戻る
「早戻しボタン」を押すと検索画面に戻ります。 [閉じる]

コーパス検索結果 (１語後でソート)

通し番号をクリックするとPubMedの該当ページを表示します
1 ical utilization of macronutrients and CO(2) drawdown.
2 fluid composition, temperature, and pressure drawdown.
3 ntial implications for net atmospheric CO(2) drawdown.
4  weathering intensity), and more rapid CO(2) drawdown.
5 deep-water column without substantial oxygen drawdown.
6 egion for significant glacial carbon dioxide drawdown.
7 s to increase primary productivity and CO(2) drawdown.
8 d have contributed to glacial carbon dioxide drawdown.
9 ments high latitude changes to amplify CO(2) drawdown.
10  microsites where warming caused water table drawdown.
11 environments that drove extensive seawater V drawdown.
12  through benthic-pelagic coupling and carbon drawdown.
13 cessing, followed by a conventional external drawdown after the dope has left the spinneret.
14 pps Institution of Oceanography (AltSIO)] to drawdown ambient DOC in a coastal ecosystem.
15 ulfate reduction rates led to more effective drawdown and (34)S-enrichment of residual porewater sulf
16       While the extent of terminal Messinian drawdown and abruptness of reconnection are debated, rec
17 that regulates photosynthetic carbon dioxide drawdown and export from surface waters by phytoplankton
18 role of silicate mineral weathering in CO(2) drawdown and its contribution to the stability of Earth'
19 us oxygen minimum zone, promoting phosphorus drawdown and persistent oligotrophic conditions.
20 ave not explicitly represented this internal drawdown and therefore overestimate CO2 available for ca
21 rotease activity, virus production, nutrient drawdown, and lipid markers indicative of nutrient stres
22 n from the atmosphere and low biological CO2 drawdown are the main causes for the higher CO2, which a
23 lfur species, while triggering temporary pO2 drawdowns as negative feedback(15).
24                                 We show that drawdowns as small as 0.5 m can stimulate ebullition eve
25 k (basalt) weathering and atmospheric pCO(2) drawdown, as well as episodic marine photic-zone euxinia
26 sediment density indicated the onset of lake drawdown at 4200 cal yr BP and a negative hydroclimate a
27 particularly important role in forest carbon drawdown, but at present we have little understanding of
28 ne systems contributes to atmospheric carbon drawdown, but little empirical evidence is available to
29                                         Like drawdown by means of silicate weathering, this source is
30  kinetic and thermodynamic controls on CO(2) drawdown by natural or enhanced weathering.
31 enhanced rates of atmospheric carbon dioxide drawdown by silicate chemical weathering.
32 rocks, rivalling or even exceeding the CO(2) drawdown by silicate weathering at the global scale(10).
33 ackenzie River, which is three times the CO2 drawdown by silicate weathering in this basin.
34   In these systems, we show that water-level drawdowns can, at least temporarily, greatly increase pe
35 t capacity and lowered its CO2 concentration drawdown capacity in the intercellular airspace and chlo
36                                         This drawdown could become sequestration because polar contin
37 prominence of Diatoms inferred from silicate drawdown, drive interannual differences in the magnitude
38 ies challenges the notion that episodic pCO2 drawdown drove this major Cenozoic climate transition.
39 urrounding haggs water tables stabilised, as drawdown during dry conditions reduced, increasing the s
40 bon export, thus promoting atmospheric CO(2) drawdown during glacial periods.
41 hesis and the key variable C(i) /C(a) (CO(2) drawdown during photosynthesis).
42 ggest that episodes of major atmospheric CO2 drawdown during the last glacial period were linked to i
43 ean, driven by a rapid (<10 kyr) evaporative drawdown event during which sea-level dropped 1.7-2.1 km
44                          During this extreme drawdown event, the eastern Mediterranean basin lost up
45                                   Given that drawdown events of this magnitude are quite common in re
46 on-cycle model results of the time needed to drawdown excess atmospheric CO(2) following a carbon rel
47              Despite incomplete carbohydrate drawdown from defoliation and relatively rapid carbohydr
48         We model the temporal effects of CO2 drawdown from the atmosphere due to chemical weathering
49 must be considered when inferring soil CO(2) drawdown from the gas phase composition.
50 t Antarctic blue ice record of ice-elevation drawdown &gt;600 m during three such retreat events related
51 t production, by increasing surface nutrient drawdown in an ocean general circulation model.
52 nstant leaf internal [CO2 ], ci , a constant drawdown in CO2 (ca - ci ), and a constant ci /ca .
53 roductivity and understanding major nutrient drawdown in glacial periods.
54 production and associated atmospheric carbon drawdown in large parts of the world's oceans [1, 2].
55 tude is dominated by enhanced photosynthetic drawdown in North America and enhanced respiration in Eu
56  thought to contribute significantly to pCO2 drawdown in the Southern Ocean.
57                            Furthermore, this drawdown is driven by plant uptake rather than other con
58 er CDR efficiency enhances atmospheric CO(2) drawdown, it simultaneously reduces the potential for bi
59  to shallow (4 to 0 meters) states, reducing drawdown levels.
60 itivities of these reactions produce a CO(2)-drawdown maximum at erosion rates of ~0.07 millimeters p
61 ange in weathering regime, a critical carbon drawdown mechanism, across the PETM.
