods 0.000 claims abstract description 20
- 239000002245 particle Substances 0.000 claims abstract description 19
- 229910052500 inorganic mineral Inorganic materials 0.000 claims abstract description 12
- 239000011707 mineral Substances 0.000 claims abstract description 12
- 239000003337 fertilizer Substances 0.000 claims abstract description 9
- 239000000126 substance Substances 0.000 claims abstract description 8
- 238000005507 spraying Methods 0.000 claims abstract description 5
- 239000002609 medium Substances 0.000 claims description 30
- 239000011435 rock Substances 0.000 claims description 17
- 230000003628 erosive effect Effects 0.000 claims description 11
- 238000002156 mixing Methods 0.000 claims description 7
- 239000011230 binding agent Substances 0.000 claims description 6
- 230000002265 prevention Effects 0.000 claims description 6
- 238000010276 construction Methods 0.000 claims description 4
- 239000003516 soil conditioner Substances 0.000 claims description 4
- 238000007873 sieving Methods 0.000 claims description 2
- 239000004615 ingredient Substances 0.000 claims 1
- 230000001052 transient effect Effects 0.000 abstract description 3
- 239000007767 bonding agent Substances 0.000 abstract 1
- 238000013329 compounding Methods 0.000 abstract 1
- 235000008935 nutritious Nutrition 0.000 abstract 1
- 241000196324 Embryophyta Species 0.000 description 27
- 235000015097 nutrients Nutrition 0.000 description 15
- 241000894007 species Species 0.000 description 13
- 230000007704 transition Effects 0.000 description 12
- XLYOFNOQVPJJNP-UHFFFAOYSA-N water Substances O XLYOFNOQVPJJNP-UHFFFAOYSA-N 0.000 description 8
- 230000008635 plant growth Effects 0.000 description 6
- 239000000084 colloidal system Substances 0.000 description 5
- 230000007423 decrease Effects 0.000 description 5
- 238000010586 diagram Methods 0.000 description 5
- 244000005700 microbiome Species 0.000 description 5
- 238000005516 engineering process Methods 0.000 description 4
- 239000000203 mixture Substances 0.000 description 4
- 150000003839 salts Chemical class 0.000 description 4
- 241000894006 Bacteria Species 0.000 description 3
- 229910021536 Zeolite Inorganic materials 0.000 description 3
- 239000002361 compost Substances 0.000 description 3
- 230000003111 delayed effect Effects 0.000 description 3
- HNPSIPDUKPIQMN-UHFFFAOYSA-N dioxosilane;oxo(oxoalumanyloxy)alumane Chemical compound O=[Si]=O.O=[Al]O[Al]=O HNPSIPDUKPIQMN-UHFFFAOYSA-N 0.000 description 3
- 230000000694 effects Effects 0.000 description 3
- 230000014759 maintenance of location Effects 0.000 description 3
- 230000000813 microbial effect Effects 0.000 description 3
- 239000010457 zeolite Substances 0.000 description 3
- 241000233866 Fungi Species 0.000 description 2
- 238000005054 agglomeration Methods 0.000 description 2
- 230000002776 aggregation Effects 0.000 description 2
- 239000002131 composite material Substances 0.000 description 2
- 230000012010 growth Effects 0.000 description 2
- 235000008216 herbs Nutrition 0.000 description 2
- 238000012423 maintenance Methods 0.000 description 2
- 239000003415 peat Substances 0.000 description 2
- 230000002035 prolonged effect Effects 0.000 description 2
- 241001156739 Actinobacteria <phylum> Species 0.000 description 1
- 244000025254 Cannabis sativa Species 0.000 description 1
- 238000013459 approach Methods 0.000 description 1
- 230000001580 bacterial effect Effects 0.000 description 1
- 239000000440 bentonite Substances 0.000 description 1
- 229910000278 bentonite Inorganic materials 0.000 description 1
- SVPXDRXYRYOSEX-UHFFFAOYSA-N bentoquatam Chemical compound O.O=[Si]=O.O=[Al]O[Al]=O SVPXDRXYRYOSEX-UHFFFAOYSA-N 0.000 description 1
- 230000015572 biosynthetic process Effects 0.000 description 1
- 239000003795 chemical substances by application Substances 0.000 description 1
- 230000000052 comparative effect Effects 0.000 description 1
- 238000007596 consolidation process Methods 0.000 description 1
- 238000001035 drying Methods 0.000 description 1
- 239000010438 granite Substances 0.000 description 1
- GPRLSGONYQIRFK-UHFFFAOYSA-N hydron Chemical compound [H+] GPRLSGONYQIRFK-UHFFFAOYSA-N 0.000 description 1
- 229910021432 inorganic complex Inorganic materials 0.000 description 1
- 230000005923 long-lasting effect Effects 0.000 description 1
- 238000004519 manufacturing process Methods 0.000 description 1
- 230000007935 neutral effect Effects 0.000 description 1
- 239000010451 perlite Substances 0.000 description 1
- 235000019362 perlite Nutrition 0.000 description 1
- 239000002952 polymeric resin Substances 0.000 description 1
- 230000001737 promoting effect Effects 0.000 description 1
- 239000007921 spray Substances 0.000 description 1
- 229920003002 synthetic resin Polymers 0.000 description 1
- 241001446247 uncultured actinomycete Species 0.000 description 1
- 239000010455 vermiculite Substances 0.000 description 1
- 229910052902 vermiculite Inorganic materials 0.000 description 1
- 235000019354 vermiculite Nutrition 0.000 description 1
Landscapes
- Pit Excavations, Shoring, Fill Or Stabilisation Of Slopes (AREA)
Abstract
Description
【発明の詳細な説明】
[産業上の利用分野]
本発明は、岩盤法面に吹付けて緑化を行う岩盤法面緑化
材および岩盤法面緑化方法に間する。[Detailed Description of the Invention] [Industrial Application Field] The present invention relates to a rock slope greening material and a rock slope greening method that are sprayed onto a rock slope to green the slope.
