2011
DOI: 10.1080/00380768.2010.541868
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Effects of herbicide application on carbon dioxide, dissolved oxygen, pH, and RpH in paddy-field ponded water

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Cited by 19 publications
(8 citation statements)
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“…4.30 -5.05 (Table 6), indicating that the application of pesticides on peat soil did not change the soil pH. The result of current study is in contrast with the study of Usui (2011) that showed that the application of herbicide (HA -ACN, (2-amino-3-chloro-1,4-naphthoquinon) 9%) on paddy soil increased the soil pH and decreased the CO 2 emissions along with the accumulation period. On the other hand, according to Bennicelli (2008), the application of the pesticide (Glyphosphat) on Histosol increased the dehydrogenase enzyme activity, pH, Eh, and CO 2 production after 42 days of incubation.…”
Section: Ph Of Peat Soilcontrasting
confidence: 55%
“…4.30 -5.05 (Table 6), indicating that the application of pesticides on peat soil did not change the soil pH. The result of current study is in contrast with the study of Usui (2011) that showed that the application of herbicide (HA -ACN, (2-amino-3-chloro-1,4-naphthoquinon) 9%) on paddy soil increased the soil pH and decreased the CO 2 emissions along with the accumulation period. On the other hand, according to Bennicelli (2008), the application of the pesticide (Glyphosphat) on Histosol increased the dehydrogenase enzyme activity, pH, Eh, and CO 2 production after 42 days of incubation.…”
Section: Ph Of Peat Soilcontrasting
confidence: 55%
“…,地球上で最も溶存 酸素濃度が高い水域の一つ(粕渕, 2010)とも言われて いる。溶存酸素が日周変化するのは,湛水層に生息 するシアノバクテリアや藻類の光合成および呼吸に よると考えられる (Saito and Watanabe, 1978;伊藤・ 増島, 1980, 1984Ito, 1987;Mowjood and Kasubuchi, 1998a, 1998bKishida et al, 2001;Usui and Kasubuchi, 2011;臼井・粕渕, 2013 Mikkelsen et al, 1978)。Mikkelsen et al(1978は太陽 放射のもと,浅い湛水中では,そこに生息している 水生生物の作用により pH が 9.5 から 10 と高い値へ と上昇することでアンモニアの揮散が生じることを 報告している。土壌 pH のみならず,湛水の pH の測 定には,肥培管理の指標として重要な側面があり, 水田湛水の pH の挙動を知ることは,作物の栽培管 理の上でも重要な役割があると考えられる(臼井・粕 渕 2013)。このほか,水田湛水中における高 pH に ついては多くの報告がなされており (Mikkelsen et al, 1978;伊藤・増島, 1980, 1984Ito, 1987;Kishida et al, 2001;Usui et al, 2003;Usui and Kasubuchi, 2011; 臼 井・粕渕, 2013),高 pH となった湛水層が,湛水層近 傍の大気中 CO2 を吸収していることも明らかとなっ ている (Usui et al, 2003) Kasubuchi, 1998a, 1998b Kasubuchi, 1998a, 2002)ことから,水田における温室効果ガスの湛水層 を介しての挙動に対して対流がどのように関わって くるのかを検討することが期待される。 また,湖沼において水の対流は生態系を維持する 上で重要と認識されている (Horne and Goldman, 1994;花里, 1998;奥宮ら, 2001 …”
Section: 水田における物理計測の重要性unclassified
“…The total dissolved oxygen (DO) is very important as it influences rice root growth and nitrogen availability in the soil. The rate of DO in the water increases when enough sunlight reaches the surface of rice leaves and bare fields (Usui & Kasubuchi, 2011). This term measures water quality for rice where water's capability to pass electrical flow.…”
Section: Introductionmentioning
confidence: 99%