（随時追記していきます）
＜ドル円＞
（02月20日、ショートサイン150.50域に到達）
＜02月20日、149.50域＞＜02月21日、149.00域＞ ＜ユーロ円＞
＜02月05日、158.00域＞＜02月06日、157.00域＞＜02月07日、156.00域＞
（02月19日、下に3枠転換。ロング161.00域、ショート155.00域から）
＜ユーロ米ドル＞
（02月20日、ロングサイン1.0500域に到達）
＜02月20日、1.0500域＞
＜豪ドル円＞
＜01月30日、95.50域＞＜02月06日、95.00域＞＜02月07日、94.50域＞
（02月21日、下に3枠転換。ロング97.00域、ショート94.00域から）
＜ポンド円＞
＜02月06日、188.00域＞＜02月07日、187.00域＞
（02月12日、上に3枠転換。ロング195.00域、ショート186.00域から）
＜ポンドドル＞
＜11月21日、1.2500域＞＜01月02日、1.2300域＞＜01月10日、1.2200域＞
（01月24日、上に3枠転換。ロング1.3500域、ショート1.2000域から）
＜豪ドル米ドル＞
＜12月04日、0.6400域＞＜12月06日、0.6350域＞＜12月17日、0.6300域＞
＜12月18日、0.6200域＞＜12月31日、0.6150域＞
（01月24日、上に3枠転換。ロング0.6950域、ショート0.6100域から）
＜ユーロポンド＞
＜09月23日、0.8300域＞＜11月08日、0.8250域＞＜12月10日、0.8200域＞
（02月03日、下に3枠転換。ロング0.8500域、ショート0.8150域から）
（P&F単位は、ユーロ円、ポンド円、ポンドドル、が100ポイント、その他50ポイントで1枠）
（個人的な見解ですので、投資は自己責任でお願いします。）日足PampFの状況 02月24日
The impact of ocean acidification caused by the increasing atmospheric CO2 has been studied in marine calcifiers, including hermatypic corals. However, the effect of elevated pCO(2) on the early developmental life-cycle stage of corals has been little studied. In this study, we reared polyps of Acropora digitifera in seawater at pH(T) 6.55, 7.31, 7.64, 7.77, and 8.03, controlled by CO2 bubbling. We measured the dry weights of polyp skeletons after the 40-d experiment to investigate the relationship between the seawater aragonite saturation state and polyp growth. In addition, we measured skeletal U/Ca ratio to estimate their pH dependence. Skeletal weights of coral polyps increased with the aragonite saturation state and reached an apparent saturation plateau above pH 7.77. U/Ca ratios had a strong inverse relationship with pH and a negligible relationship with skeletal growth rate (polyp weight), suggesting that skeletal U/Ca could be useful for reconstructing paleo-pH. Citation: Inoue, M., R. Suwa, A. Suzuki, K. Sakai, and H. Kawahata (2011), Effects of seawater pH on growth and skeletal U/Ca ratios of Acropora digitifera coral polyps, Geophys. Res. Lett., 38, L12809, doi:10.1029/2011GL047786.
>>402 打ち込みは形に入るための一人稽古としてはアリだと思いますが、技自体の練習は乱取り・又は動きながらの掛け合い(自然体で組み合って投げに入るまでの形の稽古)の方が効果的だと思います。 そして乱取りの場合は投げた後に寝技の態勢に入るまでを稽古するといいですよ。>>403 あー・・。まだあの時の話は尾を引いてたんですか。 いいじゃん。柔術やってようよ。>>404 でも、僕は近代柔道は好きになれません。
Trace elements in the Geological Survey of Japan carbonate reference materials Coral JCp-1 and Giant Clam JCt-1 were determined by inductively coupled plasma-mass spectrometry after digestion with 2% v/v HNO3. A standard addition method was adopted in this determination in order to neutralise the Ca matrix effect. in addition, Sc, Y, In and Bi were used as internal standards to control the matrix effect and correct instrumental drift. Of the eighteen elements measured in JCp-1, precisions for fourteen elements, including Cu, Cd and Ba, were better than 10% RSD and concentrations ranged from 0.002 mu g g(-1) (Cs) to 8.02 mu g g(-1) (Ba). The concentrations of measured trace elements in JCt-1, except for Cu, were lower than those in JCp-1. Precisions for all elements with concentrations higher than 0.04 mu g g(-1) in JCt-1 were also better than 10% RSD and concentrations were found to be between 0.001 mu g g(-1) (Cs) and 4.84 mu g g(-1) (Ba). The concentrations of more than fifteen trace elements in the aragonite reference materials are reported here for the first time. Both reference materials are suitable for use in geochernical studies of environmental reconstruction based upon biogenic carbonate materials.
We analyzed a 165 year delta(18)O coral record from Ishigaki Island, southwestern Japan, and compared our results with observed sea surface temperatures, as well as with the East Asian winter monsoon and El Nino Southern Oscillation. Coral skeletal delta(18)O fluctuations were consistent with other available SST information since the 1890s. The coral delta(18)O data indicated abrupt shift toward cooler condition during 1900-1905, consistent with the extremely cold winter air temperatures observed in Japan in 1902. The cold event was also supported by coral Sr/Ca data. Development of the Siberian High may have intensified the EAWM at this time, in association with active heat convection in the tropics and weak westerlies. This cooling may also have been related to surface ocean freshening in the Ogasawara Islands in the early 20th century. Thus, several phenomena were uniquely coupled during the first few years of the 20th century in the northwestern subtropical Pacific. Citation: Mishima, M., A. Suzuki, M. Nagao, T. Ishimura, M. Inoue, and H. Kawahata (2010), Abrupt shift toward cooler condition in the earliest 20th century detected in a 165 year coral record from Ishigaki Island, southwestern Japan, Geophys. Res. Lett., 37, L15609, doi: 10.1029/2010GL043451.
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