[従来の技術]
周知の如く、ゴルフ場、大規模公園、住宅団地、工業団
地、道路等の造成に際し、その工事によって無植物の状
態となった岩盤法面に緑化材を吹付けて人工培地を作り
、緑化を行う技術はすでに知られている。[Prior Art] As is well known, when constructing golf courses, large-scale parks, residential complexes, industrial parks, roads, etc., greening materials are sprayed onto rock slopes that have become devoid of vegetation due to the construction work, creating artificial culture media. The technology to create trees and carry out greening is already known.
かかる従来の緑化材としては、少なくとも土壌と有機質
資材、例えばバーク堆廁又はピートモスと、高分子系樹
脂、例えば商品名クリコートC−710、CP−750
,C−402のような浸食防止用の粒子結合剤と、化学
肥料と植物種子とを混合したものが知られており、必要
に応じてパーライトのような鉱物質資材を加えて保水性
を増大させている。そして緑化材は、岩盤法面の硬度指
数や割れ目の入り方すなわち岩盤の固結度や風化程度、
工事現場の年間降水量と標高および岩盤法面の勾配等を
勘案してその吹付は厚さを決定していた。このようにし
て、吹付けた人工培地はその後時間の経過とともに種子
が発芽し、植物が生育して法面を被覆する。Such conventional greening materials include at least soil, organic materials such as bark compost or peat moss, and polymeric resins such as Cricoat C-710 and CP-750 (trade names).
, C-402, a mixture of chemical fertilizer and plant seeds is known, and if necessary mineral materials such as perlite can be added to increase water retention. I'm letting you do it. Greening materials are determined based on the hardness index of the rock slope, the way in which cracks form, the degree of consolidation and weathering of the bedrock, etc.
The thickness of the spraying was determined by taking into account the annual rainfall and altitude of the construction site, the slope of the rock slope, etc. In this way, seeds of the sprayed artificial medium will germinate over time, and plants will grow and cover the slope.
[従来技術の問題点]
一般に、植物の育成は、土地が安定化すれば、年月の経
過とともに植生の遷移が進むものであり、0〜7年の初
期相では草本類が、5〜30年の過渡相では潅木、低木
類が、そして20〜100年以上の極相では高木類が生
育する。したがって、岩盤法面に吹付けた人工培地に生
育する植生についても自然に前記の遷移をすることが必
要である。[Problems with the prior art] In general, when growing plants, once the land is stabilized, vegetation succession progresses over time.In the initial phase of 0 to 7 years, herbaceous plants Shrubs and bushes grow in the transitional phase of 20 years, and trees grow in the peak phase of 20 to 100 years or more. Therefore, it is necessary for the vegetation growing on the artificial culture medium sprayed on the rock slope to undergo the above-mentioned transition naturally.
しかしながら、従来技術においては、無植被状態の法面
の浸食防止を急ぐために、下記の問題点があった。However, in the prior art, the following problems occurred in order to prevent erosion of slopes without vegetation cover.