62  results support available evidence that CO2 drawdown--not gateway opening--caused Antarctic ice shee
63 orm i) the scale and pace of regional carbon drawdown obligations necessary to address budget exceeda
64                    Approximately 50% of this drawdown occurs in the world's active mountain belts, em
65 en (N(2)) fixation can induce a low latitude drawdown of 7-16 ppm CO(2).
66 iosphere is recorded in fluorescence and the drawdown of [Formula: see text] during summer.
67 ly 3% benthic biomass) suggests an increased drawdown of approximately 2.9x10(6) tonnes of carbon per
68    Although approximately 10% of the ocean's drawdown of atmospheric anthropogenic carbon dioxide may
69 organic carbon correlates with a significant drawdown of atmospheric carbon dioxide (CO2) at that tim
70 gative feedback mechanisms inhibited further drawdown of atmospheric carbon dioxide by high rates of
71 od webs(1), fishery yields(2) and the global drawdown of atmospheric carbon dioxide(3).
72 r substantial contribution to the biological drawdown of atmospheric carbon dioxide.
73 n the vast Pacific abyss and the concomitant drawdown of atmospheric CO(2).
74 he upper ocean and facilitates the diffusive drawdown of atmospheric CO(2).
75  enhance primary productivity and subsequent drawdown of atmospheric CO(2).
76 an circulation crisis facilitated the coeval drawdown of atmospheric CO2 and high-latitude ice sheet
77  not support the suggestion that a long-term drawdown of atmospheric CO2 was the main cause of the cl
78 successfully modeled the persistent vertical drawdown of atmospheric COS using the quantitative relat
79 s conditions were initially conducive to the drawdown of bioavailable phosphorus, they also permitted
80 rnover rates, which could cause differential drawdown of body AA pools and impart tissue-specific iso
81                                          The drawdown of both carbon dioxide (CO2) and nitrate per mo
82                                          The drawdown of carbon dioxide began well before the Devonia
83 e interior of the ocean, contributing to the drawdown of CO(2) and the sensitivity of the ocean to at
84      A leading hypothesis for the biological drawdown of CO(2) is iron (Fe) fertilisation of the high
85 gest that the mechanisms responsible for the drawdown of CO2 may be more responsive to temperature th
86  localized glacier acceleration, concomitant drawdown of ice from neighboring areas leads to widespre
87 anotrophy, suggesting a microbially mediated drawdown of methane on and in tree woody surfaces and ti
88 toplankton blooms, accelerating the seasonal drawdown of nitrate delivered by winter mixing.
89 iple canopies, which coincided with moderate drawdown of nonstructural carbohydrate reserves.
90 t concentration of cells, which results in a drawdown of nutrients in oceanic surface waters.
91 C accounts for up to 53% of R as a result of drawdown of organic carbon within Eastern North Atlantic
92  in the Eastern Mediterranean, adding to the drawdown of soil moisture.
93                       Although more complete drawdown of surface nutrients by phytoplankton during th
94 /U ratios (from 0.06 to 0.42), indicative of drawdown of U concentrations in seawater.
95  production leading to the most rapid annual drawdown of water-column pCO(2).
96  that eutrophication magnifies the effect of drawdown on CH4 emission.
97 s over the NCIEs rather than increases of Hg drawdown or riverine transport.
98 as triggered by a major (>=1 km) evaporative drawdown, or if it took place in a brine-filled Mediterr
99 lation in fall, and shortening of the oxygen drawdown period in winter explained positive DO trends.
100 s and long-term storage collected during two drawdown periods (fall and spring), although higher ARG
101 erboreal benthos shows a similar increase in drawdown, polar continental shelves would represent Eart
102  multiple processes were active during CO(2) drawdown, potentially including decreased land carbon an
103 gn parameters including solvent composition, drawdown pressure, and the net amount of solvent injecte
104                  Here, net atmospheric CO(2) drawdown primarily occurs during spring snowmelt, govern
105 ger increases in CH4 emission in response to drawdown (R(2) = 0.84, p < 0.01), suggesting that eutrop
106 ost generally decreased when the water level drawdown rate increased from 10 to 15 and 20 mm.day(-1)
107                Modeled variations in net CO2-drawdown rates are in excellent agreement with contempor
108 of similar mineral carbonation efforts where drawdown rates cannot be estimated by other means.
109 alaria control measures such as manipulating drawdown rates into reservoir management has the potenti
110                        Reservoir water level drawdown rates of 10, 15 and 20 mm.day(-1) were applied
111 is concept of an "erosion optimum" for CO(2) drawdown reconciles conflicting views on the impact of m
112 xtent to which (and the mechanisms by which) drawdowns short-circuit connections between methanogenes
113 ater pumping in Dhaka has caused large-scale drawdown that extends into outlying areas where arsenic-
114 ayed an overlooked role in the Neogene CO(2) drawdown that led to the Ice Ages and the current, now-p
115 evated primary production and biological DIC drawdown that reverses in some places the sign of the su
116 nrecognized episode of oxygenation and CO(2) drawdown was driven by the breakup of the supercontinent
117 c glaciation would have required rapid CO(2) drawdown within the Oi-1 timeframe, to levels lower than
118    This process involves an unusual internal drawdown within the spider's spinneret that is not seen

 
Page Top