• 한국산림과학회지
• /
• 제63권1호
• /
• pp.21-27
• /
• 1984

본(本) 연구(硏究)는 몇 종(種)의 침엽수(針葉樹)에 대하여 Shoot water potential의 일변화(日變化) 및 지(枝)의 Xylem conductivity의 특성(特性)을 측정고찰(測定考察)한 것으로 다음과 같은 결과를 얻었다. 1) Shoot water potential은 광도(光度)의 크기에 따라 변화(變化)하며, 광도(光度)의 감소(減少)가 시작된지 2시간(時間) 늦게 Shoot water potential의 증가(增加)가 시작되었다. 2) 지엽(枝葉)의 일중(日中) 최대수분(最大水分) 결차(缺差)는 12시(時)부터 14시(時) 사이에 일어나며, 그 값의 크기는 일본잎갈나무 -22 bar, 잣나무 -18 bar, 소나무 -15 bar, 젓나무 -14 bar, 리기다소나무 -10 bar 정도였다. 3) 수고(樹高) 1 m 당(當) 지엽(枝葉)의 수분결차(水分缺差)의 크기를 경사도(傾斜度)(${\varphi}_L/m$)로 나타내면 잣나무 -1.7 bar/m, 일본잎갈나무 -2.1 bar/m였다. 4) 지(枝)의 Relative Xylem conductivity (K, $cm^2/hr{\cdot}atm$)의 평균치(平均値)는 일본잎갈나무 2878, 리기다소나무 2763, 소나무 2652, 잣나무 2113 이었다.

• The Korean Journal of Ecology
• /
• 제20권3호
• /
• pp.175-179
• /
• 1997

To explanin allopatric distribution of Carpinus cordata and C. laxiflora in the field the effect of soil flooding on photosynthesis and water relations was tested with field grown saplings. Under the flooding condition stomatal conductance of C. laxiflora decreased markedly from day two after flooding treatment and remanined low throughout the experiment. In contrast, flooding had no effect on stomatal conductance of C. cordata throughout the exper iment. The rate of photosynthesis of C. laxiflora was significantly suppressed under flooding conditions, whereas that of C. cordata was not affected in the flooded condition. On day seven after flooding treatment xylem pressure potential of C. laxiflora significantly decreased. Flooding, however, did not have any effect on the xylem pressure potential of C. cordata throughout the experiment. From these findings it is concluded that there is a difference in resistance to flooding between C. cordata and C. laxiflora and that one of the the factors responsible for allopatric distribution in the two species is flooding.

• The Korean Journal of Ecology
• /
• 제19권5호
• /
• pp.453-463
• /
• 1996

Diurnal changes of microclimatic conditions and tissue water relations were measured at two sites where Carpinus laxiflora and C. cordata were allopatrically distributed. The microclimatic conditions at a site where C. laxiflora was distributed produced severe water stress condition during summer months. Daily maximum temperature reached $30.4^\circC$ and the highest vapor pressure deficit was 1.31 KPa when 13 rainless days were continued. During this period soil water content decreased to below the field capacity even at a depth of 20 cm and xylem pressure potential also decreased to ­2.04 MPa. However, turgor potential was maintained more than 0.4 MPa. Patterns of stomatal conductance were changed with evaporative demand and soil water availability. On the other hand, microclimatic conditions at a site where C. cordata was distributed were moderate water strees condition compared with those at a site C. laxiflora was distributed. Though soil water content was maintained above field capacity C. cordata showed a remarkable decrease in turgor potential and stomatal conductance throughout the experiment. These results indicate that there is a difference in habitat characteristics between the two species and C. laxiflora is more resistant than C. cordata to water stress.