(1) 吹付ける人工培地に配合される種子としては、
生長は早いが培地の養分が少なくなると衰退しやすい外
来種の草本類(例えば芝草)を主とし、そして初期生育
は遅いが丈夫て”長持ちする日本在来の種を従としてい
たなめに、極く初期において、日本の風土に適した日本
在来種の草本類は、旺盛な外来種の草本類の生育に圧倒
されて、定着が困難ないしは極めて遅れることになる。(1) Seeds added to the artificial medium to be sprayed include:
The main focus is on exotic herbaceous species (such as turf grass) that grow quickly but tend to decline when the nutrients in the culture medium become low, and the species that are native to Japan are slow-growing initially but are hardy and long-lasting. In the early stages, the native Japanese herbaceous species that are suited to Japan's climate will be overwhelmed by the vigorous growth of non-native herbaceous species, and establishment will be difficult or extremely slow.
従って、植生遷移の初期相が長びき、過渡相への遷移進
行が遅れ、また初期相が長びくために、外来種の草本類
の衰退に伴う日本在来種草本類の交替が追いつかない、
そのために法面植生による被覆度が低下して、培地の浸
食防止が不十分となる。Therefore, the initial phase of vegetation succession is prolonged, the transition to the transitional phase is delayed, and because the initial phase is prolonged, the replacement of native Japanese herbaceous species due to the decline of exotic herbaceous species cannot keep up.
As a result, the degree of coverage by slope vegetation decreases, and erosion prevention of the culture medium becomes insufficient.
(2) 培地の土壌的性質の基準が確立していないため
に、植物は法面上の限られた厚さの培地を主として利用
して生育し続けなければならないから、培地の土壌的性
質が植生の維持と遷移とに対して必ずしも適合していな
いこと。(2) Since standards for the soil-like properties of the medium have not been established, plants must continue to grow mainly using the limited thickness of the medium on the slope. Not necessarily compatible with vegetation maintenance and succession.
[問題点を解決するための手段]
したがって、本発明の目的は、培地の浸食を防止すると
共に、植生の遷移が好適に行われる岩盤法面緑化材およ
び岩盤法面緑化方法を提供するにある。[Means for Solving the Problems] Therefore, an object of the present invention is to provide a bedrock slope greening material and a bedrock slope greening method that prevent erosion of the culture medium and facilitate the transition of vegetation. .
[発明の知見]
本発明者等は、花崗岩、安山岩、玄武岩、砂岩、左右等
の地質系統の異なる地帯に施工された各地の現場法面の
培地を採取し、植物生育と関係が深いと思われる要件、
すなわち、培地の水素イオン濃度(pH)、塩類含有量
を示す電気伝導度、植物が容易に利用し得る水分である
易有効水分保持能、植物養分の保持能である陽イオン交
換容量、培地中の植物養分の循環を司る土壌微生物の生
菌数と微生物生態系の状態を判定する指標である「細菌
数/糸状菌数」比および「細菌数/放線菌数」比などを
分析した。その結果、岩盤法面に51厚で吹付けた場合
に、人工培地が最低限具備しなければならない土壌的性
質は下記の通りであることが解った。[Findings of the Invention] The present inventors collected culture medium from slopes of construction sites in different geological areas such as granite, andesite, basalt, sandstone, left and right, and found that it is thought to be closely related to plant growth. requirements,
In other words, the hydrogen ion concentration (pH) of the medium, the electrical conductivity indicating the salt content, the effective water retention capacity, which is water that plants can easily use, the cation exchange capacity, which is the ability to retain plant nutrients, and the medium content. We analyzed the viable counts of soil microorganisms that control the circulation of plant nutrients, as well as the ``bacterial count/filamentous fungi count'' ratio and the ``bacteria count/actinobacteria count'' ratio, which are indicators for determining the state of the microbial ecosystem. As a result, it was found that the minimum soil properties that an artificial culture medium must have when sprayed on a rock slope at a thickness of 51 are as follows.
pH:6.5〜7.3(中性領域)
電気伝導度: 1ms (ミリシーメンス)/clI以
下
易有効水分保持能カニ20m++以上
陽イオン交換容量: 10eq (当量)/rrr以上
土壌微生物生菌数
細菌数:5X10’/g以上
細菌数糸状菌数:50〜500
細菌数/放線菌数=1〜10
その他 :水浸食に対して高抵抗性のあること
しかしながら、従来技術の場合は、上記の要件に対して
不十分であり、特に陽イオン交換容量が不足していた。pH: 6.5 to 7.3 (neutral range) Electrical conductivity: 1 ms (millisiemens)/clI or less Easy effective water retention capacity Crab 20 m++ or more Cation exchange capacity: 10 eq (equivalent)/rrr or more Soil microbial viable bacteria Bacterial count: 5 x 10'/g or more Bacteria count Filamentous fungus count: 50 to 500 Bacteria count/actinomycete count = 1 to 10 Others: High resistance to water erosion However, in the case of conventional technology, the above The cation exchange capacity was insufficient, especially the cation exchange capacity.
