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Szacowanie zniszczeń drogi startowej w wyniku oddziaływania przeciwnika. Cz.2

Brodzik Robert, Sarna Andrzej

Zeszyty Naukowe / Wyższa Szkoła Oficerska Sił Powietrznych

2017

Nr 1

103--116

Artykuł stanowi kontynuację publikacji zamieszczonej w poprzednim numerze „Zeszytów Naukowych WSOSP” (2016, nr 3). Na podstawie zapisów znajdujących się głównie w dokumentach STANAG 2929 – Naprawa Zniszczeń Lotniskowych (ang. Airfield Damage Repair – ADR) oraz zawartych w Dyrektywie Dowództwa Sojuszniczych Sił Zbrojnych NATO ACE 80-15 opisane zostały środki niszczenia infrastruktury lotniskowej oraz wybrane metody i techniki szybkiej naprawy.

The article is the continuation of the publication presented in the previous issue of PAFA Scientific Bulletin (No. 3, 2016). On the basis of provisions included in STANAG 2929 – Airfield Damage Repair (ADR) and the NATO Allied Command Europe Directive ACE 80-15, means of destroying airfield infrastructure as well as selected methods and techniques of quick repair were presented in the article.

Contribution of the vegetation layers in the nitrous oxide emission from alpine Kobresia humilis Serg. meadow ecosystem on the Tibetan Plateau

Du Y., Cao G., Deng Y., Sun G., Cui X.

Polish Journal of Ecology

2010

Vol. 58, nr 1

115-124

Nitrous oxide (N[2]O) was one of the major atmospheric greenhouse gases. Its budget was poorly understood in alpine meadow, a dominant vegetation type on the Tibetan Plateau. To characterize a Kobresia humilis meadow on the plateau, N[2]O emission rates were monitored from June 2003 to June 2006 in the study area located at 3280 m a.s.l. Nine plots with 1 m x 1 m each were divided into three treatments, i.e. intact herbaceous community (HCK), removal of aboveground plant biomass (CBK), and removal of both above and belowground plant biomass (BSK), to estimate contribution of plants, r hizosphere and bulk soil to the total N[2]O emission. N[2]O emission from plant aboveground biomass was calculated by flux difference between HCK and CBK, denoted as F[(HCK-CBK)], from rhizosphere by F[(CBK-BSK)], and from bulk soil was the flux in BSK treatment. Static chambers (height 50 cm, area 0.5 x 0.5 m2 )were used for gas collection. N[2]O emission rate was significantly correlated with soil temperature at 5 cm depth in both HCK and BSK (P <0.001). Both treatments demonstrated a seasonal peak rate in growing season and minimum rate in dormancy period. The mean emission rates in the three years were 39.7[plus or minus]2.9 and 30.6[plus or minus]2.5 [mu]g m[^-2] h[^-1] in HCK and BSK, respectively, with the former significantly higher than the latter (P <0.05). In CBK, however, the emission rate did not show consistent correlation with soil temperature, especially in growing season. Its three-year mean emission rate was 36.2[plus or minus]3.3 [mu]g m[^-2] h[^-1]. In the K. humilis meadow, bulk soil contributed much more than plants and rhizosphere. The mean emission rate was 3.5[plus or minus]2.9, 5.7[plus or minus]3.8, and 30.6[plus or minus]2.5 [mu]g m[^-2] h[^-1] (P <0.001) from plants, rhizosphere and bulk soil, and these accounted for 9, 14 and 77%, separately. Our results implied that N[2]O emission rate decreased little with grazing as indicated by the difference between HCK and CBK in K. humilis meadow (P <0.05). N2O emission from alpine meadow could not be ignored in addressing regional greenhouse gases budget on the Tibetan Plateau, considering the vast area and much higher radiative forcing of N[2]O.