• Journal of Applied Biological Chemistry
• /
• 제43권3호
• /
• pp.170-175
• /
• 2000

A pot-lysimeter experiment was conducted with 3-year-old 'Tsugaru' apple (Malus domestica Borkh) trees to examine the changes in oxygen diffusion rate (ODR) with lateral flow velocity of water through soil. The influence of lateral water flow velocity on water relations and elemental content in leaf, and sap temperature distribution patterns of the xylem of trees were also determined. Trees were grown under four soil water regimes: (1) fast laterally flowing (FWT, $2.50{\times}10^{-4}cm\;s^{-1}$), (2) slow laterally flowing (SWT, $0.25{\times}10^{-4}cm\;s^{-1}$), and (3) stagnant water table (WLT) at 60-cm, and (4) drip-irrigation at -40 kPa of soil matric potential as a control. The rate of $O_2$ diffusion converged near $2{\times}10^{-3}g\;m^{-2}\;min^{-1}$ for FWT and control soils, but decreased below $1{\times}10^{-3}g\;m^{-2}\;min^{-1}$ 40 days after treatment (DAT) for WLT soils. For SWT soils, however, the ODR at 15 cm below the soil surface was similar to that of control, but at 45 cm below the soil surface, ODR was similar to that of the WLT treatment. Leaf water potential of FWT and SWT plants was similar to that of control plants, but the values for SWT plants declined by 98 DAT. Leaf water potential of WLT plants decreased from -1.86 MPa (9 DAT) to -2.41 MPa (59 DAT) and finally down to -2.70 MPa. The sap temperature measured at 1100-hr was lowest at top and highest at bottom for FWT and control plants, but this pattern of SWT and WLT plants was disturbed from 29 DAT. However, for SWT plants, such thermal disturbance of sap temperature disappeared from 63 DAT.

• 한국환경농학회지
• /
• 제25권2호
• /
• pp.164-169
• /
• 2006

착과량을 달리한 '후지'/M.9 품종에서 생육 최성기중 토양수분 변화에 따른 수액 이동 특성과 수체 생리반응을 조사하였다. 적정 착과는 적습 조건인 -50 kPa에서 VPD 및 최대증발산량과 비슷한 양상의 수액이동량을 보였으나 과다 착과는 -50 kPa 및 -80 kPa 조건에서 최대증발산량보다 낮은 수액흡수량을 보였다. 적정 착과는 모든 토양수분 조건에서 최대증발산량보다 일중 $1.06{\sim}3.93L$ 많은 수액이 이동되는 특성을 보였고 과다 착과는 적정 착과보다 토양수분 -50 kPa 조건에서 21%, -20 kPa과 -80 kPa에서 $31{\sim}36%$ 정도 낮은 수액 이동량을 보였다. 착과 처리에 따른 신초생육과 엽면적은 적정 착과 처리구가 다른 처리구보다 유의성 있게 높았으나 과다 착과 처리구는 가장 낮았다. 적정 착과 처리구의 엽수분포텐셜은 다른 처리구에 비해 모든 토양수분 조건에서 가장 낮아서 수분소모율이 가장 높았다. 따라서 '후지'/M.9 품종은 적정 착과량 유지와 더불어 생육성기 중 적습조건을 유지하는 것이 수액이동을 고려할 경우, 증산효율을 높이는데 바람직할 것으로 판단되었다.

• 생물환경조절학회지
• /
• 제10권1호
• /
• pp.1-9
• /
• 2001

참다래 과실의 생장은 2중 S자 곡선적으로 생장을 하지만, 그 곡선은 해에 불확실할 때가 있다. 이러한 원인을 과실조직의 수분상태에 의한 것으로 생각되어, 1995년과 1996년에 참다래 과실의 생장기간 중에 psychrometer를 사용하여 일중 과실조직의 수분상태 변화를 조사했다. 과실조직의 수분 포텐셀의 변화는 1996년의 과실생자의 제3기를 제외하고는 크지 않앗다. 1995년과 1995년 모두 과실의 수확기에 가까울수록 수분 포텐셜이 점진적으로 떨어졌다. 한편, 과실조직의 삼투 포텐셜은 수분 포텐셜과 비슷하게 변화를 했지만, 1995년 10월 14일의 동이 트기 전에 -1.5MPa로 급격히 떨어진 후, 3시간이 경과한 후 -1MPa로 회복되었고, 과실수확 적기에는 -1.7MPa까지 떨어졌다. 1996년의 과실은 1995년 과실보다 낮은 삼투 포텐셜을 나타냈다. 도관의 수분상태에 관계되는 잎의 수분 포텐셜은 1996년의 경우, 과실생장 제2깅 동이 트기 전에 불구하고 -1MPa 이하로 떨어졌다. 1995년은 과실수확 적기에만 1996년과 같이 -1MPa 이하로 떨어졌다. 1996년 과실은 과실생각 제2기에 과실의 삼투 포텐셜과 팽압의 상승이 1995년 과실보다 높았다. 이러한 요인들이 1996년 과실의 당 농도를 높게 하였다. 이들 parameter의 변화는 1996년 과실이 과실생장의 제3기에 수체가 수분 스트레스를 받았다는 사실을 암시하는 것이다. 따라서, 1995년 과실과 1996년 과실의 생장 차이는 기상변화에 따른 과실 조직의 수분상태에 의한 것으로 판단된다.