[課題を解決するための手段]
本発明の岩盤法面緑化材によれば、人工培地の材料とし
て少なくとも土壌と有機質資材と浸食防止用の粒子結合
剤と化学肥料と植物種子とを混合して岩盤法面に吹付け
る岩盤法面緑化材において、前記土壌は土木工事現場又
はその近傍に分布する土壌の表層土を篩分けした粒径4
+m以下の土粒子であり、その配合率は有機質資材の容
量1に対して容量比0.4ないし0.5であり、かつ大
きい陽イオン交換容量を有する鉱物質土壌改良材が有機
質資材の容量1に対して容量比0.05ないし0.1の
割合で配合されている。[Means for Solving the Problems] According to the rock slope greening material of the present invention, at least soil, an organic material, a particle binder for erosion prevention, a chemical fertilizer, and a plant seed are mixed as materials for an artificial medium. In the bedrock slope greening material that is sprayed onto the bedrock slope, the soil has a particle size of 4, which is obtained by sieving the surface soil of the soil distributed at or near the civil engineering work site.
+ m or less soil particles, the mixing ratio of which is a volume ratio of 0.4 to 0.5 to 1 volume of organic material, and a mineral soil improvement material having a large cation exchange capacity is equal to or less than the volume of organic material. 1 to 1 at a volume ratio of 0.05 to 0.1.
また、本発明の岩盤法面緑化方法によれば、人工培地の
材料として少なくとも土壌と有機質資材と浸食防止用の
粒子結合剤と化学肥料と植物種子とを混合して岩盤法面
に吹付ける岩盤法面緑化方法において、土木工事によっ
て取り去った土壌のうち少なくとも表層土を粒径4m1
1以下の土粒子に篩分けし、その篩分けした土粒子を有
機質資料に対して容量比0.4ないし0.5と、大きい
陽イオン交換容量を有する鉱物質土壌改良材を有機質資
材に対して容量比0.05ないし0.1とを配合し、そ
の配合された材料を岩盤法面に吹付けるようになってい
る。Further, according to the rock slope greening method of the present invention, at least soil, an organic material, a particle binder for erosion prevention, a chemical fertilizer, and a plant seed are mixed as materials for an artificial medium, and the mixture is sprayed onto the bedrock slope. In the slope greening method, at least the surface soil of the soil removed by civil engineering works is
The sieved soil particles are sieved into soil particles with a volume ratio of 0.4 to 0.5 relative to the organic material, and a mineral soil conditioner having a large cation exchange capacity is mixed with the organic material. The material is mixed with a volume ratio of 0.05 to 0.1, and the mixed material is sprayed onto the rock slope.
[作用]
現地発生土である土木工事現場又はその付近の表層土を
用いるのでその土地に適する在来種の種子が比較的に多
量に含まれており、在来種の生育が促進され、その結果
、遷移がスムーズに行われる。4w以下に篩分けした理
由は、現地発生土が有機質資材に付着しやすいからであ
る。すなわち4w以上では吹付は後に乾燥すると落ちて
しまう。[Effect] Since locally generated soil from the civil engineering work site or its surroundings is used, it contains a relatively large amount of seeds of native species suitable for the site, promoting the growth of native species and increasing the number of seeds. As a result, transitions occur smoothly. The reason why the soil was sieved to 4w or less is that locally generated soil tends to adhere to organic materials. That is, at 4W or more, the spray will fall off after drying.
有機質資材としてはピートモスまたはパーク堆肥等が用
いられる。現地発生土の配合割合が有機質資材1に対し
て容量比0.4以下では現地発生土の中へ種子の量が少
なくなり、したがって遷移が遅れる。また後述の如く有
機無機複合コロイドの形成が少ない、また0、5以上で
は、エロージョンされやすくなり、土壌が落ちやすくな
る。すなわち種子の点から見れば現地発生土が多いほど
好ましいが、土壌が多すぎると培地の耐浸食性、易有効
水分保持能が低下する。したがって、容量比は0.4〜
0.5とするものである。Peat moss or park compost is used as the organic material. If the mixing ratio of locally generated soil is less than 0.4 by volume to 1 part of organic material, the amount of seeds entering the locally generated soil will be small and the transition will be delayed. Further, as will be described later, if the formation of organic-inorganic composite colloid is small, or if it is 0.5 or more, erosion will occur easily and the soil will easily fall off. That is, from the point of view of seeds, it is preferable to have as much locally grown soil as possible, but if there is too much soil, the erosion resistance and effective moisture retention capacity of the medium will decrease. Therefore, the capacity ratio is 0.4~
0.5.
一般に現地発生土には陽イオン交換容量の低いものが多
い、そこで本発明では大きい陽イオン交換容量を有する
鉱物質土壌改良材、例えばゼオライト、バーミキュライ
ト、ベントナイト等が混合されている。有機質資材に対
する配合容量比が0゜05以下では10eq/rrf以
上の陽イオン交換容量が得られず、充分な植物養分の保
持能が得られない、容量比が0.1以上では経済的に好
ましくない、したがって容量比は0.05〜0.1とす
る。Generally, many locally generated soils have a low cation exchange capacity, so in the present invention, a mineral soil conditioner having a large cation exchange capacity, such as zeolite, vermiculite, bentonite, etc., is mixed. If the blended volume ratio to the organic material is less than 0.05, a cation exchange capacity of 10 eq/rrf or more cannot be obtained, and sufficient plant nutrient retention ability cannot be obtained. If the volume ratio is 0.1 or more, it is economically preferable. Therefore, the capacitance ratio is set to 0.05 to 0.1.
本発明によれば、従来技術に対して以下の点が改善され
る
(1) 有機質資材を主材料とする培地では、無降雨の
日が続き培地が乾燥し始めると、水をはじく性質(虎水
性)を示し始めるなめ、数ミリ以下の降雨があっても、
培地がこの水を吸着・保持する量が少なくなるので植物
への水の供給が減少する。これは植物の生長を抑制する
1つの原因となる。現地発生土を配合した培地では、こ
の碗水性が抑えられるので、1〜2■の少量の降雨であ
っても、その水をよく吸着・保持するようになる。According to the present invention, the following points are improved over the conventional technology: (1) In a culture medium made mainly of organic materials, when the culture medium begins to dry after a period of no rain, the property of water repellency (difficult) Even if there is less than a few millimeters of rainfall,
The medium absorbs and retains less of this water, reducing the water supply to the plants. This is one of the causes of suppressing plant growth. A culture medium containing locally generated soil suppresses this watery property, so even a small amount of rainfall of 1 to 2 cm can adsorb and retain water well.
(2) 陽イオン交換容量の大きい鉱物質土壌改良材を
配合しないで、有機質資材と現地発生土とを配合した人
工培地の陽イオン交換容量は約7〜約14eq/nfの
範囲で変動する。現地発生土が陽イオン交換容量の小さ
い砂質土ないし壌質土であれば、陽イオン交換容量は1
0eq/rrr以下となり、規定した人工培地の土壌的
性質の基準に及ばなくなる。陽イオン交換容量の大°き
い鉱物質資材、例えばゼオライトを有機質資材に対して
0゜05〜0.1の割合で配合すると、この配合によっ
て陽イオン交換容量が3.75〜7.5eq/d増大す
るので、有機質資材・現地発生土・ゼオライトの3者を
配合した人工培地では、どのような現地発生土を利用す
る場合でも、その陽イオン交換容量は10eq/rrr
以上となり、人工培地の養分保持能力が保障される。(2) The cation exchange capacity of an artificial culture medium made by blending organic materials and locally generated soil without blending a mineral soil conditioner with a large cation exchange capacity varies in the range of about 7 to about 14 eq/nf. If the locally generated soil is sandy or loamy soil with a small cation exchange capacity, the cation exchange capacity is 1.
It becomes 0 eq/rrr or less, which does not meet the specified criteria for soil properties of an artificial medium. When a mineral material with a large cation exchange capacity, such as zeolite, is blended with an organic material at a ratio of 0.05 to 0.1, the cation exchange capacity increases from 3.75 to 7.5 eq/d. Therefore, in an artificial medium containing organic materials, locally generated soil, and zeolite, the cation exchange capacity is 10 eq/rrr no matter what type of locally generated soil is used.
With the above, the nutrient retention ability of the artificial medium is guaranteed.
(3) 人工培地の主材料であるパーク堆肥(有機質資
材)は、製造工程上、かなりの塩分を含んでいるので、
有機質資材を主材料とする培地では、乾燥が進むと、培
地中の水に含まれる塩分濃度が高まりやすく、ために植
物の生育が阻害されるおそれがある。しかし現地発生土
を混用した培地では培地中の水の塩分濃度の高まりが僅
で済むので、植物生育が阻害されることはない。(3) Park compost (organic material), which is the main material for artificial culture media, contains a considerable amount of salt due to the manufacturing process.
When a culture medium is mainly made of organic materials, as it dries out, the salt concentration in the water in the culture medium tends to increase, which can inhibit plant growth. However, in a medium mixed with locally grown soil, the salt concentration of the water in the medium increases only slightly, so plant growth is not inhibited.