• 한국작물학회:학술대회논문집
• /
• 한국작물학회 2017년도 9th Asian Crop Science Association conference
• /
• pp.35-35
• /
• 2017

How do plants take up water from soils especially when water is scarce in soils? Plants have a strategy to respond to water deficit to manage water necessary for their survival and growth. Plants regulate water transport inside them. Water flows inside the plant via (i) apoplastic pathway including xylem vessel and cell wall and (ii) cell-to-cell pathway including water channels sitting in cell membrane (aquaporins). Water transport across the root and leaf is explained by a composite transport model including those pathways. Modification of the components in those pathways to change their hydraulic conductivity can regulate water uptake and management. Apoplastic barrier is modified by producing Casparian band and suberin lamellae. These structures contain suberin known to be hydrophobic. Barley roots with more suberin content from the apoplast showed lower root hydraulic conductivity. Root hydraulic conductivity was measured by a root pressure probe. Plant root builds apoplastic barrier to prevent water loss into dry soil. Water transport in plant is also regulated in the cell-to-cell pathway via aquaporin, which has received a great attention after its discovery in early 1990s. Aquaporins in plants are known to open or close to regulate water transport in response to biotic and/or abiotic stresses including water deficit. Aquaporins in a corn leaf were opened by illumination in the beginning, however, closed in response to the following leaf water potential decrease. The evidence was provided by cell hydraulic conductivity measurement using a cell pressure probe. Changing the hydraulic conductivity of plant organ such as root and leaf has an impact not only on the speed of water transport across the plant but also on the water potential inside the plant, which means plant water uptake pattern from soil could be differentiated. This was demonstrated by a computer simulation with 3-D root structure having root hydraulic conductivity information and soil. The model study indicated that the root hydraulic conductivity plays an important role to determine the water uptake from soil with suboptimal water, although soil hydraulic conductivity also interplayed.

• 한국환경복원기술학회지
• /
• 제5권2호
• /
• pp.53-62
• /
• 2002

The objectives of this study were to understand the tolerance mechanism of woody plants to water stress and tolerance changes in relation to mycorrhizal formation. Lespedeza cyrtobotrya Miq. commonly used for erosion control in slopes were raised from seeds and transplanted to 120 plastic pots. Sixty pots received the top soil of a Fraxinus americana forest, while remaining 60 pots received the autoclaved top soil. The forest soil contained 1,200 spores per 100g of arbuscular endomycorrhizal fungus, mostly Glomus sp. The plants were raised outside with regular supply of water and mineral nutrients. Two kinds of water deficit treatment and a control were started at the middle of July : cyclic water deficit treatment with 3 cycles of sequential water stress at the point of xylem water potential of about -0.6, -0.6, and -1.7 MPa and recovery, and non-cyclic water deficit treatment with single water stress at about -1.5 MPa. The non-stressed plants received plenty of water throughout the period. In late August the plants were harvested for measurements of dry weight, N, P, carbohydrate contents, net photosynthesis and superoxide dismutase(SOD) activities. Both cyclic and non-cyclic water deficit treatments reduced dry weight by 60% and 40%, respectively, and reduced nitrogen absorption, while increased SOD activities. Water-stressed plants also showed increased carbohydrate contents in the leaves and lowered stomatal conductance. Mycorrhizal inoculation resulted in an average of 40% infection of roots and 2-3 times increase in P absorption in water-stressed as well as non-stressed plants. Mycorrhizal formation also increased shoot-root ratio. The results that SOD activities of water-stressed plants with mycorrhizal infection were significantly lower than those of non-mycorrhizal plants suggest the possibility of improvement of water-stressed condition by mycorrhizal formation. It was concluded that endomycorrhizal formation increased tolerance of Lespedeza cyrtobotrya seedlings to water stress.