(4) 培地からの植物養分の連続的供給という面から
みると、培地の活性画分(植物の生育に寄与するもの)
が、有機コロイド質単独、あるいは無機コロイド質単独
の場合より、有機・無機複合コロイドによって構成され
ている方が植物生育の培地としてはすぐれていることは
土壌学分野における定説である。現地発生土を混用した
培地では、混用しない場合とは異なり、有機・無機複合
コロイドが年月の経過とともに形成され、培地の土壌団
粒化が進む、これは植物に対する培地からの養分の連続
的供給という面から極めて有利である。すなわち、岩盤
法面上の培地では、人工培地を吹付けるさいに、肥料を
も配合するが、吹付は後1〜2年間で肥料に由来する養
分は消失してしまい、爾後は、限られた培地の中で培地
が備えている養分循環能(枯れると再び養分が土にもど
る)によって、養分は絶えず植物に供給されねばならな
い事態となる。この培地中の養分循環を司るのは土壌微
生物である。土壌微生物は、培地の土壌団粒化が進むと
、恰好の棲み家が多くなるので、多様な土壌微生物がバ
ランスよく培地中で棲み分けするようになり、その結果
、健全な土壌微生物生態系が維持されるようになる。し
たがって、培地より植物への養分の連続的供給が滞りな
く進行する。(4) From the perspective of continuous supply of plant nutrients from the medium, the active fraction of the medium (those that contribute to plant growth)
However, it is a well-established theory in the field of soil science that a medium composed of organic and inorganic composite colloids is superior to a single organic colloid or an inorganic colloid alone as a medium for plant growth. Unlike when soil is not mixed, organic and inorganic complex colloids are formed over time, and soil agglomeration in the medium progresses. This is due to the continuous flow of nutrients from the medium to plants. This is extremely advantageous in terms of supply. In other words, in the case of a culture medium on a bedrock slope, fertilizer is also mixed in when spraying the artificial medium, but the nutrients derived from the fertilizer disappear within one to two years after spraying, and after that, the nutrients derived from the fertilizer disappear. Due to the ability of the culture medium to circulate nutrients (nutrients are returned to the soil once it withers), nutrients must be constantly supplied to the plants. Soil microorganisms control the nutrient circulation in this medium. As soil agglomeration in the medium progresses, suitable habitats for soil microorganisms increase, allowing a variety of soil microorganisms to live in a well-balanced manner in the medium, resulting in a healthy soil microbial ecosystem. will be maintained. Therefore, the continuous supply of nutrients from the culture medium to the plants progresses without any hitch.
(5) 岩盤法面に吹付ける人工培地の土壌的性質を規
定し、人工培地の主材料を有機質資材と現地発生土との
混用とすれば、上記(1)、(2)(3)、(4)で述
べた植生培地としての改善が進むので、これらの作用が
総合的に、法面植生の維持と遷移の進行を反映する。(5) If the soil properties of the artificial culture medium sprayed onto the rock slope are defined and the main materials of the artificial culture medium are a mixture of organic materials and locally generated soil, then (1), (2), (3) above, As the improvement as a vegetation medium described in (4) progresses, these effects collectively reflect the maintenance of slope vegetation and the progression of succession.
[好ましい実施の態様〕
本発明の実施に際して、浸食防止用の粒子結合剤、化学
把料および外来植物種子は任意の公知のものを使用でき
る。また現地発生土としては表層土が不足する場合は、
次層上の上部の土を用いることができる。[Preferred Embodiment] In carrying out the present invention, any known particle binder, chemical binder, and exotic plant seed for erosion prevention can be used. In addition, if there is insufficient surface soil as locally generated soil,
The top soil on the next layer can be used.
[実施例] 以下図面を参照して本発明の詳細な説明する。[Example] The present invention will be described in detail below with reference to the drawings.
第1図は、代表的な土壌の断面形態を示し、地表Sには
草本類Pが生育しており、その地表Sのすぐ下側の層で
あるA層は表層土すなわちいわゆる黒土であり、植物の
根が主として伸長する範囲であって、土壌微生物の生息
数が多い、その厚さは通常10011位である。その下
のB層は次層上であり、岩石が風化して土壌化している
が、無機質が多く、植物養分に乏しい、その下の0層は
岩石の風化した比較的に小さい破砕物質から成っており
、前記A層およびB層の母材である。地表Sから0層の
下面までの深さは一定ではないがほぼ100an程度で
ある。0層の下のR層はまだ強い風化を受けていない岩
石の層であり、その下のG部は弱い風化を受けている岩
石である。Figure 1 shows the cross-sectional form of a typical soil.Herbaceous plants P grow on the ground surface S, and the layer A, which is the layer immediately below the ground surface S, is surface soil, or so-called black soil. This is the area where plant roots mainly grow, where a large number of soil microorganisms live, and its thickness is usually about 10,011 mm. The B layer below is the next layer, and is made up of weathered rocks that turn into soil, but it is rich in minerals and lacks plant nutrients. It is the base material of the A layer and B layer. The depth from the ground surface S to the bottom surface of the 0th layer is not constant, but is approximately 100 an. The R layer below the 0 layer is a rock layer that has not yet been strongly weathered, and the G layer below it is a rock layer that has been weakly weathered.
本発明の実施に際して、まず第2図において符号1で示
す斜線部分の土壌を土木工事によって取り去り、その土
木工事によって法面2が露出する。In implementing the present invention, first, the soil in the shaded area indicated by reference numeral 1 in FIG. 2 is removed by civil engineering work, and the slope 2 is exposed by the civil engineering work.
地表Sには在来の木本類Tおよび草本類Pが生育してい
る。Native woody plants T and herbaceous plants P grow on the ground surface S.
次いで第3図に示すように本発明を実施した緑化材を法
面2に吹付けて培地3を形成する0通常その厚みはSa
a位である。吹付けた土壌の表面には数日後にまず緑化
剤に混合された種子が発芽して草本類4として生育する
が、この草本類4は初めは外来種の草本類と在来種の草
本類とが一緒に生育するが、徐々に在来のものが優勢に
なって、植生遷移の初期相が確立し、過渡相への移行が
早まる。この過渡相への移行は4ケ月余位から開始され
る。Next, as shown in FIG. 3, a greening material according to the present invention is sprayed onto the slope 2 to form a culture medium 3. Usually, the thickness thereof is Sa.
It is in position a. After a few days, the seeds mixed with the greening agent germinate on the surface of the sprayed soil and grow as herbaceous plants 4, but these herbaceous plants 4 are initially divided into exotic plants and native plants. The native species gradually become dominant, establishing the initial phase of vegetation succession and hastening the transition to the transitional phase. The transition to this transitional phase begins in about four months.
その結果、数年を経過すると、第4図に示す通り、培地
3に生育している草本類4としては在来種が優勢となり
、比較的多数の潅木類5も生育する。As a result, after several years, as shown in FIG. 4, native species become dominant as the herbs 4 growing in the medium 3, and a relatively large number of shrubs 5 also grow.
[比較例]
第5図は従来技術による植生遷移を示し、緑化工後節4
図と同様に数年経過した後に、培地3に植生した草本類
4としては依然として外来種が優先であり、そのために
潅木類5の定着は僅である。[Comparative example] Figure 5 shows the vegetation transition according to the conventional technology.
As shown in the figure, after several years have passed, foreign species still have priority as the herbaceous plants 4 that have grown on the medium 3, and therefore the establishment of shrubs 5 is slight.
これは過渡相への移行が遅れていることを意味する。This means that the transition to the transient phase is delayed.
[発明の効果]
以上の如く、本発明によれば、初期相から過渡相への進
行が4ケ月余で始まり、従来例の数年に比してはるかに
短い。[Effects of the Invention] As described above, according to the present invention, the progression from the initial phase to the transient phase begins in more than four months, which is much shorter than several years in the conventional example.
寿命の短い外来種の草本類の衰退が始まっても、寿命が
長い在来種の草本類の生育が一層旺盛となるので、法面
上の培地は浸食されることなく、植生の遷移は一層加速
される。そのなめに、岩盤法面上の人工的な植生が速か
に自然の状態に近付き、周辺の自然景観にとけこみ、岩
盤法面の安定はまとまり、景観上も好ましい。Even if the short-lived non-native herbaceous species begin to decline, the long-lived native herbaceous species will continue to grow even more vigorously, so the medium on the slope will not be eroded and the transition of vegetation will be even faster. be accelerated. As a result, the artificial vegetation on the bedrock slope rapidly approaches its natural state and blends into the surrounding natural landscape, making the bedrock slope more stable and aesthetically pleasing.