• 한국산림과학회지
• /
• 제96권4호
• /
• pp.438-447
• /
• 2007

이 연구의 목적은 송이산 소나무림생태계의 구조와 기능, 그리고 토양 수분동태를 이해하는 것이다. 연구는 충북 괴산군 칠성면 속리산국립공원내 쌍곡의 송이산 소나무림에서, 생태계 구조에 속하는 식생구성 및 엽면적지수 그리고 기능에 속하는 광합성, 증산, 목부수분포텐셜과 토양수분변동을 측정분석하였다. 송이산의 수직적 구조로써 주요 상층식생은 소나무였고, 중층은 신갈나무, 하층은 진달래, 철쭉, 신갈나무, 쇠물푸레나무였다. 송이산의 엽면적지수는, 6월~9월에 3.8, 10월에 2.6, 11월~4월에는 2.1로 연중 변하였다. 수목들의 광합성은 8월말에 $6.0{\sim}7.0{\mu}mol\;CO_2/m^2/s$였으나, 10월 말경에는 소나무 $4.0{\mu}mol\;CO_2/m^2/s$, 신갈나무 $2.0{\mu}mol\;CO_2/m^2/s$, 철쭉은 마이너스 값이었고, 쇠물푸레나무는 낙엽되었다. 수목들의 증산량은 8월말경에 $2.5{\sim}3.5mmol\;H_2O/m^2/s$, 10월 중순경에는 약 $1.0 mmol\;H_2O/m^2/s$로 감소하였다. 신갈나무는 다른 활엽수보다 늦게까지 광합성과 증산작용을 하였다. 각 수종의 목부수분포텐셜은 소나무가 -10~ -22 bars, 진달래와 철쭉, 신갈나무, 쇠물푸레나무는 -5~-12 bars의 범위로 변화하였는데, 8월 말경이 -12 bars로 가장 낮았고, 10월 중순경에 -3 bars 정도였다. 송이산의 토양수분은 지형과 관련이 깊었다. 수분함량은 산능선부에서 7~11%, 중간인 산복에서 8~15%, 산록은 11~19%의 범위였다. 송이균환내부의 온도는 비균환보다 약 0.2~0.4 높은 경향이었고 송이원기 형성온도인 $19.0^{\circ}C$는 9월 중순경에 도달한 것으로 추정되었다. 송이균환의 수분은 비균환보다 약 0.5~2.0% 낮았다. 이것은 송이균환이 대사작용을 하면서 열이 발생하고 수분을 소비하고 있음을 나타낸다. 송이 발생에는 생태계의 구조와 기능이 복합적으로 관여하므로 이들의 관계에 대한 연구가 더욱 필요하다고 생각한다.

• 한국물환경학회지
• /
• 제33권6호
• /
• pp.689-695
• /
• 2017

This study was carried out to investigate the physicochemical and adsorptive characteristics of black carbon (BC) materials for cesium in case of severe nuclear accidents. The BC was prepared with a xylem of oak and pine trees incompletely combusted with different ramp rate and final temperature. Carbon (C), hydrogen (H) and oxygen (O) atomic ratios, BET, pore structure, and zeta potential were characterized for the produced BC. A low cesium concentration ($C_w{\approx}10^{-7}M$) was used for sorption batch experiments. The H/C and O/C ratios of BC decreased with the increase of final temperature, which indicates a carbonization of the wood materials regardless of ramp rate and tree species. However, SEM images showed different pore structures depending on tree species such as steric and plate-like for oak-BC and pine-BC, respectively. The greatest sorption distribution coefficients of $K_{d,Cs}{\approx}1,200{\sim}1,800L\;kg^{-1}$ were observed for the oak-BC produced at $400^{\circ}C$, while comparatively low $K_{d,Cs}$ < $100L\;kg^{-1}$ for pine-BC. In addition, the sorption capabilities of BC declined with the increase of combustion temperature up to $600^{\circ}C$, because high temperature destroyed surface functionalities with the rise of ash components in the BC. Therefore, the sorption processes of BC for radioactive cesium are predominantly controlled by final production temperature of BC as well as raw materials (e.g., tree species).