第1図は自然の土壌の断面形態の一例を示す図、第2図
は本発明の実施の一例を示す説明図、第3図は本発明に
より緑化工が完了して草本類が培地に生育したところを
示す説明図、第4図は数年経過後の植生の遷移を示す説
明図、第5図は従来例による植生の遷移を示す説明図で
ある。
1・・・土木工事で取り去られる部分 2・・・法面
3・・・培地 4・・・草本類5・・・潅木類Fig. 1 is a diagram showing an example of the cross-sectional form of natural soil, Fig. 2 is an explanatory diagram showing an example of the implementation of the present invention, and Fig. 3 is a diagram showing an example of the implementation of the present invention. FIG. 4 is an explanatory diagram showing the transition of vegetation after several years, and FIG. 5 is an explanatory diagram showing the transition of vegetation according to a conventional example. 1... Parts removed during civil engineering work 2... Slope 3... Culture medium 4... Herbs 5... Shrubs
Claims (2)
材と浸食防止用の粒子結合剤と化学肥料と植物種子とを
混合して岩盤法面に吹付ける岩盤法面緑化材において、
前記土壌は土木工事現場又はその近傍に分布する土壌の
表層土を篩分けした粒径4mm以下の土粒子であり、そ
の配合率は有機質資材の容量1に対して容量比0.4な
いし0.5であり、かつ大きい陽イオン交換容量を有す
る鉱物質土壌改良材が有機質資材の容量1に対して容量
比0.05ないし0.1の割合で配合されていることを
特徴とする岩盤法面緑化材。(1) In a bedrock slope greening material that is sprayed onto a bedrock slope by mixing at least soil, organic materials, a particle binder for erosion prevention, chemical fertilizer, and plant seeds as materials for the artificial medium,
The soil is soil particles with a particle size of 4 mm or less obtained by sieving the surface soil of soil distributed at or near civil engineering construction sites, and the mixing ratio is 0.4 to 0.4 mm in volume to 1 volume of organic material. 5 and a mineral soil improvement material having a large cation exchange capacity is blended at a volume ratio of 0.05 to 0.1 to 1 volume of the organic material. Greening material.
材と浸食防止用の粒子結合剤と化学肥料と植物種子とを
混合して岩盤法面に吹付ける岩盤法面緑化方法において
、土木工事によって取り去った土壌のうち少なくとも表
層土を粒径4mm以下の土粒子に篩分けし、その篩分け
した土粒子を有機質資料に対して容量比0.4ないし0
.5と、大きい陽イオン交換容量を有する鉱物質土壌改
良材を有機質資材に対して容量比0.05ないし0.1
とを配合し、その配合された材料を岩盤法面に吹付ける
ことを特徴とする岩盤法面緑化方法。(2) In a bedrock slope greening method in which at least soil, organic materials, particle binders for erosion prevention, chemical fertilizers, and plant seeds are mixed as materials for an artificial culture medium and sprayed onto the bedrock slope, the materials removed by civil engineering work. At least the surface soil of the soil is sieved into soil particles with a particle size of 4 mm or less, and the sieved soil particles are mixed with organic material at a volume ratio of 0.4 to 0.
.. 5 and a mineral soil conditioner with a large cation exchange capacity to the organic material at a volume ratio of 0.05 to 0.1.
A rock slope greening method characterized by blending the above ingredients and spraying the blended material onto the rock slope.
Priority Applications (1)
Application Number | Priority Date | Filing Date | Title |
---|---|---|---|
JP7489089A JPH02256718A (en) | 1989-03-29 | 1989-03-29 | Bedrock slope face tree-planting material and bedrock slope face tree-planting method |
Applications Claiming Priority (1)
Application Number | Priority Date | Filing Date | Title |
---|---|---|---|
JP7489089A JPH02256718A (en) | 1989-03-29 | 1989-03-29 | Bedrock slope face tree-planting material and bedrock slope face tree-planting method |
Publications (2)
Publication Number | Publication Date |
---|---|
JPH02256718A true JPH02256718A (en) | 1990-10-17 |
JPH052772B2 JPH052772B2 (en) | 1993-01-13 |
Family
ID=13560419
Family Applications (1)
Application Number | Title | Priority Date | Filing Date |
---|---|---|---|
JP7489089A Granted JPH02256718A (en) | 1989-03-29 | 1989-03-29 | Bedrock slope face tree-planting material and bedrock slope face tree-planting method |
Country Status (1)
Country | Link |
---|---|
JP (1) | JPH02256718A (en) |
Cited By (1)
Publication number | Priority date | Publication date | Assignee | Title |
---|---|---|---|---|
CN103962054A (en) * | 2014-05-20 | 2014-08-06 | 江苏杰成凯新材料科技有限公司 | Method for pelletizing weathered powdery sandstone |
-
1989
- 1989-03-29 JP JP7489089A patent/JPH02256718A/en active Granted
Cited By (1)
Publication number | Priority date | Publication date | Assignee | Title |
---|---|---|---|---|
CN103962054A (en) * | 2014-05-20 | 2014-08-06 | 江苏杰成凯新材料科技有限公司 | Method for pelletizing weathered powdery sandstone |
Also Published As
Publication number | Publication date |
---|---|
JPH052772B2 (en) | 1993-01-13 |
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